Book
One Planet Many People: Atlas of Our Changing Environment
SINGH, Ashbindu, et al.
Reference
SINGH, Ashbindu, et al. One Planet Many People: Atlas of Our Changing Environment.
United Nations Environment Programme, 2005
Available at:
http://archive-ouverte.unige.ch/unige:32650
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ONE PLANET
MANY PEOPLE
Atlas of Our Changing Environment
i
Copyright2005,UnitedNationsEnvironmentProgramme
ISBN:92-807-2571-8
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ii
ONE PLANET
MANY PEOPLE
Atlas of Our Changing Environment
United Nations Environment Programme
2005
iii
Editorial and Production Team
UNEP
AshbinduSingh,TeamCoordinator
USGS
ThomasR.Loveland,Writer
SAIC,TSSCtotheUSGS
MarkErnste,RemoteSensing/GISScientist
KimberlyA.Giese,DesignandLayout
RebeccaL.Johnson,Editor
JaneS.Smith,EditorialAssistant/Support
JohnHutchinson,Cartographer
EugeneFosnight,Writer
Consultant
H.GydeLund,LeadWriter
TejaswiGiri,ProjectManager
JaneBarr,Writer
EugeneApindiOchieng,RemoteSensing/GISAnalyst
UNEP–Nairobi
AudreyRingler,CoverDesign
Toobtainacopyofthispublication,pleasecontact:
AshbinduSingh,RegionalCoordinator
UNEP/GRID-SiouxFalls
USGSNationalCenterforEarthResources
ObservationandScience(EROS)
47914252ndStreet
SiouxFalls,SD57198
Phone:1605594-6117
Fax:1605594-6119
E-mail:
[email protected]
iv
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Table of Contents
FOREWORD................................................................................................................................................................................vi
PREFACE.................................................................................................................................................................................... vii
1 Introducing the Planet – A Story of Change.......................................................................................................................... 1
References..................................................................................................................................................................... 9
2 People and Planet – Human Influences on the Planet........................................................................................................ 13
2.1WorldPopulation................................................................................................................................................. 16
2.2Culture.................................................................................................................................................................. 21
2.3LandUseandDegradation.................................................................................................................................. 25
2.4EcoregionsandEcosystems................................................................................................................................. 32
2.5Biodiversity,InvasiveSpecies,andProtectedAreas.......................................................................................... 35
2.6EnergyConsumptionandResourceExtraction.................................................................................................. 43
References................................................................................................................................................................... 62
3 Human Impacts on the Planet – Visualising Change over Time......................................................................................... 67
3.1Atmosphere........................................................................................................................................................... 72
3.2CoastalAreas........................................................................................................................................................ 90
3.3Water.................................................................................................................................................................... 118
3.4Forests.................................................................................................................................................................. 156
3.5Cropland.............................................................................................................................................................. 194
3.6Grasslands............................................................................................................................................................ 216
3.7UrbanAreas........................................................................................................................................................ 230
3.8TundraandPolarRegions.................................................................................................................................. 260
References................................................................................................................................................................. 280
4 Natural and Human-induced Extreme Events................................................................................................................... 289
4.1Geo-hazards........................................................................................................................................................ 291
4.2ClimaticHazards................................................................................................................................................ 300
4.3IndustrialHazards............................................................................................................................................... 307
References................................................................................................................................................................. 314
EPILOGUE................................................................................................................................................................................ 316
ACRONYMS AND ABBREVIATIONS........................................................................................................................................ 318
ACKNOWLEDGEMENTS.......................................................................................................................................................... 320
v
Foreword
P
eopleaffecttheenvironmentasthey
interactwithit,usingitforfood,
shelter,andrecreationandmaking
changestobettersuittheirneeds,purposes,andinclinations.Throughourability
toadaptnaturalresourcestoouruse,we
havealteredtheenvironmentinwaysthat
cannowbeobjectivelymeasured.Our
presenceontheEarthcanbeseenthrough
changesonthelandscape,asviewedfrom
space.Thispublicationpresentsimages
fromspacethatportraythenatureand
extentofourimpactontheplanet.
Changeisinevitableandanintegral
partofourplanet,ourenvironment,and
evenus.Ourabilitytoadapttodiverse
surroundingshasallowedustoovercome
manyenvironmentalconstraintsandtailor
theplanettoourbenefit.Weharnessed
fire,cultivatedplantsanddomesticatedanimals.Webuilthomes,thenvillages,and
thencities.Webecame“hewersofwood
anddrawersofwater.”Webuilttoolsand
discoveredhowtoquarryrocksandlater
metals.Eachadvanceallowedustofurther
adapttoandaffecttheenvironmentthat
shapedus.
Ourabilitytoactpositivelytosafeguard
ourheritageandnaturalwealthmaybe
KlausTöpfer,Ph.D.
ExecutiveDirector
UnitedNationsEnvironmentProgramme
vi
affectedbytheconsequencesofoursuccess,however.Asournumbershave
increased,wehavealsoevolvedsocially
andculturally,applyingdifferentbeliefs
andpracticestolivinginandusingthe
environment.Whatwedoaffectsthosefar
awayfromus,eventhoseseparatedfrom
usbymountains,deserts,andoceans.Our
activitieschangetheplanetinwaysthat
affectourhealthaswellasthehealthofthe
plantsandanimalsuponwhichwedepend.
Weharvesttheseas,consumewaterand
energyresources,andconvertforestsinto
pastureandcropland.Wemustbeever
consciousofthepotentialtooveruse
thelandandstressitinwaysthatit
cannotbear.
Ourgrowingpopulationsandsettlementsmakelifeeasierinsomeways,but
alsomakeusmorevulnerabletomassive
earthquakes,volcaniceruptions,andother
disasters.Imaginewhatwouldhappenin
ItalytodayifVesuviuseruptedonthesame
scaleitdidwhenitdestroyedPompeii.
Wehavegravitatedtotheshores,makingourselvesmorevulnerabletostorms
andhurricanes.Wehavesettledalong
rivers,makingourselvesmorevulnerable
tofloods.Wehavespreadintomarginal
GhassemAsrar,Ph.D.
ScienceDeputy
AssociateAdministrator
NationalAeronautics
andSpaceAdministration
climates,makingourselvesmorevulnerabletodrought.Wildfiresthreatensome
ofourcitiesandsettlements,justasthey
doourforestsandcroplands.Eachof
theseeventscanaffecthundredsofthousandsofpeople,andthecostofprotecting
ourselvesandreducingtheriskofdisaster
continuestoincrease.Ourownactivities
canalsoleadtodisasterssuchasoilspills
andnuclearandindustrialaccidentsthat
candevastateasmuchasanynaturalevent.
Ourdilemmaistoavoidthemostproblematicconsequenceswithoutconstraining
ourneedandabilitytoprovidetheworld’s
inhabitantswiththeenvironmentand
resourcesthatwillenableeverypersonto
pursueanequitablelifewithallthatsucha
lifeentails.
Theimagespresentedhereshowboth
thepositiveandnegativeimpactsofhumanlifeonEarth.Wehopealsotheywill
providefoodforthought,asweseekways
tobalanceouruseoftheEarth’sresources
withtheneedtosustaintheenvironments
thatproducethemandsupporttheliving
systemsthatwevaluesohighly.
CharlesG.Groat,Ph.D.
Director
UnitedStatesGeologicalSurvey
JohnTownshend,Ph.D.
UniversityofMaryland
Chair,AdvisoryCommittee
UNEP/DEWA–NorthAmerica
Preface
O
urpopulationisgrowing,yetour
landbaseiscurrentlyfixed.With
eachnewinhabitantcomesa
needtomakemoremodificationstothe
Earth’senvironment.Theimpactsofthese
modificationsmaybebothdetrimental
andbeneficial.Forexample,weestimate
thattheEarthislosing15millionhectares
oftropicalforestlandperyear,alossthat
hasanegativeeffectonbiodiversity.Atthe
sametime,muchofthisdeforestedland
isbeingconvertedtoagriculturallandto
feedourgrowingpopulation;thisisapositiveeffect.
Inthepast30years—sincetheUnited
NationsConferenceontheHumanEnvironmentinStockholmin1972—wehave
madeaconcertedefforttounderstandthe
limitsoftheEarth’sbountifulresources
andhavetakenactionstopreserveand
sustainthem.Thispublicationillustrates
someofthechangeswehavemadetothe
environmentintherecentpast.Itserves
bothasanearlywarningforthingsthat
maycomeandasabasisfordeveloping
policydecisionsthatcanhelpsustainthe
Earth’sandourownwell-being.
Thefirstchapterofthisatlasprovidesa
shortenvironmentalhistoryoftheworld,
onethatillustrateshowwegottowherewe
are.Chapter2looksatthepeopleandthe
planettoday,coveringstatusandtrends
overthelast30years.Chapter3examines
commonissuesregardingtheEarth’sland
coverandprovidesexamplesthatillustrateenvironmentalstatus,trends,causes
andconsequencesofchangeintheatmosphere,oceansandcoastalzones,fresh-
waterecosystems,forests,cropland,grasslands,urbanareas,andtundraincluding
polarregions.Chapter4illustrateschanges
thataretheresultofextremeevents,both
naturalandhuman-induced.
Theseexamplesraisemanyquestions.
Whatisourlikelyenvironmentalfuture?
Arewebetterorlesspreparedforenvironmentalchange?Whatcanpeopledoto
createabetterfuture?Theanswersdepend
ontheactionswechoosetotake.
SteveLonergan,Ph.D.
Director
UnitedNationsEnvironmentProgramme
DivisionofEarlyWarningandAssessment
PhotoCredits(lefttoright):
KernKhianchuen/UNEP/Topfoto
DirkHeinrich/UNEP/Topfoto
AimenAl-Sayya/UNEP/Topfoto
vii
Topographic Map of the World
Credit: UNEP/NASA–GTOPO30
viii
ix
Credit:MarkErnste/UNEP/UNEP-GRIDSiouxFalls
x
1
Introducing the Planet
A Story of Change
I
noursolarsystem,asingleplanet—theEarth—supportshumanlife.
Worldpopulationisincreasing.Yet
forthemoment,theEarthremains
theonlyhomeforthehumanspecies.The
wayinwhichwecareforthisplanetwill
affectourfutureandthefutureofourchildrenforgenerationstocome.
Seenfromspace,theEarthislargelya
blueplanetaroundwhichswirlsofwhite
cloudsconstantlymove.TheEarth’sblue
areasareitsoceans.Oceansaccountfor
approximately70percentoftheEarth’s
totalsurfacearea;theremaining30per
centisland.Thetotalsizeoftheterrestrial
surfaceisapproximately149millionkm2
(59.6millionsquaremiles)(McNeill2000;
Gracen.d.).
TheEarth’slandsurfaceisrichinits
variety.ThehighestpointontheEarth’s
landsurfaceisMountEverest,abreathtak-
ing8850m(29035ft)abovesealevel.
ThelowestpointistheDeadSea,whichis,
onaverage,about400m(1312ft)below
sealevel.Terrestrialsurfacesgainandlose
heatmuchmorequicklythanoceansanda
region’sdistancefromtheequatordramaticallyaffectsitsclimate.Lands
nearesttheequatortendtobe
thewarmest.Thosethatliein
themiddlelatitudestypically
havecoolerclimates,butare
notascoldaslandsnearthe
poles.Some20percentof
theEarth’sterrestrialsurfaceiscoveredby
snow.Another20percentismountainous.
Just30percentoftheEarth’slandsurface
issuitableforfarming.
Mostpeopleareaccustomedtoseeingtheworldaroundthemasarelatively
stableplace,agenerallynurturingenvironmentthathasallowedthehumanraceto
expandanddevelopincountlessways.In
fact,theEarthisconstantlychanging,as
isourunderstandingofit(Figure1.1).
SomechangestotheEarth’ssurfaceoccur
onmicroscopiclevels.Otherchangestake
placeonascalesolargeastobealmost
“The only thing permanent
is change.”
— TheBuddha(SiddarthaGautama)
inconceivable.Sometypesofchangeare
instantaneous,whileothertypesoccur
slowly,unfoldingovercenturies,millennia,
andeveneons.Somechangesarecaused
bytheactionsofpeople.Manyothersare
partofnatural,inexorablecyclesthatcan
onlybeperceivedwhencataclysmicevents
occurorthroughpainstakingresearch.
Credit:BlueMarble/UNEP/NASA(2002)
Figure1.1:TheEarth’ssurfacehaschangeddramatically
overtime—ashasourunderstandingofit.Earlyideas
abouttheshapesandlocationsofthecontinents,for
example,werefardifferentfromwhatisknownaboutthe
landsurfacetoday.
Credit:Unknown/UNEP/Tapestries&More
1
Table1.1–ApproximatechangeoftheEarth’sglobalvegetativecoverinrelationtohumanpopulation
(AdaptedfromMcNeill2000).
Year
PercentoftheEarth’sVegetatedLandArea
Forestand
Woodland
Grassland
Pasture
Cropland
HumanPopulation
(Billions)
8000B.C.
51
49
0
0
0.005
1700A.D.
47
47
4
2
0.6
1900
43
40
10
6
1.6
1920
43
38
12
7
1.9
1940
41
35
16
8
2.3
1960
40
31
20
9
3.0
1980
38
26
25
11
4.4
1990
36
27
26
11
5.3
Credit:PaulFusco/UNEP/NRCS
Credit:ChatreeWanasan/UNEP/Topfoto
AgentsofEnvironmentalChange
Inordertosurvive,everyorganismmust
FromtheEarth’searliestbeginnings,forces eitheradapttoitsenvironmentormodify
theenvironmenttomakeitmorehospisuchasclimate,wind,water,fire,earthtable.Humansareparticularlyadeptat
quakes,volcaniceruptions,andtheimmodifyingtheirenvironments.Bytheiracpactsofmeteorsandcometshaveshaped
theEarth’sterrestrialenvironments.These tionsandinteractionswiththelandscape,
sameforcesareatworktodayandwillcon- forexample,peoplecanincreasetherange
tinuefarintothefuture.Inaddition,every ofcertainplantspecies,eitherbymodifylivingthinginfluencesitsenvironmentand ingexistingenvironmentsorbydispersisinfluencedbyit.Onespeciesmaylessen ingseedsintonewones.Environmental
thechancesforsurvivaloftheorganismsit modificationsmadebypeoplemaybe
beneficialordetrimentaltoafewormany
consumesforfood.Thatsamespecies,in
otherspecies.Large-scaleenvironmental
turn,isaffectedbytheactionsof
changesmaynotbenefitorbetotheliking
otherorganisms.
ofpeoplethemselves(Nott1996).Asworld
FiveMajorEventsintheHistoryoftheEarth
ThroughouttheEarth’shistory,eventshaveoccurredthatdramaticallyimpactedlifeonour
planet.Fiveofthoseeventsstandoutashavingresultedinwidespreadextinctions,insomecases
destroyingmorethan90percentofalllivingthings(Eldredge2001):
•Around440millionyearsago,arelativelysevereandsuddenglobalcoolingcauseda
massextinctionofmarinelife(littleterrestriallifeexistedatthattime).Anestimated25
percentoftheexistingtaxonomicfamilieswerelost.(Afamilymayconsistofafewto
thousandsofspecies.)
•NeartheendoftheDevonianPeriod,some370millionyearsago,asecondmajor
extinctionoccurred.Roughly19percentoftheexistingtaxonomicfamilieswere
wipedout.Itisuncertainwhetherclimatechangewasadrivingfactor.
•About245millionyearsago,athirdmajorextinctiontookplace.Scientists
estimatethatmorethanhalf(54percent)ofalltaxonomicfamilieswerelost.
Climatechangemayhaveplayedarole,andthatchangemayhavebeencaused
byacometormeteorimpactingtheEarth.
•AttheendoftheTriassicPeriod,around210millionyearsago,roughly23
percentofexistingtaxonomicfamiliessuddenlybecameextinct.Thisevent
occurredshortlyaftertheappearanceofthefirstdinosaursandmammals.Its
causesarenotyetfullyunderstood.
•Thefifthmajorextinctionisthemostwell-known.Itoccurredabout65millionyearsagoattheendoftheCretaceousPeriod.Theeventledtotheextinctionofallterrestrialdinosaursandmarineammonites,alongwithmany
otherspeciesoccupyingmanydifferenthabitats.Alltold,approximately17
percentofalltaxonomicfamiliesvanishedinaveryshorttime.Currently,
themostwidelyacceptedhypothesistoexplainthismassextinctionisthata
cometorotherlargeextra-terrestrialobjectstrucktheEarth.Anotherview
proposesthatagreatvolcanicevent,orseriesofevents,disruptedecosystemssoseverelyworldwidethatmanyterrestrialandmarinespeciesrapidly
succumbedtoextinction.
Credit:Unknown/UNEP/Bigfoto
22
populationhasincreasedandthescope
andnatureoftechnologyhaschanged,
peoplehavebroughtaboutenvironmental
changesthatmayseriouslyimpacttheir
futurewell-beingandevensurvival.
Humansbeganmodifyingtheirenvironmentalongtimeago(Table1.1).EvidenceoftheexistenceofourfirsthumanoidancestorsdatestothePlioceneEpoch,
whichextendedfromroughly5million
to1.8-1.6millionyearsago(Wikipedia
n.d.).Theseprotohumanssoughtprotectionfromtheelementsandfrompredatorsinnaturalshelterssuchascavesand
rockoverhangs.Overtime—andpossibly
Fire—AToolforHumankind
Forthousandsofyearshumanshaveusedfirefor:
Hunting
Bysettingfiretopartsofthelandscape,peoplewereabletodrivegame
animalsintosmaller,moreconfinedareasthatmadehuntingeasier.Fire
wasalsousedtodriveanimalsintoimpoundments,chutes,riverorlakes,or
overcliffs.Firesalsohelpedmaintainopenprairiesandmeadowsbykilling
bushesandtreesandencouragingrapidgrowthofgrasses.
Improvingplantgrowthandyields
Settingfireswasawaytoimprovegrassforgrazinganimals,bothwildand
domestic,andtopromotethegrowthofcertaindesirableplantspecies.
Protection
Firewasusedtoprotecthumanhabitations.
Collectinginsects
Sometribesused“firesurrounds”tocollectandroastcrickets,grasshoppers,
andmoths.Peoplealsousedfiresmoketoquietbeeswhilecollectinghoney.
Managingpests
Firewasahandytoolforreducingordrivingawayinsectpestssuchasflies
andmosquitoesaswellasrodents.Firewasalsoeffectiveforeliminating
undesirableplants.
Warfareandsignaling
Firewasbothaneffectivedefensiveandoffensiveweapon.Offensively,itwas
usedtodepriveenemiesofhidingplacesintallgrassesorunderbrush.Used
defensively,firecouldprovidecoverduringanescape.Smokesignalshelped
alerttribestothepresenceofpossibleenemiesortogatherforcestocombat
afoe.Largefiresweresettosignalatribalgathering.
Clearingareasfortravel
Firesweresometimesstartedtocleartrailsthroughdensevegetation.
Burninghelpedtoimprovevisibilityinforestsorgrasslandsforhunting
andwarfare.
Fellingtrees
Singedorcharredtreeswereeasiertofellandtoworkwith.
Clearingriparianareas
Firewasusedtoclearvegetationfromtheedgesoflakesandrivers.
Managingcrops
Burningwaslaterusedtoharvestcropsandcollectgrassseeds.Firealso
helpedpreventabandonedfieldsfrombecomingovergrownandwasemployedtoclearareasforplanting.
Credit:JeffVanuga/UNEP/NRCS
influencedbytheonsetofcolderweather
duringtheIceAges—theycreateddwelling
placesforthemselvesinlocationsthathad
nonaturalshelter.
Theoldestsurvivingtracesofsucha
human-madehabitationdatetoabout
2millionyearsagofromOlduvaiGorge
incentralAfrica.There,asmallcircleof
stoneswasfoundstackedinsuchawayas
toapparentlyhaveheldbranchesinposition.Thisearlyexampleofmodification
oftheenvironmentwastheworkofHomo
habilis,atool–makinghumanancestor
(Kowalskin.d.).
ThePleistoceneEpoch,includingthe
PaleolithicandMesolithicPeriods(Wikipedian.d.),isusuallydatedfromtheend
ofthePlioceneto10000yearsago.The
PaleolithicPeriod,orOldStoneAge,isa
termcoinedinthe19thcenturytodefine
theoldestperiodinthehistoryofhumankind.Itlastedforsome2.5millionyears,
fromthetimehumanancestorscreated
andusedthefirststonetoolstotheendof
thelastglacialperiodsome10000years
ago.Homoerectus,thoughtbymanytobe
thedirectancestorofmodernhumans,
livedfromapproximately2millionto
around400000yearsago.Asaspecies,
Homoerectuswasverysuccessfulindevelopingtoolsthathelpedinadaptingto
newenvironments.Theywerepioneersin
developinghumanculture,ultimatelymovingoutofAfricatopopulatetropicaland
sub-tropicalenvironmentalzonesinthe
OldWorld,possiblyasearlyas1.8million
yearsago.
Homoerectusmayalsohavemastered
theuseoffirearound1.6millionyears
ago(Mcrone2000).Fireisanexception-
allypowerfultool.Sincemostanimals,
includinglargepredators,areafraidof
fire,earlyhumansquicklydiscoveredthat
campfiresofferedprotectionfromattack
duringthenight.Controloffireallowed
themtomoveintocolderregionsasitprovidedwarmthaswellassecurity.Firealso
changedthewayfoodwasprepared.Food
thatiscookedislesslikelytocarrydisease
organismsanditssoftertexturemakesit
easiertoeat,enhancingthesurvivalof
youngchildrenandoldmembersof
apopulation.
TheuseoffirealmostcertainlyincreasedduringthePaleolithicPeriod.At
thattime,humanswereprimarilyhuntergatherers.Theroleoffireinmodern
hunter-gathererculturesgivesussomeidea
ofitsimportanceduringthePaleolithic
andhowpeoplethenmostlikelyused
3
it(Williams2001).Firewasanimportant
toolineverydaylife.Itwasalsoatoolwith
greatpotentialtomodifyandchange
theenvironment.
ThetransitionfromHomoerectusto
Homosapiens—ourmodernhumanspecies—occurredapproximately300000
to400000yearsago.Throughoutthe
PaleolithicPeriod,humanssurvivedby
exploitingresourcesintheirenvironment
throughsubsistenceactivitiessuchasfishing,hunting,andplantgathering.From
ethnographicstudiesofmodernhuntergatherers,wecaninferthatthebasicsocial
unitofPaleolithictimeswastheband:a
looselybound,relativelysmallgroup(25
peopleonaverage)formedbythevoluntaryaggregationofafewfamilies.Bands
weremobile,regularlychangingresidence
insideadelimitedterritoryaccordingto
fluctuationsintheabundanceofdifferent
foodsources.Inter-regionalmigrations,
suchasthosewithintheWestern
Hemisphere,probablytookplaceduring
thistime.
Thismobilelifewaspunctuatedbyepisodesofreunion,whenseveralalliedbands
wouldmeetandperformreligiousceremonies.Suchoccasionswouldhaveprovided
atimeandplaceforthetransmissionof
techniquesandartisticfashions,promoting
theirspreadacrossvastexpanses
ofterritory.
Some10000yearsago,anewgeological
timeperiod,theHolocene,began.World
sealevelsroseabout35m(116ft)inthe
earlyHoloceneduetomeltingglaciers.As
theicemeltedandglaciersreceded,many
landareasthathadbeendepressedby
glacialweightslowlyroseasmuchas180
m(594ft)abovetheirlate-Pleistoceneand
early-Holocenelevels.Bothsea-levelrise
anddepressionsinthelandscapeallowed
temporaryocean-waterincursionsinto
regionsthataretodayfarfromanysea.
Climaticshiftsalsowereverylargeduring
thisperiod.Habitablezonesexpanded
northwards.Large,mid-latitudeareassuch
astheSaharathatwerepreviouslyproductivebecamedeserts.Atthestartofthe
Holocene,largelakescoveredmanyareas
thatarenowquitearid.
Animalsandplantsdidnotundergo
majorevolutionarychangesduringthe
Holocene,butthereweresignificantshifts
intheirdistribution.Severaltypesoflarge
mammalsincludingmammoths,mastodons,saber-toothedcats,andgiantsloths
wentextinctinthelatePleistoceneand
earlyHolocene.Ecological“islands”ofisolatedspecieswerecreatedthroughoutthe
world,includinghigh-altituderemnants
ofcooler,previouslyregionalclimate
ecosystems.
Theperiodfrom10000to5000or
4000yearsagoisrecognizedastheNeolithicPeriod(NewStoneAge).Itwas
precededbytheMesolithicPeriod(Middle
StoneAge),whichroughlycorresponds
withthebeginningoftheHolocene.The
MesolithicPeriodformedatransition
betweenthePaleolithicandNeolithic
Periods,thatis,fromtheendofthePleistocenetotheintroductionofagriculturein
anygivengeographicalregion
(Wikipedian.d.).
Thesizeoftheworld’shumanpopulation10000yearsagoisestimatedtohave
beenaround5million(IPC2003a).This
periodsawthebeginningofagriculture
andthedomesticationofanimals.People
learnedtocultivatecropsratherthanto
simplygatherwhatnatureprovidedinthe
wildandtotameandraiseanimalssuchas
sheep,goats,cattle,horses,anddogs,ratherthanhuntthem.Theseactivitieshelped
ensurebetterfoodsuppliesandresulted
inwide-rangingculturalconsequences.
Permanentcommunitieswerenowestablished,sincepeoplewerenolongerdependentonfollowingwildanimalsormoving
withtheseasons.Day-to-dayexistence
changedfromalifeofnomadicforaging
tooneofpermanence.Thisallowedsome
individualstoexploretoolproductionto
refinerudestonetoolsandimproveimplementssuchasstone-bladeknives,bowdrills
withflintsforstartingfires,fishhooks,
axes,andplows.Otherpeoplefoundtime
toimproveagriculturalandpastoraltechniques,enablingcommunitiesto
growmorefoodandtendlivestock
moreeffectively.
Thecultivationofplantsandthedomesticationofanimalsdramatically
Credit:PuneYanachot/UNEP/Topfoto
4
Credit:T.Revter/UNEP/Topfoto
impactedhumanlifestylesduringthe
NeolithicPeriod.Peoplelefttheirtemporaryrockandwoodensheltersandbegan
tobuildmorepermanenthomesinclose
proximitytotheirfarmsandgardens,
wheretheystartedproducingcerealgrains
whichbecameanimportantpartoftheir
diet(WadleyandMartin1993).
TheNeolithicPeriodmarkedthebeginningoftruecivilization,layingthefoundationsformajordevelopmentsinsocial
evolutionsuchaspermanentsettlements,
villagelife,formalizedreligion,art,architecture,farming,andtheproductionof
advancedtoolsandweapons.
Agriculture
Thefirstcultivationofwildgrainssome
12000to10000yearsagoturnedhuntergatherersintofarmers.Thetransitiongave
peopleamoreabundantanddependable
sourceoffoodandchangedtheworld
forever(Wilford1997).Thepracticeof
agriculturefirstdevelopedintheFertile
CrescentofMesopotamia(partofpresentdayIraq,Turkey,Syria,andJordan).This
region,whichwasmuchwetterthenthan
itistoday,washometoagreatdiversityof
annualplantsand32ofthe56largestseedproducinggrasses(PrimalSeedsn.d.).
Around11000yearsago,muchofthe
Earthexperiencedlongdryseasons,probablyasaconsequenceofthemajorclimate
changethattookplaceattheendofthe
lastIceAge.Theseconditionsfavored
annualplantsthatdieoffinthelongdry
season,leavingadormantseedortuber.
Suchplantsputmoreenergyintoproducingseedsthanintowoodygrowth.An
abundanceofreadilystorablewildgrains
Figure1.2:TheEarth’sclimatesysteminvolves
complexinteractionsamongmanyelementsand
processes.Source:http://www.usgcrp.gov/usgcrp/Library/
ocp2004-5/ocp2004-5.pdf
5
andotheredibleseedsenabledhuntergatherersinsomeareastoformpermanentlysettledvillagesatthistime(Primal
Seedsn.d.).
Theoriesvaryastohowagriculture
cameintobeing.Somescientistsarguethat
risingglobaltemperaturescreatedfavorableconditionsforagriculture.Others
proposethatanincreaseinseasonality
afterthelastIceAgeencouragedpeopleto
domesticateplants.Stillotherresearchers
maintainthatecologicalchanges,social
development,oragrowinghumanpopulationintensifiedtheexploitationofspecific
plantspecies(Baldia2000).
Anothersuggestionisthatanincrease
incarbondioxide(CO2)onaglobalscale
mayhaveplayedacriticalroleinbringing
aboutthesynchronyofagriculturalorigins
aroundtheglobe(Sage1995).Studies
haveshownthatariseinatmosphericCO2
levelswouldhaveincreasedproductivity
ofmanyplantsbyasmuchas50percent.
Furthermore,thewaterefficiencyofcultivatedplantsincreased,givingtheseplants
acompetitiveadvantageoverwildspecies.
Afewscientistshaveproposedthatclimaticchangesattheendofthelastglacial
periodledtoanincreaseinthesizeand
concentrationofpatchesofwildcerealsin
certainareas(WadleyandMartin1993).
Increasedavailabilityofcerealgrains
providedpeoplewithanincentivetomake
amealofthem.Thosewhoatesizable
amountsofcerealgrainsinadvertently
discoveredtherewardsofconsumingthe
variouschemicalcompoundsthatcereal
grainscontain.Asprocessingmethods
Credit:EdSimpson/UNEP/PhotoSpin
suchasgrindingandcookingmadecereal
grainsmorepalatable,greaterquantities
wereconsumed.
Atfirstthesepatchesofwildcereals
wereprotectedandharvested.People
begantosettlearoundthesefoodsources.
Theygraduallyabandonedtheirnomadic
lifestyleandbeganworkingtogethermore
cooperatively.Later,landwascleared,
seedswereplanted,andseedlingstended
toincreasethequantityandreliabilityof
cerealgrainsupply.
Theriseofmorepermanentsettlementsintensifiedthedomesticationof
6
Credits:MichaelVanWoert/UNEP/NOAA
animals.Thefirstcandidatefordomestication,around11000yearsago,wasprobablythedog.Thecowwasdomesticated
around10000yearsago.Goats,sheep,and
pigswereaddedtothegrowinglistofdomesticatedanimalsaround8000yearsago
inwesternAsia.ThehorsewasfirstdomesticatedinnorthernRussiaaround4000
yearsago.Localequivalentsandsmaller
specieswereincreasinglydomesticated
from2500yearsago(Wikipedian.d.).
Farmingandherdingfacilitatedthe
growthoflargersettledhumanpopulationsandledtoincreasedcompetitionfor
productivelands,layingthefoundationfor
organizedwarfare.Foodsurplusesfreed
peopletospecializeinvariouscrafts,such
asweaving,and,inlargercommunities,
supportedtheemergenceofaprivileged
eliteclass.Archaeologistsandhistorians
agreethattheriseofagriculture,including
thedomesticationofanimalsforfoodand
labor,producedthemostimportanttransformationintheinteractionbetweenthe
environmentandhumanculturesincethe
lastIceAge—perhapsthemostsignificant
developmentinhumanhistorysincethe
controloffire(Wilford1997).
Othermilestonesinhumanhistorythat
benefitedpeopleandchangedtheenvironmentinclude:
ClassicalGreeceandRome(0toabout
500A.D.)
Theworldpopulationatthebeginningof
thisperiodwasroughly200million(IPC
2003a).Duringthisperiod,glasswasinventedandmap-makingdeveloped.
MiddleAgestotheRenaissance(500to
about1700)
Bythispoint,worldpopulationhadgrown
toabout250million(IPC2003a).The
clock,compass,telescope,thermometer,
andbarometerweredeveloped,enabling
peopletoexpandtheirknowledgeofthe
EarthandtheUniverse.
TheIndustrialRevolution(1700–present)
By1700,worldpopulationhadrisento
about600million(IPC2003a).Thisperiodwitnessedthedevelopmentofmechanizationandthebeginningofseriousair
pollution.Industrialchangesalsoledtoan
agriculturalrevolution.
TheAgriculturalRevolution(1750–1900)
By1750,worldpopulationhadrisento790
million(IPC2003a).Inmanycountriesthe
wayinwhichfarmersproducedfoodbegantochange.Newcropswereexploited
usingnewtechnologiessuchastheseed
drillandtheironplow.Thesemethodsof
productionproducedgreaterquantities
TheBronzeandIronAges(roughly3300
ofmorenutritiousfoods,therebyimprovB.C.to0A.D.)
ingpeoples’dietsandhealth.Better,more
Theworldpopulationapproximately5000 efficientfarmingmethodsalsomeantthat
fewerpeoplewereneededtofarm.Asa
yearsagoisestimatedtohavebeenabout
7million(IPC2003a).Thisperiodsawthe result,unemployedfarmersformedalarge
introductionofmetallurgyandmining,the newlaborforce.
inventionofthewheel,andthedomesticationofthehorse.
TheGreenRevolution(1944–present)
In1944,worldpopulationreached2350
million(Anonn.d.).Abreakthroughin
wheatandriceproductioninAsiainthe
mid-1960s,whichcametobeknownasthe
GreenRevolution,symbolizedtheprogressofagriculturalscienceasitdeveloped
moderntechniquesforuseindeveloping
countries.TheGreenRevolutionhadits
origininMexico,wherea“quiet”wheat
revolutionbeganinthe1940s
(Borlaug2000).
ThegoaloftheGreenRevolutionis
toenhancetheefficiencyofagricultural
processesinordertoincreasetheproductivityofcrops,therebyhelpingdeveloping
countriestomeettheneedsoftheirgrowingpopulations.TheRevolutionconsisted
ofthreeprimaryelements:continuing
expansionoffarmingareas,double-croppingexistingfarmlands,andusinggeneticallyimprovedseeds.ThankstotheGreen
Revolution,weareabletogrowmorecrops
onlessland.
However,theGreenRevolutionhas
impactedbiodiversityandinsomeareas
waterqualityandcoastalecosystems.The
newtechniquesencouragedlarge-scaleindustrialagricultureattheexpenseofsmall
farmerswhowereunabletocompetewith
high-efficiencyGreenRevolutioncrops
(Wikipedian.d.).Nevertheless,theGreen
millionmetrictonnesperyear.By2025,
productionmustbenearlydoubled.In
ordertofeedtheworld’speoplethrough
ThePresentDay
2025,anadditional1000millionmetric
tonnesofgrainmustbeproducedannuWorldpopulationnowstandsat6billion
ally.Mostofthisincreasewillhavetobe
people(IPC2003b).Whileglobalresourcsuppliedbyimprovingcropyieldsonland
esweresufficienttosupporttheEarth’s
alreadyinproduction.
humanpopulationasawholepriortothe
IndustrialRevolution,individualgroupsor
Thiswillnotbepossibleunlessfarmevenentirecivilizationssometimesreached ersworldwidehaveaccesstoexisting
environmentallimitsforaparticularresource;anumbercollapsedasaresultof
unsustainablehunting,fishing,logging,
orlandusepractices.Theever-increasing
culturalglobalizationofthe20thand21st
centurieshasbroughtwithitglobalization
ofresourcedegradation,makingcurrent
environmentalproblemsanissueforthe
entireworldratherthanforindividual,
isolatedgroups.Althoughperceived
environmentallimitscansometimesbe
overcome,neithersciencenortechnology
hasyetmadepossibleunlimitedsuppliesof
naturalresourcesordepositoriesforwaste
(CasagrandeandZaidman1999).
Moderateprojectionsputworldpopulationataround8300millionby2025(FigCredit:LeeTsunhua/UNEP/Topfoto
ure1.3),withthehopethatitwillstabilize
high-yieldcropproductionmethodsas
atroughly10000to11000millionbythe
wellasbiotechnologicalbreakthroughs
endofthecentury.Ittookapproximately
thatincreasetheyield,dependability,and
10000yearstoexpandglobalfoodproductiontothecurrentlevelofabout5000 nutritionalqualityofourbasicfoodcrops
(Borlaug2000).
Revolutionisasuccess.Weareabletofeed
morepeoplenow,thaneverbefore.
Credit:PaulusSuwito/UNEP/Topfoto
7
Figure1.3:Earth’sshrinkingbiospherelandarea(ha)/capita
1900-2000AD
Currently,theEarthistheonlyhomewehave.Witheachnewperson
addedtoourgrowingpopulation,theamountofourlivingspace
decreases.Thuswehavelesslandavailablebutanincreasingneedto
feedmorepeople.Thisputsmorepressureonourlimitedresources
andexacerbateschangesintheenvironment.Source:LundandIremonger2000
HumanbeingshavebeenverysuccessfulinexploitingtheEarth’sresources.Intheprocess,however,theyhavebroughtaboutmajorchangesinthe
Earth’secosystems,especiallyinrecentyears:
•halftheworld’swetlandswerelostduringthe
lastcentury;
•loggingandlanduseconversionhavereduced
forestcoverbyatleast20percent,andpossiblyas
muchas50percent;
•nearly70percentoftheworld’smajormarine
fish
stocksareeitherover-fishedorbeingfishedatthe
biologicallimit;
•overthelasthalfcentury,soildegradationhasaffectedtwo-thirdsoftheworld’sagriculturalland.Itis
estimatedthateachyearsome25000millionmetric
tonnesoffertiletopsoil—theequivalentofallofthe
wheatfieldsinAustralia—islostglobally(Casagrandeand
Zaidman1999);
•eachyear,anestimated27000speciesdisappearfromthe
planet—approximatelyoneevery20minutes(Casagrandeand
Zaidman1999);
•theEarthnowappearstobeexperiencingasixthmass
extinctioneventthatbeganabout50000yearsagowiththe
expandingroleofhumansintheworld(Recer2004).Unlikepastevents,thismassextinctionisbeingcausedby
humanactivitiessuchastransformingthelandscape,
overexploitingspecies,pollution,andalienspecies
introductions(Eldredge2001);
•damsandengineeringworkshavefragmented60
percentoftheworld’slargeriversystems.They
havesoimpededwaterflowthatthetimeittakes
foradropofwatertoreachtheseahastripled;
•humanactivitiesaresignificantlyaltering
thebasicchemicalcyclesuponwhichall
ecosystemsdepend
(Kirby2000).
HistorianJ.R.McNeillrecently
wrote(McNeill2000):“Itisimpossibletoknowwhetherhumankind
hasenteredagenuineecologicalcrisis.Itisclearenough
thatourcurrentwaysare
ecologicallyunsustainable,butwecannot
knowforhowlong
wecanyetsustain
88
Credit:NoguchiYoshi/UNEP/Topfoto
themorwhatmighthappenifwedo.”In
thepast,humanitytrodrelativelylightlyon
theEarth,eventhoughcivilizationswere
intenselyconcentratedinsomeplacessuch
asMesopotamiaandtheNileRivervalley.
Today,however,theevidencefromspace
showssignsofthehumanpresencein
almosteverycorneroftheplanet.
Globalconcernabouttheenvironment
andthefateoftheEarthemergedinthe
1970s,asdidinternationalinitiativesto
addressthoseconcerns.Inroughlythepast
30years,theenvironmenthasbornethe
stressesimposedbyafour-foldincreasein
humanpopulationandaneighteen-fold
increaseinworldeconomicoutput(UNEP
2002).Notsurprisingly,whenscientists
comparerecentsatelliteimagesofthe
Earth’ssurfacewiththosetakenoneorseveraldecadesago,theimpactpeoplehave
hadontheplanetisobviousand
oftendisturbing.
Thisatlasvividlyillustratessomeofthe
changesthehumanracehasbroughtabout
ontheEarth—bothgoodandbad—over
thepast30years.Indoingso,italsoserves
asanearlywarningforenvironmental
eventsthatmayoccur.Wehopeitwillbe
usefulasabasisfordevelopingpolicydecisionsandpromotingindividualactionsto
helpsustaintheEarthandensurethewellbeingofitsinhabitants.
References
Kirby,A.(2000).Humansstressecosystemstothelimit.BBCNews,
UK.http://news.bbc.co.uk/1/hi/sci/tech/926063.stmon19
March2004.
UNEP(2002).GlobalEnvironmentOutlook3(GEO3)–Past,
presentandfutureperspectives.Earthscan,London,UK,446.
http://www.unep.org/geo/geo3/on4March2004.
Kowalski,W.J.(n.d.).http://www.personal.psu.edu/users/w/x/
wxk116/habitat/on19March2004.
USGlobalChangeResearchProgram(2004).OurChanging
Planet:TheU.S.ClimateChangeScienceProgramforFiscal
Years2004and2005,8.http://www.usgcrp.gov/usgcrp/Library/ocp2004-5/ocp2004-5.pdfon13October2004.
Anon.(n.d.).Worldpopulationthroughtheyears.http://www.
neopage.com/know/worldpop.htmon19March2004.
Baldia,M.O.(2000).Theoriginsofagriculture.Version2.01.
http://www.comp-archaeology.org/AgricultureOrigins.htmon
19March2004.
Borlaug,N.E.(2000).TheGreenRevolutionrevisitedandtheroad
ahead.Special30thAnniversaryLecture,TheNorwegianNobel
Institute,Oslo,Norway,September8,2000,23.http://www.
nobel.se/peace/articles/borlaug/borlaug-lecture.pdfon1
August2004.
Casagrande,J.andZaidman,Y.(1999).Defininganewbalance
betweenhumansandtheenvironment.Changemakers.http://
www.changemakers.net/journal/99September/index.cfmon
18March2004.
Eldredge,N.(2001).Thesixthextinction.ActionBioscience
Journal.http://www.actionbioscience.org/newfrontiers/eldredge2.htmlon19March2004.
Grace,J.(n.d.).WorldForestsandGlobalChange.Universityof
Edinburgh,TheInstituteofEcology&ResourceManagement,
Edinburgh,UK.http://www.ierm.ed.ac.uk/ierm/teaching/
slides.pdfon7October2004.
IPC(2003a).Historicalestimatesofworldpopulation.U.S.Census
Bureau,PopulationDivision,InternationalProgramsCenter,
Cambridge,UK.http://www.census.gov/ipc/www/worldhis.
htmlon19March2004.
IPC(2003b).Totalmidyearpopulationfortheworld:1950-2050.
U.S.CensusBureau,PopulationDivision,InternationalProgramsCenter,InternationalDataBase,Cambridge,UK.http://
www.census.gov/ipc/www/worldpop.htmlon19March2004.
Lund,H.G.andIremonger,S.(2000).Omissions,commissions,and
decisions:theneedforintegrstedresourceassessments.Forest
EcologyandManagement,128(1-2):3-10.
McNeill,J.R.(2000).Somethingnewunderthesun–Anenvironmentalhistoryofthetwentiethcenturyworld.W.W.Norton&
Company,NewYork,USA,421.
Mcrone,J.(2000).Thediscoveryoffire.NewScientist.May2000.
http://www.btinternet.com/~neuronaut/webtwo_features_
fire.htmon18March2004.
NASA(2002).BlueMarble:LandSurface,ShallowWater,and
ShadedTopography.http://visibleearth.nasa.gov/view_rec.
php?vev1id=11656on18August2004.
Nott,A.(1996).EnvironmentalDegradation.http://www.geocities.
com/atlas/env/on6October2004.
Wadley,G.andMartin,A.(1993).Theoriginsofagriculture–abiologicalperspectiveandanewhypothesis.AustralianBiologist
6:96–105.http://www.veganstraight-edge.org.uk/GW_paper.
htmon19March2004.
Wikipedia(n.d.).Thefreeencyclopedia.http://en.wikipedia.
org/wiki/Main_Pageon18March2004.
Wilford,J.N.(1997).Newcluesshowwherepeoplemadethegreat
leaptoagriculture.TheNewYorkTimesCompany.http://
www.spelt.com/origins.htmlon19March2004.
Williams,G.W.(2001).ReferencesontheAmericanIndianuse
offireinecosystems.U.S.DepartmentofAgriculture:Forest
Service,Washington,DC,USA.http://www.wildlandfire.com/
docs/biblio_indianfire.htmon15March2004.
PrimalSeeds(n.d.).AgricultureOrigins.http://www.primalseeds.
org/agricult.htmon19March2004.
Recer,P.(2004).Manyspeciesatriskofextinction.Research
Study.AssociatedPress.http://story.news.yahoo.com/
news?tmpl=story&u=/ap/wildlife_goneon19March2004.
Sage,R.F.(1995).WaslowatmosphericCO2duringthePleistocene
alimitingfactorfortheoriginofagriculture?GlobalChange
Biology,1:93-106.http://www.greeningearthsociety.org/Articles/origins.htmon23March2004.
TapestriesandMore.http://www.tapestries.cc/Imagehtm/gMap.
htmlon12May2004.
9 9
Nightlight Map of the World
Credit: UNEP/NOAA, NASA
10
11
Credit:BusakornBuranabunpo/UNEP/Topfoto
12
2
People and Planet
Human Influences on the Planet
H
umansareaprolificandopportunisticspecies,among
themostsuccessfulofallthe
Earth’sinhabitants.Asthesize
ofthehumanpopulationhasincreased,
peoplehavespreadacrosstheglobeinto
everyimaginablehabitat.Throughout
humanhistory,peoplehavedemonstrated
anuncannyabilitytoadapttoandsurvive
insomeveryharshplaces,including,most
recently,outerspaceandtheocean—at
leastforshortperiodsoftime.
Ashumanculturehasevolved,people
havedevelopednewwaysoflivinginand
usingtheirenvironment,andofhelping
themselvestoallthattheEarthhasto
offer.TheirabilitytoexploittheEarth’s
seeminglyendlessresourceshasbeenavitalkeytothesuccessofthehumanspecies.
However,manymajoradvancesin
humanculture—fromthecultivationof
cropsandthedevelopmentofcitiesto
moderntechnologies—havetendedto
insulatepeoplefromtheveryenvironment
thatshapedthemanduponwhichthey
depend.Asagroup,peoplehaveoften
forgottenthatforeveryactiontakenthere
isareaction,animpact.
Theimpactsofhumanactivitieson
theEarthoftenhavebothnegativeand
positivecomponents.Forexample,when
peopleconvertforestsorgrasslandsto
croplandtheyimprovethemeansby
whichtofeedtheirever-growingnumbers.
Atthesametime,theyinvariablyreduce
biologicaldiversityintheconvertedareas.
Overtime,peoplehaverarelybeenfully
awareofthetremendouschangetheyhave
wroughtontheEarthorthattheirsuccesseshaveoftenbeenachievedattheexpense
ofotherspeciesandtheenvironment.
Sincetheearly1970s,manyexcellent
textshavebeenwrittenabouttheplight
oftheworld(Heywood1995;Middleton
1997;WRI2000;Chew2001;FAO2001;
HarrisonandPearce2001;IPCC2001;
McNeill2001;UNEP2002a).Thisatlas
supplementstheseworksbyproviding
illustrationsofbothpositiveandnegative
human-causedchangesthathavetaken
placeontheEarth.Satelliteimages,togetherwithphotographs,provideaunique
viewofhowpeopleareimpactingtheterrestrialenvironmentandwhattheconsequencesofenvironmentalchangemean
intermsofhumanwell-being.Theimages
Credit:DavoliSilvaho/UNEP/Topfoto
andthechangestheyillustratearediverse.
Buttheyareunitedbyacommonmessage:
environmentalchangedoesmatter.
TheInternationalConferenceon
PopulationandDevelopmentProgramme
ofActionnotedthatstabilizationofworld
Credit:EdSimpson/UNEP/PhotoSpin
13
PopulationChange
Latin America 3% Others 2.5%
Africa 4.5%
Asia Pacific
US 5%
(including former
Soviet Asia) 54%
Europe
(including
Russia)
25%
Europe
(including
Russia)
14%
Asia 60%
Africa 10%
Latin America
& Caribbean 8%
Middle East &
North Africa 6%
North America 5%
Others 3%
populationiscrucialtoachievingsustainabledevelopment.Populationstabilizationisalsonecessaryformanaginghuman
impactsontheEarth’senvironmentand
resources.In1999,theEarth’shuman
populationreached6000million,having
grownduringthemid-1990satarateof13
percentperyear,withanaverageannual
additionof78millionindividuals.Asof
1999,countrieswithpopulationsof100
millionormoreincludedChina,India,the
UnitedStates,Indonesia,Brazil,Pakistan,
theRussianFederation,Bangladesh,Japan,
andNigeria.Accordingtothemedium
variantoftheUnitedNations’population
estimatesandprojections,worldpopulationwillreach7200millionbytheyear
2015.Ninety-eightpercentofthepopulationincreasewilltakeplaceinless-developedregionsoftheworld.Africawill
experience,byfar,themostrapidrateof
growth(PopulationDivision2000).
Theoverallimpactthathumanshave
ontheglobalenvironmentisproportional
tothenumberofpeopleontheEarthand
theaverageinfluenceofeachindividual.
Ifthatoverallimpactistobereduced,addressingbothofthesefactorsisessential.
Changeindistributionofworldpopulation1900and2000.Source:http://www.newint.org/issue309/facts.html
CaseStudy:Parrot’sBeak
BetweenSierraLeoneandLiberia,
thereisasmallstripoflandbelonging
toGuineaknownasthe“Parrot’sBeak.”
AscivilwarsragedinSierraLeone
andLiberia,hundredsofthousandsof
refugeeshavefledtorelativesafetyin
Guinea,manyofthemsettlinginthe
Parrot’sBeak.TheUnitedNationsHigh
CommissionerforRefugees(UNHCR)
estimatesthattherefugeepopulation
constitutesupto80percentofthelocal
populationthere(UNEP2000).
The1974imageoftheParrot’s
BeakinGuinea(left)showsthesurroundingterritoryofLiberiaandSierra
Leone.Scatteredthroughoutthedeep
greenforestoftheParrot’sBeakregion
aresmallflecksoflightgreen,where
compoundsofvillageswithsurrounding
agriculturalplotsarelocated.Several
darkspotsintheupperleftoftheimage
aremostlikelyburnscars.
The2002image(facingpage)shows
theParrot’sBeakregionclearlydefined
byitslightgreencolorsurroundedby
darkergreenforest.Thelightgreen
Deforestationofindigenouspalmtreesin
therefugeecamphasleftbarrenhillsides.
Credit:Unknown/UNEP/UNEP-GRIDGeneva
14
WorldBiomes
Biomes
Tropical and Subtropical Moist Broadleaf Forests
Tropical and Subtropical Dry Broadleaf Forests
Tropical and Subtropical Coniferous Forests
Temperate Broadleaf and Mixed Forests
Temperate Conifer Forests
Boreal Forests / Taiga
Tropical and Subtropical Grasslands, Savannas, and Shrublands
Temperate Grasslands, Savannas, and Shrublands
Flooded Grasslands and Savannas
Montane Grasslands and Shrublands
Tundra
Mediterranean Forests, Woodlands, and Scrub
Deserts and Xeric Shrublands
Mangroves
Bare Rock / Ice
Source: World Wildlife Fund Terrestrial Ecoregions Dataset.
Abiomeisamajorecologicalcommunityofplants
andanimalswithsimilarlifeformsandenvironmentalconditions.SomeoftheEarth’smajorterrestrial
biomesincludeforests,grasslands,deserts,rain
forests,andtundra.Differentbiomesarethesource
ofdifferentkindsofresourcesandprocesses(collectivelycalledecosystemservices)suchaswater,
soil,oil,naturalgasandotherfuels,mineralsand
otherrawmaterials,wildlifehabitat,erosioncontrol,
nutrientcycling,waterfiltration,foodproduction,
andgeneticresources.Theestimatedglobalvalue
oftheEarth’sbiomesforecosystemservicesalone
rangesfromUS$16trilliontoUS$54trillionayear
(Costanzaetal.1997).
coloristheresultofdeforestationin
the“safearea”whererefugeeshave
setupcamp.Manyoftherefugees
integratedintolocalvillages,created
theirownfamilyplots,andexpanded
thezonesofconvertedforestareauntil
theyallmergedintothelargerdefined
area.Intheupperpartofthe2002imagetheforestdevastationisespecially
obvious,asareasthatweregreeninthe
1974imagenowappeargray.Logging
interestsalsomovedintothehigher
elevationsofthisregion,expandingthe
deforestedzonevisibleintheupper
leftcorneroftheimage.
Overallimpoverishmentofthe
environmentoftheParrot’sBeakis
directlyrelatedtotherapidlyincreasingpopulationinthearea,mainlydue
toimmigration,andagrowthrateof
aboutthreepercentamongtheindigenouspopulation.Naturalresources
arebeingexploitedtocreatemorearablelandforcrops,woodforcharcoal,
firewoodandconstructionmaterials,
andcommercialloggingforrevenue.
Source:UNEP2000.
Deforestationisevidentonthehillssurroundingtherefugeecamp.
Credit:Unknown/UNEP/UNEP-GRIDGeneva
15
2.1 World Population
A
simpledefinitionofworldpopulationisthenumberofpeoplealiveontheEarthatanygiven
pointintime.Worldpopulationreached
6400millionin2004anditcontinuestogrowbysome
80millioneachyear(Table2.1).Sincethe1950s,China
hasbeentheworld’smostpopulouscountry(Table2.2).
China’spopulationiscurrentlygreaterthanthatofsome
entireworldregions(GlobalPopulationProfile2002).By
2050,worldpopulationisestimatedtoreach7900to
10900million,whenstabilizationoftheEarth’spopulationislikelytotakeplace.Whetherornotworldpopulationfallswithinthatrangebythismiddleofthiscentury—ratherthanexceedingit—willdependuponmany
ofthechoicesandcommitmentsthatpeoplemakeinthe
comingyears(UNFPA2001).
Table2.1–Worldpopulationforgivenpointsintime
Source:ESA2003
Year
Population
1970
3692492000
1975
4068109000
1980
4434682000
1985
4830979000
1990
5263593000
1995
5674380000
2000
6070581000
2005
6453628000
2010
6830283000
ThesizeofanypopulationchangesasaresultofflucCredit:KhinAyeMyat/UNEP/Topfoto
tuationsinthreefundamentalfactors:birthrate,death
rate,andimmigrationoremigration.Whenanyorallof
Figure2.1:Timetosuccessivebillionsinworldpopulation:1800-2050.
thesefactorsdeviatefromzero,thesizeofthe
populationwillchange(GlobalPopulation
Populationinbillions
Totalworldpopulation
Profile2002).Theprimarydrivingforceof
10
2048
populationchange,whetherinanindividual
9
countryorfortheentireworld,ischangein
2028
8
birthanddeathrates.
Worldpopulationisgrowingmoreslowly
thanwasexpected(Figure2.1)asaresultof
aid,familyplanningprograms,andeducationalandeconomicprogramsdirectedat
women.Peoplearealsohealthierandliving
longerthantheydidinthepast;averagelife
expectancyhasincreasedwhilecrudebirth
rateanddeathratearefollowingadownward
trend(Tables2.3,2.4,2.5and2.6).
2013
7
1999
6
1987
5
1974
4
1959
3
1922
2
1
1804
0
1800
37years
13
years
12
years
15
years
14
years
15
years
118years
1850
1900
1950
2000
Mostfuturepopulationgrowthislikelyto
Source:UnitedNations(1995b);U.S.CensusBureau,InternationalProgramsCenter,InternationalDataBaseandunpublishedtables.
Source:GlobalPopulationProfile2002
beincountriesthathaverelativelylargenumbersofyoungpeopleandwherelargefamilies
arestillthenorm.Furthermore,decliningmortalityand
increasedlongevityhaveresultedin,andwillcontinueto
leadto,theexpansionofolderpopulations.Worldwide,
16
20
years
2050
Table2.2–TheTopTenMostPopulousCountries:1950,2002,2050
1950
1.China
1.China
1.India
2.India
2.India
2.China
3.UnitedStates
3.UnitedStates
3.UnitedStates
4.Russia
4.Indonesia
4.Indonesia
5.Japan
5.Brazil
5.Nigeria
6.Indonesia
6.Pakistan
6.Bangladesh
7.Germany
7.Russia
7.Pakistan
8.Brazil
8.Bangladesh
8.Brazil
9.UnitedKingdom
9.Nigeria
9.Congo(Kinshasa)
10.Italy
2002
theaveragelifeexpectancyin1950was46years;in2050,
itisprojectedtobe76years(Hunter2001).
2050
10.Japan
10.Mexico
Whileanincreaseinlifeexpectancyisapositivedevelopment,itpresentsanewsetofchallenges.InEurope,
forexample,wherewomengivebirthtoanaverageof1.4
children,governmentsareconcernedthattherewillbe
toofewworkersinfutureyearstosupportthegrowing
numberofretireesinthepopulation.Anagingpopulationstrainsanation’ssocialsecuritysystemandpension
plans,andputspressureonhealthbudgetsbecauseof
higherhealthcarecostsfortheelderly.Somegovernmentsarealsoconcernedthatashortageofworking-age
individualsmayleadtoincreasedimmigration,andthata
declineinpopulationmaysignalaweakeningofacountry’spoliticalandeconomicclout(Ashford2004).
Source:U.S.CensusBureau,InternationalProgramsCenter,InternationalDataBaseareunpublishedtables.
Table2.3–Medianageforgivenpoints
intimeSource:ESA2003.
Year
Medianage
1970
1975
1980
1985
1990
1995
2000
2005
2010
21.7
22.0
22.7
23.4
24.3
25.3
26.4
27.4
28.4
Oneofthemainreasonsthatworldpopulationhas
grownsorapidlyoverthelast200yearsisthatmortalityrateshavedeclinedfasterthanfertility
Table2.4–Averagelifeexpectancyatbirth-Medium
rates.Improvedsanitation,healthcare,
variantSource:ESA2003.
medicine,shelter,andnutritionhaveall
Period
Bothsexes
Male
Female
combined
ledtodramaticincreasesinlifeexpectancy.
Fertilityrates,ontheotherhand,declined
1970-1975
58.0
56.5
59.5
1975-1980
59.8
58.1
61.5
morerecentlythanmortalityratesdid
1980-1985
61.3
59.4
63.2
(UNEP1999).
1985-1990
1990-1995
1995-2000
2000-2005
2005-2010
62.9
63.8
64.6
65.4
66.3
60.9
61.7
62.5
63.3
64.2
Table2.5–Crudebirthrateper1000
population-MediumvariantSource:ESA2003.
Table2.6–Crudedeathrateper1000
population-MediumvariantSource:ESA2003.
Period
Period
1970-1975
1975-1980
1980-1985
1985-1990
1990-1995
1995-2000
2000-2005
2005-2010
Crudebirthrate
30.9
28.1
27.4
26.8
24.5
22.7
21.3
20.4
1970-1975
1975-1980
1980-1985
1985-1990
1990-1995
1995-2000
2000-2005
2005-2010
Crudedeathrate
11.6
10.9
10.3
9.7
9.5
9.2
9.1
9.0
64.8
65.9
66.9
67.6
68.4
Thereisastrikingparadoxinglobal
populationtrends:formorethantwodecades,manydevelopingcountrieshaveexperiencedarapiddeclineinfertilitywhile
fertilityratesinmosthighlydevelopednationshaveremainedverylow(Figures2.3
and2.4).Yetinthecomingyears,amassive
increaseoftheworldpopulationisalmost
certain(Heilig1996).
TheDemographicTransitionModel
(Figure2.2)showshowacountry’spopulationcanchangeasthecountrydevelops.
However,thismodeldoesnottakeinto
accountmigration.Worldwide,migration
ofpeopleoutofruralareasisaccelerating,
makinginternalandinternational
Credit:EdSimpson/UNEP/PhotoSpin
17
Credit:Unknown/UNEP/Topfoto
Figure2.2:TheDemographicTransitionModelshowshowpopulationgrowthoccurs
naturallyinfourstages.Stage1:Birthrateanddeathratearehigh,limitingboththe
rateofincreaseandtotalpopulation.Stage2:Birthrateremainsrelativelyhighbut
deathratebeginstofall,causingthepopulationtogrowrapidly.Stage3:Declining
birthrateandlowdeathratemaintaincontinuedpopulationgrowth.Stage4:Both
birthrateanddeathratearelow,slowingpopulationgrowth,butleavingalargetotal
population.Source:http://www.geography.learnontheinternet.co.uk/topics/growth
Figure2.3:Childbearingtrendsinmajorworld
regions,1970and2004
Totalfertilityrate(childrenperwoman)
6.7
5.1
5.1
2.6
Africa
1970
5.0
Asia
2.6
2.0 2.0
LatinAmerica North
&Caribbean America
2004
2.2 1.4
Europe
Source:UNPopulationDivision.WorldPopulationProspects:The2002Revision(1970
data),andC.Haub,2004WorldPopulationDataSheet(2004data).
migrationpotentiallyoneofthemost
importantdevelopmentandpolicyissues
ofthiscentury.Themigrationoflabor
geographically,outofruralareas,and
Figure2.4:Differentpatternsoffertility
occupationally,outoffarmjobs,isoneof
decline,1970-2000
themostpervasivefeaturesofagricultural
Childrenperwoman
transformationsandeconomicgrowth.Yet 7
6
inaworldofcompleteandwell-functionBangladesh
India
5
ingmarkets,thereislittleornoeconomic
4
rationaleforpoliciestoreducemigration;
3
themovementoflaboroutofagricultureis 2 Argentina
Thailand
bothaquintessentialfeatureofagricultural 1
0
transformationsandaprerequisitefor
1970 1975 1980
1985
1990
1995 2000
Sources:RegistrarGeneralofIndia;InstitutoNacionaldeEstadística(Argenefficientandbalancedeconomicgrowth
tina);UnitedNationsPopulationDivision;InstituteofPopulationandSocial
Research,MahidolUniversity,Thailand;DemographicandHealthSurveys;and
(TaylorandMartin2002).
PopulationReferenceBureauestimates.
Clearly,humannumberscannotcontinuetoincreaseindefinitely.Themore
peoplethereareandthelongertheylive,
themorecompetitiontherewillbeforthe
Earth’slimitedresources.Unlessallnationsadoptmoresustainablemethodsof
PopulationDensityMap
Population Density
persons per squar
5,000 and higher
2,000 - 4,999
1,000 - 1,999
500 - 999
200 - 499
100 - 199
50 -
99
10 -
49
1-
9
No data
No data
1-9
10 - 49
50 - 99
100 - 199
200 - 499
500 - 999
1,000 1,999
2,000 4,999
5,000 and
higher
Source:http://beta.sedac.ciesin.columbia.edu/
18
GlobalUrbanExtentMap
Themapportraystheboundariesofurbanareaswithdefinedpopulationsof5000personsormore.Source:Modifiedfromhttp://beta.sedac.ciesin.columbia.edu/gpw/global.jsp
productionandconsumption,theplanet’s
carryingcapacitywillbeexceeded(UNEP
1999).
Naturalresourcesarealreadyseverely
limited,andthereisemergingevidence
thatnaturalforcesarealreadystarting
tocontrolhumanpopulationnumbers
CaseStudy:MonitoringRapidUrban
ExpansionofTehran,Iran
1975and2000
TehranislocatedatthefootoftheAlborz
Mountains.Thecityoccupiesthenorthernpart
ofthealluvialTehranPlain,slopingfromthe
mountainstotheflatGreatSaltDesert.Theurbanareaisboundedbymountainstothenorth
andeastmakingitdifficulttodifferentiatethe
urbanareafromthemountainousanddesert
areathatsurroundsTehran.
ThepopulationofTehranhasgrownthreefoldsince1970whenthepopulationwasthree
million.In1987,thecityhadgrowntomore
throughmalnutritionanddisease(Pimenteletal.1999).
Theenvironmentalchallengesthatpeoplenowfaceandmostlikelywillcontinue
tofaceinthefuturewouldbelessdifficult
ifworldpopulationweregrowingvery
slowlyornotatall.Thenumberofpeople
thansevenmillionpeopleandcoveredanarea
of575km2(230squaremiles).Todaythecity
hasninemillionresidents.
TherapidexpansionofTehran,aswellasits
sharppopulationgrowthinrecentdecades,has
hadmanyadverseimpactsontheenvironment.
Airandwaterpollutionaremajorproblemsin
thecity.Urbanareasarereplacingfarmsand
waterresources.Amajorconcernisitslocation
onarecognizedzoneofactivefaultingwitha
modesttohighseismicrisk.Recentplanning
andconstructiontechniquesaredesignedto
improvetheresistancetoamajorearthquake
thatcouldthreatenthecity.
ontheEarthandtherateatwhichthat
numberincreases(Table2.7)dramatically
impacttheavailabilityofwater,soil,arableland,minerals,fuels,andmanyother
naturalresourcesworldwide.Accesstoand
useoffamilyplanningservicescanhelp
lowerfertilityratesanddelaychild-bearing
Credit:SamanSalariSharif/UNEP/UNEP-GRIDGeneva
19
Credit:EdSimpson/UNEP/PhotoSpin
PopulationDensity
(people/km2)
High(>100)
Medium(25–100)
Low(<25)
Water
LakeVictoria,Kenya
PopulationgrowtharoundLakeVictoria,
Kenya,issignificantlyhigherthanintherest
ofAfricabecauseofthewealthofnatural
resourcesandeconomicbenefitsthelakeregionoffers.Notetheincreaseinpopulation
ina100-km(62miles)bufferzonearound
LakeVictoriabetween1960and2000.Duringeachdecade,populationgrowthwithin
thiszoneoutpacedthecontinentalaverage.
Source:UNEP/GRID-SiouxFalls
years,years,therebyhelpingtoslowpopulationgrowth.Comprehensivepopulation
policiesareanessentialelementinaworld
Table2.7–WorldVitalEventsPerTimeUnit:2004
(Figuresmaynotaddtototalsduetorounding)
Timeunit
Births
Natural
Death
Population
Increase
Year
Month
Day
Hour
Minute
Second
29358036
10779836
353437
14727
245
4.1
56150533
4679211
153417
6392
107
1.8
73207503
6100625
200021
8334
139
2.3
Source:http://www.census.gov/cgi-bin/ipc/pcwe
developmentstrategythatcombinesaccess
toreproductivehealthservices,education
andeconomicopportunities,improved
energyandnaturalresourcetechnologies,
andmorereasonablemodelsofconsumptionandwhatconstitutes“thegoodlife.”
Suchastrategyhasthepotentialtobring
humanityintoanenduringbalancewith
theenvironmentandthenaturalresources
uponwhichpeoplewillalwaysdepend
(PopulationFactSheet2000).
Inadditiontotheoverallglobalincreasesinpopulation,thegeographicdistributionofhumanpopulationunderwent
Figure2.5:Populationchangeinthe20thcentury
Source:http://www.bioone.org/pdfserv/i0044-7447-031-03-0251.pdf
Population density
(people per sq km)
0 – 0.5
0.5 – 10
10 – 100
100 – 250
250 – 500
500 – 1000
greater than 1000
20
massivechangesduringthe20thcentury
(Figure2.5).Forexample,between1900
and1990,thepopulationofnorthern
SouthAmericaincreasedby214million,or
681percent,comparedtotheglobalaveragepopulationincreaseof3700million,
or236percent(Ramankuttyand
Olejniczak2002).
2.2 Culture
Cultureencompassesthecustomarybeliefs,socialforms,
andmaterialtraitsofaracial,religious,orsocialgroup.
Cultureincludesthesetofvaluesandinstitutionsthat
enableasocietytodevelopandmaintainitsidentity.
Culturalsignaturesdifferaroundtheglobeandoften
holdtoverydifferentidealsandideas,suchastherole
ofeconomicsasanintegratingsystemofvaluesorthe
importanceoftechnologyandtechnologicalchangeas
springboardsforhumanprogress.Differentculturesalso
differintheirconceptsofjusticeandfairnessandtheir
beliefsabouttherelationshipbetweenpeopleandthe
naturalandspiritualworld(UNEP2002a).
Manyofthesedifferencesaredisappearingascultures
worldwidebecomeincreasinglyhomogeneous.Major
stepsinthisdirectionoccurredinthefifteenthcentury
withEuropeanexplorationandcolonizationandinthe
nineteenthcenturywiththeIndustrialRevolution.In
recentdecadesthecreationoftheEuropeanUnionand
spreadofglobalizationhasloweredmanyinternational
barriersandconcurrentlyimpactedculturaldiversity.
FollowingthecollapseoftheEasternBlocin1989,capitalismbecamemorepervasiveandlessnationallylimited.
Globally,world-spanningcommunicationnetworks,
andinexpensiveairtravelhavereducedthecostsof
cross-culturalconnectionsofallkinds,boostingtelevision,tourism,andemigrationtonewlevels.Global
financialintegrationhasproceededatafuriouspace,
alongwiththeinternationalflowofgoodsandservices
ascountriesbecomeincreasinglydependentonone
Credit:Unknown/UNEP/Bigfoto
TheWorld’sBioculturalDiversity.People,LanguagesandEcosystems
Source:Terralingua,UNESCO,andWWF2003
21
LanguagesoftheWorld
Source:http://highered.mcgraw-hill.com/site/dl/free/007248179x/35299/map12.pdf
anotherforfoodandbasiccommodities
(Wilk2000).Explosivedevelopmentof
electronicmediahasintensifiedcultural
homogenizationbypromotingtheideals
ofahandfulofculturesoverthoseofmany
others(GaryandRubino2001).Thetechnologicalexpansionofthemedia,inparticulartheInternet,isbringingdifferent
culturesandcivilisationsevercloser;while
thisincreasesthepossibilityofdialogue,it
canalsobeperceivedasathreattoculturaldiversity,Inshort,currentglobalization
oftradeandmassculture,togetherwith
unprecedenteddemandforconsumer
goods,hassignificantlyimpactedindigenousculturesaroundtheglobe.
Everycivilisationandcultureisuniqu
andirreplaceable,inthatallcultures
andcivilisationsarepartofthecommon
legacyofhumankind(UN2000).Inmany
partsoftheworld,Englishhasbecome
thedominantlanguage,havingdisplaced
nativetonguesanddialects.Accordingto
arecentUNEPreport(UNEP,2001)there
were5000to7000spokenlanguagesin
theworldwith4000to5000oftheseclassifiedasindigenous.Thirty-twopercent
Source:Modifiedfromhttp://www.neiu.edu/~ejhowens/104/6/cultur.gif
22
Table2.8–Themostcommonlanguagesintheworld
Language
1.
2.
3.
4.
5.
6.
7.
8.
9.
10.
11.
12.
13.
14.
15.
MandarinChinese
874000000
Hindi(India)
366000000
English
341000000
Spanish
322-358000000
Bengali
207000000
(IndiaandBangladesh)
Portuguese
176000000
Russian
167000000
Japanese
125000000
German(standard)
100000000
Korean
78000000
French
77000000
WuChinese
77000000
Javanese
75000000
YueChinese
71000000
Telegu(India)
69000000
Approximatenumber
Countrieswith
ofnativespeakers substantialnumbers
(intheyear2000)
ofnativespeakers
16
17
104
43
9
33
30
26
40
31
53
1
4
20
7
Note:Thesestatisticsareonlyroughapproximationsinmostcases.
(Source:TheWorldAlmanacandBookofFacts,2003)
Credit:Unknown/UNEP/Bigfoto
oftheworld’sspokenlanguagesarefoundinAsia,30percent
inAfrica,19percentinthePacific,15percentintheAmericas,andthreepercentinEurope.Morethan2500languages
areindangerofimmediateextinction,while234havealready
diedoutandmanymorewerelosingtheirconnectiontothe
modernworld.Someresearchersestimatethatoverthenext
century90percentoftheworld’slanguageswillhavebecome
extinctorvirtuallyextinct.Morethan350languagesalready
havefewerthan50speakers(Table2.8).Suchrarelanguages
aremorelikelytodeclineordisappearthanthosethatare
morecommon(Sutherland2003).Thedisappearanceofany
languagerepresentsanirreparablelossfortheheritageofall
humankind(Wurm1970).Thelosshasbeenlikenedtothe
extinctionofaspecies—anunfortunateculturalanalogtothe
alarmingeventsnowoccuringinthebiologicalworld.Infact,
ReligionsoftheWorld
Source:http://highered.mcgraw-hill.com/site/dl/free/007248179x/35299/map11.pdf
23
Anaturalwonderformedbynaturalprocesses,Rainbow
Bridge(farleft)straddlesatributaryoftheColorado
RiverinsouthernUtahintheUnitedStates.Twocontemporarybridges,onefromSydney,Australia(left),
andtheotherfromLondon,England(belowleft),echo
thenaturalformofRainbowBridge,butaretheobvious
byproductsofmodernculture.
Credit:W.R.Hansen/UNEP/USGS
Credit:Unknown/UNEP/Bigfoto
Credit:Unknown/UNEP/Bigfoto
thenumberof“living”languagesspoken
ontheEarthisdwindlingfasterthanthe
planet’sbiodiversity.
Cultureisanaspectandameansof
development.Muchhasbeensaidabout
theexpansionofWesternculturetothe
detrimentofothers.Itisclearthatmany
individualsaspiretoWesternlifestyles,
whileothersassociateWesterncultural
valueswithselfishindividualismandexcessiveconsumption.ThespreadofWestern
cultureisbothacauseandaneffectof
economicglobalization,aidedbythe
far-reachingpenetrationofinformation
technologiesandelectronicmedia.Atthe
sametime,therehavebeennationalistand
religiousreactionsagainstthatculture,
sometimesresultinginterroristactivities
andinopenwarfarewithinorbetweennations(UNEP2002a).
TheWorldhassome6000communities.Theinternationalmigrationrateis
growingeveryyearandthenumberofmigrantshasdoubledsincethe1970s.While
thereasonsformigrationvary,itissafeto
saythatweliveinanincreasinglyheterogeneoussociety.Differencenaturallyleadsto
diversityofvision,values,beliefs,practices
andexpression,whichalldeserveequalrespectanddignity(UNESCO2003).While
highlightingtheroleofcultureindevelopment,thereisalsoaneedtoemphasize
theroleofcultureinpromotingpeace
(UNESCOn.d).
Justasbiodiversityenrichesournatural
environmentandisessentialforitsprotection,culturaldiversityisatreasureof
humanityandaprerequisiteforhuman
development(UN2000).CulturalDiversity
presupposesrespectoffundamental
freedoms,namelyfreedomofthought,
conscienceandreligion,freedomofopinionandexpression,andfreedomtoparticipateintheculturallifeofone’schoice.
CulturalDiversityisnotjustanaturalfact
thatweneedsimplyrecognizeandrespect.
Itisaboutpluralityofknowledge,wisdom
andenergy,allofwhichcontributeto
improvingandmovingtheWorldforward
(UNESCOn.d.).
Varietyinallaspectsoflifehasbeen
asourceofwonderandcelebrationfor
countlesscenturies,andthelossofthat
varietyisanunfortunateprospect(Gary
andRubino2001).
Credit:EdSimpson/UNEP/PhotoSpin
24
2.3 Land Use and
Degradation
Growingcrops,clearingland,plantingtrees,drainingawetland—
theseandmanyotheractivitiesfallintothebroadcategoryofland
use,orhowpeopleuseland.Land-useintensityistheextentto
whichlandisused.Itisanindicationoftheamountanddegreeof
developmentinanarea,andareflectionoftheeffectsgenerated
bythatdevelopment(PlanningDepartment2001).
Asameasureofactivity,land-useintensitycanrangefromvery
low(forexample,apristinewildernessarea)tointermediate(a
managedforestecosystem)toveryhigh(urbanandindustrial
settings)(LebelandSteffen1998).Fromaglobalchangeperspective(Figure2.6),land-useintensityisanimportantcharacteristic
inassessingchangeanditsimpact(Berkaetal.1995).Land-use
intensityisdeterminedbythespatialrequirementsofaland-use
activity,relationshiptoopenspace,requirementsforinfrastructure(transportationroutes,water,sewer,electricity,andcommunications),andenvironmentalimpact.Parametersformeasuring
land-useintensitytypicallyinclude:
•typeofland-useactivity,suchasagriculture,grazing,wood
production,orresidential,commercialorindustrialusage,
•durationofuse,
•numberofpeople,animals,plants,structures,ormachines
thatoccupythelandduringagivenperiod,and
•amountoflandinvolved.
Credit:AndreLouzas/UNEP/Topfoto
Figure2.6:Thisseriesofillustrationsdepictsgloballand-usechange,particularly
theexpansionofcroplandandgrazingland,between1700and1990.Credit:Klein
Goldewijk,K.,2001.Source:NASA2002,http://www.gsfc.nasa.gov/topstory/20020926landcover.
html
tropicalevergreen/deciduousforest
savana
grasslandandsteppe
intensiveagriculture
desert
openshrubland
temperatedeciduousforest
temperateneedle-leafevergreenforest
marginalcroplandusedforgrazing
25
Figure2.7:ConceptualframeworkoftheAgro-EcologicalZonesmethodology
Alsoimportantinassessingland-use
intensityistoexaminetherelativeimperviousnessofthelandscape.Impervious
surfaces,suchaspavedroads,inhibitor
entirelyblocktheabsorptionofwaterby
underlyingsoil(Forneyetal.2001).Once
pavedorotherwisemadeimpervious,land
isnoteasilyreclaimed.Asenvironmentalist
RupertCutlernoted(Brown2001),
“Asphaltistheland’slastcrop.”
Land-useintensitytrendsareusually
expressedthroughchangesininputs,
management,ornumberofharvestsovera
givenperiodoftime.Onlychangeswithin
thesameland-usecategoryandonthe
samearea(changeofintensity)—asopposedtochangesfromonetypeofland
usetoanother(forexample,forestto
cropland)—aretakenintoaccountwhen
assessingtrends(vanLyndenetal.n.d.;
FAO2002).
TheAgro-EcologicalZones(AEZ)
methodology(Figure2.7)isasystemdevelopedbytheFoodandAgricultureOrganizationoftheUnitedNations(FAO)with
thecollaborationoftheInternationalInstituteforAppliedSystemsAnalysis(IIASA),
thatenablesrationallanduseplanningon
R
A
Rio C
an d ei a s
R
thebasisofaninventoryoflandresources
andevaluationofbiophysicallimitations
andpotentials.Thismethodologyutilizes
alandresourcesinventorytoassess,for
Z
I
specifiedmanagementconditionsand
levelsofinputs,allfeasibleagricultural
land-useoptionsandtoquantifyexpected
productionofcroppingactivitiesrelevant
L
ari
R i o Ja m
B
Source:FAO2000,http://www.fao.org/ag/agl/agll/gaez/index.htm
A
Rio C
an d e i a s
B
Karitiana
Indigenous
Area
ari
R i o Ja m
ana
nous
a
Z
I
Ariquemmes
L
Ariquemmes
Rondônia
Rondônia
São Cruz
São Cruz
São Joao
Rio Branco
São Joao
Rio Branco
Figure2.8:Asatelliteimagerevealsatypical“feather”or“fishbone”patternofdeforestationinBrazil.Thepatternfollows
theconstructionofanewroadthroughtherainforest.Roads
provideeasyaccessformechanicizedloggingtoclearcutforestsections.Clearcutsectionscanthenbeturnedintoagriculturalfieldsasroadsprovideeasyaccesstolocalmarkets.
Joao Filipe
Uru-Eu-Wau-Wau
Indigenous
Area
0
26
10
Ki l om e t e r s
Pacaás Novos
National Park
Source:UNEP/GRID–SiouxFalls
19Sep2001
Credit:XintianPan/UNEP/Topfoto
inthespecificagro-ecologicalcontext.
Thecharacterizationoflandresources
includescomponentsofclimate,soilsand
landform,whicharebasicforthesupplyof
water,energy,nutrientsandphysicalsupporttoplants(FAO2000).
Scientistsestimatethatbetweenonethirdandone-halfoftheEarth’sland
surfacehasbeentransformedbyhuman
activities(Figure2.9)(Herringn.d.).The
activitythathashadthegreatestimpacton
thegloballandscapeisagriculture.Twelve
Worldwide,theeffectpeoplearehaving percentoftheworld’slandsurface—an
areaequivalenttothatoftheSouthAmeriontheEarthissubstantialandgrowing.
cancontinent—isunderpermanent
Satelliteimagesrevealinstartlingdetail
cultivation(RamankuttyandFoley1999;
thesignsofhumanimpactonthelandDevitt2001).
scape.Fromtheherringbonepatterns
ofdeforestationetchedintoonce-undisOverthenext30years,theannualrate
turbedrainforests(Figure2.8)tothe
ofgrowthinglobalcropproductionisexpatchworkpatternsofagriculturalfields
pectedtodecrease.However,theFoodand
AgricultureOrganizationoftheUnited
andconcretesplotchesofurbansprawl,
Nationspredictsthatproductionwillstill
theevidencethatpeoplehavebecomea
exceeddemand,despitetheworld’sgrowpowerfulforcecapableofreshapingthe
Earth’senvironmentiseverywhere.
ingpopulation.By2030,75percentofthe
GlobalSoilDegradationMap
projectedglobalcropproductionwilloccurindevelopingcountries,comparedto
50percentintheearly1960s.Increasesin
productionwillbeachievedbyimproving
plantyieldsandthroughmoreintensive
land-useactivities,includingmulti-croppingorhigh-croppingintensities(UCS
2004).Inlightoftheseprojections,continuedsupportofagriculturalresearchand
policiesindevelopingcountriesisvital.
Nearlyone-thirdoftheworld’scropland—1500millionhectares—hasbeen
abandonedduringthepast40years
becauseerosionhasmadeitunproductive
(Pimenteletal.1995).Restoringsoillost
byerosionisaslowprocess;ittakesroughly500yearsforamere2.5cm(1inch)
ofsoiltoformunderagricultural
Source:http://www.isric.nl/
Source:http://www.isric.nl/
27
27
Figure2.9:Human-inducedlanddegradation(severeandverysevere)aspercentageoftotallandarea
30
Area(millionsq.km)
25
Totalhuman
inducedland
degradation
20
15
Totalland
10
5
0
SubNorth
Saharan Africa
Africa andNear
East
North
Asia,
eastof
Urals
North Europe
Asiaand South
America
Pacific
and
Central
America
Source:WorldAtlasofDesertification(UNEP1992)
conditions(Pimenteletal.1996).Thusthe
approachtoreplacingerodedagricultural
landstypicallyhasbeentoclearmoreand
moreareasofgrasslandorforestandconvertthemtocropland.Theever-growing
needforagriculturallandaccountsfor60
to80percentoftheworld’sdeforestation
(Figure2.9).
Despitesuch“replacement”strategies,
theamountofavailablecropland
worldwidehasdeclinedto0.27hectare
(0.67acres)perperson(Pimenteletal.
1996).Itispossibletofeedoneadulton
aplantdietgrownonabout0.2hectares
(0.5acres)ofland(Knee2003)—and
thisland-per-personminimumisroughly
whatwillbeavailablewhenworld
populationreaches8000million—but
onlyifcropyieldsnowbeingachieved
indevelopedcountriesareachieved
worldwide.Todosorequiresthatmost
countries’inputsoffertilizer,andprobably
pesticides,risetomatchthoseofNorth
AmericaandEurope.Furthermore,any
mechanizationofcropproductionwill
entailadditionalenergyconsumption.
Increasedmechanizationislikelygiven
themassmigrationfromruralareasto
citiescurrentlyunderwayonallcontinents.
Whileagricultureaccountsforonlyabout
twopercentofenergyconsumptionin
NorthAmericaandEurope,itaccounts
forroughlytenpercentofenergy
consumptionintherestoftheworld
(Knee2003).
associatedhumanmalnutrition.Political
unrest,economicinsecurity,andunequal
fooddistributionpatternsalsocontribute
tofoodshortagesworldwide(Pimentelet
al.1996).
Inadditiontoagriculture,theglobal
trendtowardurbanizationisanotherkey
factorbringingchangetothelandscape.
Historically,forestsandgrasslandshave
beenconvertedtocropland.Increasingly,
croplandisbeingconvertedtourbanareas
(RamankuttyandFoley1999;Devitt2001).
Millionsofhectaresofcroplandinthe
industrialworldhavebeenpavedtocreate
roadsandparkinglots.Theaveragecarrequires0.07hectares(0.17acres)ofpaved
landforroadsandparkingspace
(Brown2001).
Iffarmersworldwidefailtomeetthe
challengeofincreasingyieldsonexisting
cropland,ortheycannotaccessthetools
necessarytoachieveincreasedyields,the
onlyalternativewillbetocleartheworld’s
remainingforestsandgrasslands(Green
2001).Yetindicationsarethattheworld
doesnothaveenoughforeststofulfillall
thecurrentandfuturedemandsbeing
placedonthem(Nilsson1996).
Asnaturalforestsareexhaustedor
comeunderprotection,thedemandfor
woodandwoodproductswillbeincreasinglysatisfiedbytreefarms.Between1980
and1995,forestplantationsindeveloped
countriesincreasedfrom45-60million
Theshortageofcropland,togetherwith
hectares(111-147millionacres)to80-100
fallingproductivity,isasignificantfactor
millionhectares(198-247millionacres).
contributingtoglobalfoodshortagesand
Credit:ChoosakKhemtai/UNEP/Topfoto
28
Credit:PaiboonPatta/UNEP/Topfoto
Inthedevelopingworld,theareainforest
plantationsdoubledfromroughly40milliontoabout81millionhectares(99-200
millionacres)overthesameperiod.More
than80percentofforestplantationsin
thedevelopingworldarefoundinAsia,
wheredemandforpaperandotherwood
productscontinuestogrowrapidly.Forestplantationsnowcovermorethan187
millionhectares(462millionacres)worldwide.Thataccountsforlessthanfive
percentoftheEarth’stotalforestedarea,
but20percentofcurrentglobalwoodproduction(Larsen2003).
LandDegradation
andDesertification
Bythebeginningofthetwenty-firstcentury,unprecedentedglobalenvironmental
changeshadreachedsufficientproportionstoimpingeuponhumanhealth—simultaneouslyandofteninteractively.These
changesincludetheprocessesofland
degradationanddesertification(Menne
andBerollini2000).
Landdegradationisthedeclineinthe
potentialoflandresourcestomeethumaneconomic,social,andenvironmental
functionsneeds(AfricaMountainForum
n.d.).Desertificationissoildegradationin
aridregions,oftentosuchanextentthat
itisimpossibletomakethesoilproductiveagain(Table2.9).Desertificationis
theresultofcomplexinteractionsbetween
unpredictableclimaticvariationsand
unsustainablelandusepracticesbycommunitieswho,intheirstruggletosurvive,
overexploitagricultural,forest,andwater
resources(CIDA2001).
(Watsonetal.1998).Theconsequencesof
desertificationinclude(UNEP2002a):
•reductionoftheland’snaturalresiliencetorecoverfromclimaticdisturbances;
Over3600millionhectares(8896millionacres)—25percentoftheEarth’sland
area—areaffectedbylanddegradation.
Desertificationoccurstosomeextenton
30percentofirrigatedlands,47percent
ofrain-fedagriculturallands,and73per
centofrangelands(Figure2.10).Annually,
anestimated1.5to2.5millionhectares
(3.7to6millionacres)ofirrigatedland,
3.5to4.0millionhectares(8.6to9millionacres)ofrain-fedagriculturalland,
andabout35millionhectares(86million
acres)ofrangelandloseallorpartoftheir
productivityduetolanddegradationprocesses(Watsonetal.1998).
Desertificationanddroughtareproblemsofglobaldimensionthatdirectly
affectmorethan900millionpeoplein
100countries,someofwhichareamong
theleastdevelopednationsintheworld
•reductionofsoilproductivity;
•damagedvegetationcover,suchthat
edibleplantsareeasilyreplacedby
non-edibleones;
•increaseddownstreamflooding,reducedwaterquality,sedimentationin
riversandlakes,andsiltationofreservoirsandnavigationchannels;
•aggravatedhealthproblemsdueto
wind-blowndust,includingeyeinfections,respiratoryillnesses,allergies,
andmentalstress;
•underminedfoodproduction;and
•lossoflivelihoodsforcingaffected
peopletomigrate.
Desertificationresultsfrommismanagementoflandandthusdealswithtwo
interlocking,complexsystems:thenatural
Table2.9–Degreeofsoildegradationbysubcontinentalregions(percentoftotalarea)
None
Light
Africa
83
6
Moderate
6
4
0.2
Asia
82
7
5
3
<0.1
Australiasia
88
11
0.2
<0.1
Europe
77
6
0.5
15
Strong
1
Extreme
0.3
NorthAmerica
93
1
5
1
0
SouthAmerica
86
6
6
1
0
World:
Percentage
85
Area(‘000km2)110483
6
7490
7
9106
2
2956
<0.1
92
Source:WorldAtlasofDesertification(UNEP1992)
29
Credit:RickCollins/UNEP/Topfoto
ecosystemandthehumansocialsystem
(Eswaranetal.1998).Whilemuchdesertificationisattributedtopoorland-usepractices,hotteranddrierconditionsbrought
aboutbypotentialglobalwarmingwould
extendtheareapronetodesertification
northwardstoencompassareascurrently
notatrisk.Inaddition,therateofdesertificationwouldincreaseduetoincreases
inerosion,salinization,firehazard,and
reductionsinsoilquality.Asaresult,the
processofdesertificationislikelytobecomeirreversible(Karasn.d.).
Worldwide,anestimated6to27million
hectares(15to67millionacres)ofland
arelosteachyeartodesertification.Seventypercentoftheworld’sdrylandisdegradedenoughtobevulnerabletodesertification(Anon2002).Theamountofland
susceptibletodesertification(areasknown
astensionzones)alsoisincreasing.Currently,7.1millionkm2(2.7millionsquare
miles)oflandfacelowriskofhuman-induceddesertification,8.6millionkm2
(3.4millionsquaremiles)areatmoderate
risk,15.6millionkm2(6.2millionsquare
miles)areathighrisk,and11.9million
km2(4.6millionsquaremiles)areatvery
highrisk.Tensionzonesresultfrom:
•excessiveandcontinuoussoilerosion
resultingfromoveruseandimproper
useoflands,especiallymarginaland
slopinglands;
•nutrientdepletionand/orsoilacidificationduetoinadequatereplenishmentofnutrientsorsoilpollution
fromexcessiveuseoforganicand
inorganicagrichemicals;
•reducedwater-holdingcapacityof
soilsduetoreducedsoilvolumeand
reducedorganicmattercontent,both
ofwhichareaconsequenceoferosion
andreducedinfiltrationduetocrustingandcompaction;
•salinizationandwater-loggingfrom
over-irrigationwithoutadequate
drainage;and
•unavailabilityofwaterstemmingfrom
decreasedsupplyofaquifersand
drainagebodies.
Thefollowingnegativeeffectsarehighestinthetensionzones(Eswaranetal.
1998):
•systematicreductionincropperformance,leadingtofailureinrain-fed
andirrigatedsystems;
•reductioninlandcoverandbiomass
productioninrangelands,withan
accompanyingreductioninqualityof
feedforlivestock;
Figure2.10:Soilsareclassifiedaccordingtotheproportionsofdifferentsizedparticlestheycontain.
Asseeninthisfigure,thelargestpercentageofworldlandareaunsuitableforagricultureislandthat
istoodry.Source:FAO2000,http://www.fao.org/desertification/default.asp?lang=en
30
•reductionofavailablewoodyplants
forfuelandincreaseddistancesto
harvestthem;
Thissub-sceneofanASTERsatelliteimageshows
sanddunescoveringanarearoughly12kmx15km
(8x9miles)intheTharDesertofnorthwestern
IndiaandeasternPakistan.Theduneshereshift
constantly,takingonnewshapes.Approximately800
km(497miles)longand490km(305miles)wide,
theTharDesertisboundedonthesouthbyasalt
marshknownastheRannofKutch,andonthewest
bytheIndusRiverplain.Thedesert’sterrainisprimarilyrollingsandhills,withscatteredoutcroppings
ofshrubandrock.Source:NASA2004,http://asterweb.jpl.
nasa.gov/gallery/gallery.htm?name=Thar
•significantreductioninwaterfrom
overlandflowsoraquifersandaconcomitantreductioninwaterquality;
•encroachmentofsandandcropdamagebysand-blastingandwinderosion;
and
•increasedgullyandsheeterosionby
torrentialrain.
Ultimately,desertificationprocessesimpactabout2600millionpeople,or44per
centoftheworld’spopulation(Eswaran
etal.1998).
CaseStudy:Mt.Kenya–Diversity
inEcosystems
ChristianLambrechts
MountKenyaislocatedon
theequator180kilometres
northofNairobi.Itisasolitarymountainofvolcanic
Credit:NASA/GSFC/METI/ERSDAC/JAROS,
andU.S./JapanASTERScienceTeam.
TanaRiverwhere50percentofKenya’stotal
2002,astudywascarriedouttoassesstheeffec-
electricityoutputisgenerated.
tivenessofthenewmanagementpracticesput
Forestconservationinitiative
inplacein2000.Thestudyrevealedsignificant
Followinga1999aerialsurvey,theentireforest
improvementinthestateofconservationof
beltofMountKenyawasgazettedasNational
theforests.
Reserveandplacedunderthemanagementof
KenyaWildlifeServicesintheyear2000.In
originwiththebasediameterofabout120km(75
miles).Itsbroadconeshape
reachesanaltitudeof5199m(17057ft)with
deeplyincisedU-shapedvalleysintheupper
parts.Forestvegetationcoversthemajorpart
ofthemountain,withatotalareaaround
220000hectares(548574acres).Theforests
arecriticalandinvaluablenationalassetsthat
mustbeprotected.
Highdiversityinecosystemsandspecies
Thewiderangeinaltitudeclines—from1200
to3400m(3900to11000ft)—andrainfall
clinesfrom—from900mm/year(35in/year)
inthenorthto2300mm/year(91in/year)in
thesouth-easternslopes—contributestothe
highlydiversemosaicpatternsofMountKenya
forests.MountKenyaaddsvaluetothenationbyprovidingtourismpotentialandlocal
culturalandeconomicbenefits.Italsoprovidesimportantenvironmentalservicestothe
nationsuchasawatercatchmentareaofthe
Forestisshowninredontheseimages.Notethechangesinforestcoverintheboxes.
Source:UNEP/GRID–Nairobi
31
2.4 Ecoregions
and Ecosystems
Anecosystemisanorganiccommunityofplantsandanimalsviewedwithinitsphysicalenvironment(habitat);
theecosystemresultsfromtheinteractionbetweensoil
andclimate.Itisadynamiccomplexofplant,animal,
andmicroorganismcommunitiesandtheirnon-living
environmentinteractingasafunctionalunit(UNEPWCMC2003).
Anecoregionisacartographicaldelineationofa
relativelylargeunitoflandorwatercontainingageographicallydistinctassemblageofspecies,naturalcommunities,andenvironmentalconditions.Anecoregion
isoftendefinedbysimilarityofclimate,landform,soil,
surfaceform,potentialnaturalvegetation,hydrology,
andotherecologicallyrelevantvariables.Ecoregions
containmultiplelandscapeswithdifferentspatialpatternsofecosystems.
Theecoregionconceptisoneofthemostimportant
inlandscapeecology,bothformanagementandunderstanding(HargroveandHoffman1999).Ecoregion
classificationsarebasedonparticularenvironmental
conditionsanddesignedforspecificpurposes,andno
singlesetofecoregionswouldbeappropriateforall
potentialuses(Wikipedian.d.).
Theenvironmentofanecoregionintermsof
climate,resourceendowments,andsocioeconomic
Credit:JohnRJones/UNEP/Topfoto
Tropical rainforest
Tropical moist
deciduous forest
Tropical dry forest
32
Tropical shrubland
Subtropical humid forest
Temperate oceanic forest
Boreal coniferous forest
Polar
Tropical desert
Subtropical dry forest
Temperate continental forest
Boreal tundra woodland
Water
Tropical mountain
Subtropical steppe
Temperate steppe/prairie
Boreal mountain
No Data
Subtropical desert
Temperate desert
Subtropical mountain
Source:USGSNationalCenterforEROS
Credit:PhilipDeMancz/UNEP/Topfoto
conditionsishomogeneous.Specificadvantagesofusinganecoregionapproach
forplanninganddecision-makinginclude:
•easieridentificationofproductioncapabilitiesandconstraints;
•bettertargetingofprospective
technologies;
•improvedassessmentofresponsesto
newtechnologies;and
•wideradoptionandlargerimpactof
researchoutputs(Saxenaetal.2001).
Table2.10–Lossofbiodiversityfrom2000to2003—expressedaschangesinspecies
numbers—inanimalsandplantsclassifiedascriticallyendangered,endangered,and
vulnerable
CriticallyEndangered
Endangered
Vulnerable
Group
2000 2002 2003 2000 2002 2003 2000
2002 2003
Mammals
Birds
Reptiles
Amphibians
Fishes
Insects
Mollusks
Plants
180
181
184
182
182
182
56
55
57
25
30
30
156
157
162
45
46
46
222
222
250
1014 1046 1276
340
321
74
38
144
118
237
1266
339
326
79
37
143
118
236
1291
337
331
78
37
144
118
243
1634
610
680
161
83
452
392
479
3311
617
684
159
90
442
393
481
3377
609
681
158
90
444
389
474
3864
Source:http://www.redlist.org/info/tables/table2.html
Trends
Anincreaseinaverageglobaltemperaturehasthepotentialtobringabout
dramaticchangeinecosystems.Some
speciesmaybeforcedoutoftheirhabitats
(possiblytoextinction)becauseofchangingconditions.Otherspeciesmayflourish
andspread.Few,ifany,terrestrialecoregionsontheEarthareexpectedtoremain
unaffectedbysignificantglobalwarming.
Since1970,therehasbeena30
percentdeclineintheworld’sliving
thingsandthedownwardtrendiscontinuingatonepercentormoreperyear(Collins2000;UNEP1997).Table2.10shows
anincreaseinthenumberofendangered
andvulnerablespeciesbetweentheyears
2000–2003.Modificationoflandscapes,
lossofnativespecies,introductionof
exoticspecies,monoculture-focusedagriculture,soilenhancement,irrigation,and
landdegradationhavealltendedto“simplify”ecosystems,leadingtoareduction
inbiodiversity.Inaquaticenvironments,
eutrophicationandhabitatdestruction
havehadasimilareffect(Tilmanetal.
2001).Asecosystemsbecomesimpler,so
doecoregions.
Ecoregionandecosystemfragmentationalsocontributestoadeclineinbiodiversityandthreatensmanyspecies.Globally,overhalfofthetemperatebroadleaf
andmixedforestsandnearlyonequarter
ofthetropicalrainforestshavebeenfragmentedorremoved(Wadeetal.2003).
33
Impacts
Simplificationofecosystemsandecoregionsresultsinspeciesextinctionsand
alossofnaturalresources(Tilmanetal.
2001).Climatechangeandthewayin
whichecologicalcommunitiesrespondto
ithaveenormousconservationimplications.Theseincludedevelopingawareness
ofthetransienceofnativerangesand
plantassociationsandthesignificanceof
populationdeclinesandincreases,aswell
astheneedtodeveloptargetsandreferencesforrestoration,andstrategiesfor
dealingwithglobalwarming(Millar2003).
Forexample,changesinthepotentialdistributionoftreeandshrubtaxainNorth
Americainresponsetoprojectedclimate
changeareexpectedtobefar-reaching
andcomplex;growingrangesforvarious
specieswillshiftnotonlynorthwardand
upwardinelevationbutinalldirections
(Shaferetal.2001).Somemodelspredict
thatmorethan80percentoftheworld’s
Credit:RonLevy/UNEP/Topfoto
ecoregionswillsufferextinctionsasa
resultofglobalwarming(Malcolmetal.
2002).Ecoregionsexpectedtobemost
dramaticallyalteredbyclimatechange
includetheborealforestsoftheNorth-
ernHemisphere,thefynbosofSouthern
Africa,andtheTerai-Duarsavannaand
grasslandsofnortheasternIndia(Malcolm
etal.2002).
Credit:GaryWilson/UNEP/NRCS
34
2.5 Biodiversity,
Invasive Species,
and
Protected Areas
Biologicaldiversity,or“biodiversity,”referstothe
varietyoflifeontheEarthinallitsforms.There
arethreelevelsofbiodiversity:biodiversityofa
landscapeorecosystem,speciesbiodiversity,and
geneticbiodiversity(IUCN,UNEP,andWWF
1991).Thesethreelevelsareintimatelyconnected.
Forexample,geneticdiversityisoftenthekeyto
survivalforaspecies,equippingitwiththenecessaryresourcestoadapttochangingenvironmental
conditions.Speciesdiversity,inturn,istypicallya
measureofecosystemhealth(Rosenzweig1999).
Wehavejustbeguntoidentifyandfullyunderstandthediverselivingthingsthatcurrently
inhabittheEarth.Scientistshavediscoveredand
describedroughly1.75millionspeciestodate.
Thatnumberisexpectedtoincreasesubstantially
whenallmarineorganisms,arthropods,bacteria,
andvirusesareeventuallyaddedtothelist.Tragically,however,humansaredestroyingthisgreat
diversityatanalarmingrate.Ratesofhuman-inducedspeciesextinctionareestimatedtobe50to
100timesthenaturalbackgroundrate;thiscould
Credit:GydeLund/UNEP
Credit:WilliamM.Ciesla/UNEP/Invasive.org
35
increaseto1000to10000timesthenaturalrateinthenext25years(Lundetal.
2003;Pellew1996).
Whyaresomanyspeciesbecoming
extinct?Humanactivitiesoverthelast
threecenturieshavesignificantlytransformedtheEarth’senvironment,primarily
throughtheconversionofnaturalecosystemstoagriculture(RamankuttyandFoley
1999).Itisestimatedthatcroplandexpandedfrom3-4millionkm2(1.2-1.5millionsquaremiles)in1700to15-18million
km2(5.8-6.9millionsquaremiles)in1990,
primarilyattheexpenseofforests.Atthe
sametime,grazinglandsexpandedfrom5
millionkm2(1.9millionsquaremiles)in
1700to31millionkm2(12millionsquare
36
miles)in1990,largelyviatheconversionof
nativegrasslands(GoldewijkandRamankutty2001).Inadditiontoagriculture-drivenlandscapetransformations,themove
tomonoculture-basedformsofagriculture
hascontributedtodecliningbiodiversity.
Wildplantsandanimalsareamajor
sourceoffood.Billionsofpeoplestillharvestwildor“bush”foodaroundtheworld.
Betweenone-fifthandone-halfofallfood
consumedbypoorpeopleindeveloping
countriesisgatheredratherthancultivated.Onaglobalscale,oceanfishcaught
inthewildaccountfor16percentofthe
humandiet(HarrisonandPearce2001).
Wildplantsarealsoamajorsourceof
medicine,andthelossofbiologicaldiver-
sityhasseriousimplicationsintermsof
humanhealth.Ofthe150mostfrequently
prescribeddrugs,morethanhalfare
derivedfromorpatternedafterchemical
compoundsfoundinplants(Brehm2003).
Moreover,plantsareanimportantsource
offuel.Nearly15percentoftheworld’s
energyisderivedfromtheburningofplant
materials(DeLeoandLevin1997).
Worldwide,peopleeatonlyasmallfractionofthe70000plantsknowntobeedibleortohaveedibleparts(Wilson1989).
Butretainingbiodiversityisstillvitalfor
thefoodsupply,sincemostfoodcropsconstantlyrequireaninfusionof“wild”genes
tomaintaintheirresistancetoever-evolvingpests(HarrisonandPearce2001).
Photoslefttoright:AfamilyofelephantsinAfrica(Credit:GydeLund/UNEP).Aclear-cutsectionofforest(Credit:StevenPoe/UNEP/Topfoto).YellowstoneNationalPark(Credit:GydeLund/
UNEP).Peopleoftenpeeltheloosebarkoffbirchesforsouvenirs.Danforth,MEUSA(Credit:
RandyCyr/UNEP/Forestryimages.org).
Despiteourdependenceonbiodiversity,ithasbeenestimatedthat27000
speciesarelosteveryyear—roughlythree
perhour.Otherestimatesputthenumber
muchhigher.Thegreatestlossofbiodiversityiscurrentlytakingplaceinwet
tropicalregionswhererainforestecosystemsarebeingaltereddramatically.But
lossofbiodiversityisalsoevidentindrier
regions,duetodesertification.Majorcontributorstospeciesextinctionsandlossof
biodiversityworldwideinclude:
•humanpopulationgrowth;
•unsustainablepatternsofconsumptionsuchasover-harvestingofplant
andanimalresources;
•pooragriculturalpractices;
•increasedproductionofwastesand
pollutants;
•urbandevelopment;and
•internationalconflict(UNEP2002b).
Lossofbiodiversityoccurshand-inhandwithhabitatloss,andhabitatlossis
generallygreatestwherehumanpopulationdensityishighest(Harrison1997).
Onetypeofhabitatlossisfragmentation.
Fragmentationoccurswhereaonce-continuousecosystemisbrokenupintomany
small,poorlyconnectedpatchesofland,
whichhappenswhenblocksoftreesare
removedfromaforest.Achangeinland
covertypicallyaccompaniesfragmentation.Sixcategoriesoffragmentationhave
beenidentified(interior,perforated,
edge,transitional,patch,andundetermined)dependingonhowagivenarea
oflandisbrokenup(Riittersetal.2000).
Fragmentationmaybehuman-inducedor
duetonaturalcausessuchasfire,floods,
orwind.Fragmentationmaycreatemore
diverselandscapesthanwereoriginally
present,andwhileitmaydestroyhabitats
ofsomespecies,itcanalsocreatehabitats
forothers.
Lefttoright:JunipersnearnearPaulina,Oregon.Withoutnaturalfirestocontroltheirspread,juniperscanbecomeinvasiveinrangelands(Credit:GydeLund/UNEP).Womenherdinggoats(Credit:
Unknown/UNEP/Topfoto).Cattlegrazinginabog(Credit:RubaiWang/UNEP/Topfoto).Kudzu
takingoverthelandandtreesinthesoutheasternUnitedStates(Credit:GydeLund/UNEP).
37
CumulativeGrowthinProtectedAreasby5YearIncrements:
1872–2003
AreaofSites
Numberofsites
18,000,000
100,000
16,000,000
14,000,000
80,000
12,000,000
60,000
10,000,000
8,000,000
40,000
6,000,000
4,000,000
20,000
2,000,000
0
Figure2.11:Thenumberandextentoftheworld’s
protectedlandsincreasedsignificantlyduringthe
periodfrom1872to2003.Thegreatestincreasehas
occurredoverthepastfewdecades.In2003,thetotal
numberofprotectedsitessurpassed100000,while
totalareaincreasedtomorethan18millionkm2(7
millionsquaremiles).Source:Chapeetal.2003
1872
1902
1917
1932
1947
InvasiveSpecies
Mostplantsandanimalsexistinplacesin
whichtheydidnotoriginate.Theymoved
orwereintroducedintonewareasover
time.Whilerootedplantscannotthemselvesmovefromplacetoplace,thedispersionoftheirseedsbywind,water,and
animalshasenabledthemtospreadinto
manynewhabitats.
Anintroducedspeciesisonewhose
existenceinagivenregionisduetosome
CaseStudy:LakeMaracaibo,Venezuela
LakeMaracaiboinnorthwesternVenezuelais
thelargestnaturallakeinSouthAmericaat
13330km2(5146squaremiles).Atitswidest
point,itismorethan125km(78miles)wide.
ThelakeitselfliesintheMaracaibobasin,
whichissemi-aridinthenorth,butaverages
over1200mm(47in)ofannualrainfallin
thesouth.Ithasbeensufferingfromaserious
problemofinvasiveduckweed,atinyaquatic
plantthatgrowsinfreshwater.Thisfirstimage
1952
1962
1977
1992
2003
0
typeofhumanactivity.Thatactivitymay
enablethespeciestocrossnaturalgeographicbarriersoritmaytransformconditionsinanareaastobeinsomewayfavorabletothespecies’growthandspread.
Introducedspeciesarealsocalledalien,or
exotic,species.
Manyintroducedspecieshavebeen
activelytransportedbypeopletonewareas
forspecificpurposesandhaveplayed
importantandbeneficialrolesinhuman
(left),takenbytheAquaMODISsatelliteon
17December2003,showsthelakeduringthe
wintermonths,whenduckweedisabsentfrom
thelake’swaters,andthesilverysunglintisabsent.Insummertheweedblooms.Thetrue-colourimagefrom26June2004(middle)shows
strandsofduckweedcurlingthroughthelake,
floatingatthesurface,orslightlysubmerged
inthebrackishwater.AcloserlookinAugust
2004(right)revealsthestrangleholdtheduckweedhasonportareas,especiallyalongthe
importantoilshippingroutesintheneckof
history.Mostmodernagriculturalcrops
wereintroducedintotheregionsthey
nowinhabit.Forinstance,corn(maize)is
thoughttohaveoriginatedinMexicosome
7000yearsago.Todayitisfoundworldwide.Wheatprobablyoriginatedinthe
MiddleEast.Currently,wheatisgrownon
morelandareaworldwidethananyother
cropandisaclosethirdtoriceandcornin
totalworldproduction.
Manymoderndomesticatedanimals
werealsonewspeciesintroductionsat
somepointintheirhistory.Moderndomesticcattleevolvedfromasingleearly
ancestor,theauroch.Cattleweredomesticatedbetween10000and15000years
agoneartheboundaryofEuropeandAsia
orSouthwestAsia.Cattlearenowwidely
distributedthroughouttheworld.The
totalworldcattlepopulationinthelate
LakeMaracaibo.Fishandthefishingindustry
sufferasthickgreenmatsblockphotosynthesis
andalterfishhabitats.Theweedalsoadheres
toboats,affectscoolingsystems,andobstructs
travel.InSeptember2004,Venezuela’sMinistryofEnvironmentandNaturalResources
reportedthatithadreducedtheduckweed
areaby75percent,usingduckweedharvesting
machinesfromtheUnitedStates.Theministry
isinvestigatingusingtheharvestedweedas
animalfodder.
Credit:(Left,rightimages)NASA;(middle)LPDAAC–USGSNationalCenterforEROS
38
Table2.11–Growthofprotectedareasoftheworldin1994and2004(inpercent)
Ratio
1994
2004
World
DevelopedCountries
CommonwealthIndependentStates(CIS)
CIS-ASIA
CIS-Europe
Developing
NorthernAfrica
Sub-SaharanAfrica
LatinAmerica&theCaribbean
EasternAsia
SouthernAsia
South-easternAsia
WesternAsia
Oceania
LeastDevelopedCountries(LDCs)
LandlockedDevelopingCountries(LLDCs)
SmallIslandDevelopingStates(SIDs)
7.8
11.3
2.8
3.6
2.6
7.6
3.5
8.1
8.0
8.2
4.5
4.8
21.4
1.0
7.7
8.4
1.6
9.5
14.1
3.0
3.8
2.8
9.1
3.9
8.3
9.9
14.2
5.1
5.9
22.0
1.1
7.9
9.6
2.8
couldallowtheweedstoadapttonew
environmentsmorequickly,andbetter
resistattackbyinsects.Higherlevelsof
carbondioxideintheatmospheremayalso
favorplantsthatcanutilizeextracarbon
dioxideandgrowfaster.Onesuchexample
ischeatgrass,anintroducedspeciesthat
nowdominatesvastareasoftheAmerican
West(Holmes1998).Inotherpartsofthe
world,invasiveexoticplantspeciesmake
up4to44percentofthetotalnumberof
speciesinecosystems(Lövei1997).
Invasiveexoticspeciesareoneofthe
mostsignificantdriversofenvironmental
changeworldwide.Theyalsocontribute
tosocialinstabilityandeconomichardship,andplaceconstraintsonsustainable
development,economicgrowth,andenvironmentalconservation.Worldwide,the
annualeconomicimpactofinvasivespecies
Thereisconsiderablevariationinthetotalareaprotectedbetweenregions,rangingfrom1.1percentin
thedevelopingcountriesofOceaniato22.0percentinWesternAsia.Thepercentagecoverageinboth
onagriculture,biodiversity,fisheries,forWesternandEasternAsia(14.2percent)exceedsthecoverageofalldevelopedcountries(14.1
ests,andindustryisenormous.TheWorld
percent)representingasignificantcommitmentbytheseregionstoconservation.However,theconstraintsimposeduponthedatabythecriterionforadateofestablishmentwithintheMillenniumDevelConservationUnion(IUCN)estimatesthat
opmentGoals(MDG)reportingperiodsuggestthatallfiguresshouldbetreatedcautiously.
theglobaleconomiccostsofinvasiveexotic
Source:UNEP-WCMC2005
speciesareaboutUS$400billionannually
(UNEP2002a).Alieninvaderscost140bil1980swasestimatedtobenearly1.3bilareundersiegefromincreasingnumbers
liondollarsayearintheUSAalone(Mclion.Chickens—theworld’smostabundant ofharmfulinvasivespecies.Theseinclude
Grath2005).Lesseasilymeasuredcosts
domesticatedbird—aregenerallybelieved diseaseorganisms,agriculturalweeds,and
alsoincludeunemployment,impactson
tohavedescendedfromjunglefowlin
destructiveinsectsandsmallmammalsthat
infrastructure,shortagesoffoodandwater,
SoutheastAsia.Theyweresubsequently
threateneconomicproductivity,ecological
environmentaldegradation,increasesin
stability,andbiodiversity.Onalocalscale,
introducedintoalmosteverycountryand
therateandseverityofnaturaldisasters,
regionoftheworld.
suchinvasionsdecreasediversityofnative
andhumanillnessanddeath.InvasiveexInstarkcontrasttosuchpositivespecies floraandfauna.Globally,theycontribute
oticspeciesrepresentagrowingproblem,
tomakingthebiospheremorehomogeintroductionsarethosewhereintroduced
andonethatisheretostay—atleastfor
exoticspecieshavebecomeinvasive.Scien- neousandlessresilient.
theforeseeablefuture(Brandt2003).
Naturalbiodiversityhelpstomaintain
tificallyspeaking,invasivespeciesarethose
ecologicalresilienceinthefaceofvarying
organismsthatareunwantedandhavea
ProtectedandWildernessAreas
tendencytospread.Invasivespeciesharm, environmentalconditions(Hollingetal.
Wildernessareasarethoseareasofland
1995).Invasionbyexoticspecieslessens
orhavethepotentialtoharm,agiven
thatarerelativelyuntouchedbyhuman
ecosystemorpeoples’healthoreconomic ecologicalresilienceandcantransform
ecosystemsinunpredictablewaysthatmay activities.Toqualifyaswilderness,anarea
well-being(Clinton1999).Historically,
musthave70percentormoreofitsorigisomeinvasiveexoticspecieshavebeen
havenegativeconsequencesforpeople.
nalvegetationintact,coveratleast10000
intentionallyintroducedintonewsettings; Thisproblemisgrowinginseverityand
km2(3861squaremiles),andbeinhabtheintroductionofthecommonstarling
geographicextentasglobaltradeand
itedbyfewerthanfivepeopleperkm2(12
intotheUnitedStatesandtherabbitinto
internationaltravelexpand,asmarkets
peoplepersquaremile).
Australiaaretwoclassicexamples.Introareliberalizedandderegulated,asecosysductionsofotherinvasivespecieshave
temsarefurtheralteredandfragmented,
Wildernessareasaremajorstorehouses
occurredbyaccident,suchasthatofzebra andasglobalclimatecontinuestochange ofbiodiversity.Theyalsoprovidecritical
musselsintotheAmericanGreatLakesasa (Brandt2003;Dalmazzone2000).
ecosystemservicestotheplanet,including
resultofshippingactivities.
watershedmaintenance,pollination,and
Invasionsbyalienspeciesaresetto
Nativeorindigenousspeciesarethose
thatoccurnaturallyinanareaorhabitat.
Invasivespeciesoftenout-competeanddisplacenativespeciesbecausetheinvaders
havenonaturalenemiesandcanspread
easilyandquickly.Bothmanagedand
naturalecosystemsthroughouttheworld
worseninthenextfewdecadesifthe
worldcontinuestowarmasmostscientists
predictitwill.Longergrowingseasons
spawnedbyglobalwarmingmaygive
invasiveweedyplantstimetoflowerand
setseedswherepreviouslytheycouldonly
spreadasexually.Thisnew-foundability
carbonsequestration.Wildernessareas
currentlycovernearlyhalftheEarth’sterrestrialsurface(Mittermeieretal.2003).
Whilethatrepresentsasignificantamount
oflandarea,however,mostwilderness
areasarenotprotected,andaretherefore
atrisk.
39
WorldEnvironmentalHotspotsasidentifiedbyConservationInternational.
Source:www.conservation.org
Oneofthemosteffectivemeansfor
conservingwildernessisthroughthedevelopmentofprotectedareas.Aprotected
areaisanareaofland(orwater)especially
dedicatedtotheprotectionandmaintenanceofbiologicaldiversity,alongwith
naturalandassociatedculturalresources,
thatismanagedthroughlegalorother
effectivemeans(IUCN1994).Protected
areasaremanagedforawidevarietyof
purposes,including:
•protectionofspecificnaturaland
culturalfeatures;
•tourismandrecreation;
•education;
•sustainableuseofresourcesfrom
naturalecosystems;and
•maintenanceofculturalandtraditionalattributes(GreenandPaine1997).
andCanadacombined,ormorethan12
percentoftheEarth’ssurface(Chapeet
al.2003).Thattotalexceedstheten
percentcalledforintheCaracasAction
PlanformulatedattheFourthWorldParks
Congressheldin1992inCaracas,Venezuela.Between10and30percentofsomeof
theplanet’svitalnaturalfeatures,suchas
Amazonianrainforestsandtropicalsavannahgrasslands,areclassifiedasprotected
areas.However,ecoregionalandhabitat
representationremainsuneven.
The2003UnitedNationsListofProtectedAreas—compiledbyUNEPand
theIUCNandreleasedduringtheFifth
•scientificresearch;
WorldParksCongressinDurban,South
Currently,almosthalfoftheworld’s
•wildernessprotectionandpreservation
Africa—revealsthattherearenow102102 protectedareasarefoundinregionswhere
ofspeciesandecosystems;
protectedareas,togetherrepresentinga
agricultureandloggingareprimaryland•maintenanceofenvironmental
totallandarearoughlyequivalenttoChina usestrategies.Allindicationsarethatfood
services;
40
andtimberproductionwillneedtoincreaseincomingdecadestokeepupwith
populationgrowthandincreasingdemand
forwoodandwoodproducts.Thus,establishingadditionalprotectedareas,while
helpingtopreservebiologicaldiversity,will
takelandoutofproductionandputmore
stressonlandselsewhere(Sohngenetal.
1999).Balancingtheneedtoprotectwild
speciesandconservehabitatwhileatthe
sametimeincreasingagriculturalandtimberproductionrepresentsatremendous
challenge(McNeelyandScherr2001).
Oftheworld’sprotectedareas,thevast
majority—91.3percent—arefoundinterrestrialecosystems.Fewerthanten
percentoftheworld’slakesandlessthan
0.5percentoftheworld’sseasandoceans
liewithinprotectedareas(SBSTTA2003).
Recognizingthattheworld’smarineenvironmentremainslargelyunprotected,
theFifthWorldParksCongressputforth
theDurbanActionPlan.ThePlancallsfor
theestablishmentofatleast20-30percent
marineprotectedareasworldwideby2012.
ThePlanalsocallsfortheconservationof
allgloballythreatenedorendangeredspeciesby2010.
Inthecomingyears,furtherdevelopmentofglobalnetworksofprotectedareas
willneedtofocusonfourareas(Green
andPaine1997):
•consolidatingexistingnetworksbyaddressingmajorgaps;
•physicallylinkingprotectedareasto
oneanothersotheyfunctionmoreeffectivelyasnetworks;
Credit:HarriettO’Mahony/UNEP/Topfoto
•expandingnetworksbyformingor
strengtheninglinkswithothersectors,
notablytheprivatesector;
mostdevastatingdiseasesintheformof
uniquechemicalcompoundsandas-yet-undiscoveredgeneticmaterial.
•andimprovingtheeffectivenesswith
whichprotectedareasaremanaged.
ArecentanalysispublishedbyConservationInternationalidentifiednine
additionalsitesasareasofextraordinarily
highbiologicaldiversity,popularlyknown
ashotspots,takingthecountofhotspotsto
34.These34regionsworldwidearewhere
75percentoftheplanet’smostthreatened
mammals,birds,andamphibianssurvive.
Inthese34hotspots,estimated50percent
ofallvascularplantsand42percentof
terrestrialvertebratesexist.Thereforeitis
criticaltoprotectandpreservetheseareas
(ConservationInternational2005).
Protectedareasareoftenconsidereda
kindofsacrifice,afinancialburdenrather
thananasset.Yetestablishing,maintaining,andexpandingprotectedareasisa
fundamentalapproachtosafe-guarding
theenvironmentandconserving
biologicaldiversity.
Protectedareasarealsoimportantin
otherrespects,suchashelpingtomaintain
freshwaterresources.Protectedareasmay
alsoholdthecurestosomeoftheworld’s
Credit:ChristianLambrechts/UNEP
41
CaseStudy:KamengandSonitpur
ElephantReserves,
MapofStudyArea
ArunachalPradesh,India
S.P.S.KushwahaandRabulHazarika
TheKamengandSonitpurElephantReservesinnortheasternIndiaarecomprisedof
transbordersubtropicalevergreentotropical
moistdeciduousforestsofArunachalPradesh
andAssam.Thereservesarefacingdeforestationandhabitatlossinrecentyears.Thisstudy
attemptstoinvestigatethelossofhabitatin
thesereservesusingtemporalsatelliteimagery
ofperiods1994,1999and2002.Theon-screen
visualinterpretationofthethree-periodimageryrevealedalarmingandcontinuoushabitat
lossfrom1994to2002.Theoverallhabitatloss
wasfoundtobe344km2(133squaremiles)between1994and2002.Theaverageannualrate
ofdeforestationworkedouttobe1.38
Sonitpur
percent,whichismuchbiggerthanthenationalaverage.Therateofdeforestationwas
highestbetween1999and2002.Thestudyindicatedthatatthisratemuchoftheforestsinthe
studyareawouldbedepletedwithinthenext
fewyears.Italsoshowedthatmoistdeciduous
forests,whichpossessthehighestbiodiversity
inAssam,arefacingmaximumdeforestation.
Highdeforestationhasresultedinhighmanelephantconflicts.
Habitatloss(1994–1999)
Habitatloss(1999–2002)
Habitatloss(1994–2002)
Credit:Dr.BibhabTalukdar
4242
2.6 Energy
Consumption
and Resource
Extraction
Energyismeasuredbyitscapacitytodowork
(potentialenergy)ortheconversionofthis
capacitytomotion(kineticenergy).Mostofthe
world’sconvertibleenergycomesfromfossilfuelsthatareburnedtoproduceheatthatisthen
convertedtomechanicalenergyorothermeans
inordertoaccomplishtasks(EIA2004a).
Energyisessentialforthefulfillmentofmany
basichumanneeds,suchasgeneratingelectricity,heatingandcoolinglivingspaces,cooking
food,forgingsteel,andpoweringenginesfor
manyformsoftransportation(Harrisonand
Pearce2001).Energyuseiscloselytiedtohumanhealthandwell-being.Worldwide,roughly
2000millionpeopledonothaveaccesstoelectricity.Countriesinwhichenergyuseislowtend
tohavehighinfantmortalityrates,lowliteracy
rates,andlowlifeexpectancies.Itisthrough
theutilizationofconvertibleenergysourcesthat
themodernworldhastranscendeditsagrarian
rootsandfosteredtheenergy-drivensocieties
thatcharacterizeittoday.Generatingthepower
tosustainthesesocietieshasentailedextractingmassiveamountsofnaturalresourcesfrom
theplanet.ExtractionistheprocessofobtainCredit:DarrenDefner/UNEP/Topfoto
NightlightMapoftheWorld
Credit:NOAA/UNEP/NASA
43
G l oba l N a tura l Resources
Affluentcountriesconsumevastquantitiesofglobalnaturalresources,butcontribute
proportionatelylesstotheextractionofmanyrawmaterials.Thisimbalanceisdue,in
part,todomesticattitudesandpoliciesintendedtoprotecttheenvironment.Ironically,
developednationsareoftenbetterequippedtoextractresourcesinanenvironmentally
prudentmannerthanthemajorsuppliers.Thus,althoughcitizensofaffluentcountries
mayimaginethatpreservationistdomesticpoliciesareconservingresourcesand
protectingnature,heavyconsumptionratesnecessitateresourceextractionelsewhereand
oftentimeswithweakenvironmentaloversight.Amajorconsequenceofthis“illusionof
naturalresourcepreservation”isgreaterglobalenvironmentaldegradationthanwould
ariseifconsumptionwerereducedandalargerportionofproductionwassharedby
affluentcountries.Clearly,environmentalpolicyneedstoconsidertheglobaldistribution
andconsequencesofnaturalresourceextraction(Berliketal.2002).
Credit:JonPBonetti/UNEP/Topfoto
ingausefulsubstancefromarawmaterial
(NCR&LB2003).Suchrawmaterialsmay
includefossilfuels,metals,minerals,water,
andbiomass,includinganimalsandraw
materialsfromplantsandcrops
(EEA2001).
centbetween2001and2025,from404
quadrillionBritishthermalunits(Btu)in
2001to640quadrillionBtuin2025(EIA
2003;EIA2004b).Whileaslow,steadyincreaseinenergyconsumptionisexpected
inindustrializednations,wheremostenResourcescanbedividedintothosethat ergyusecurrentlytakesplace,ameteoric
increaseinconsumptionisanticipatedin
arerenewable,suchasplantandanimal
material,andthosethatarenot,including thedevelopingworldduringthatperiod
(Tilford2000).
coal,oil,andminerals.TheEarthhasa
Thetempoatwhichenergyresources
finitesupplyofnon-renewableresources.
arebeingusedtofuelmodernsocieties
Evenrenewableresources,however,are
exhaustibleiftheyareusedfasterthanthey israpidlydepletingsuppliesofnon-recanbereplenished.
newableresourcesandfarexceedingthe
rateatwhichrenewableresourcescanbe
Totalworldenergyconsumptionhas
naturallyrenewed(Ernst2002).Inmany
risenalmost70percentsince1971(WRI
least–developedcountries,forinstance,
1998).Itisexpectedtoincreaseby58per
CaseStudy:Blackoutin
UnitedStatesandCanada
14August2003
On14August2003,partsofthenortheasternUnitedStatesandsoutheasternCanada
experiencedwidespreadpowerblackouts.
Amongthemajorurbanagglomerationsaffectedbytheelectricalpoweroutagewere
thecitiesofNewYorkCity,Albany,andBuffaloinNewYork,ClevelandandColumbus
inOhio,DetroitinMichigan,andOttawa
andTorontoinOntario,Canada.Other
U.S.states,includingNewJersey,Vermont,
Pennsylvania,Connecticut,andMassachusetts,werealsoaffected.Theblackout
resultedintheshuttingdownofnuclear
powerplantsinNewYorkandOhio,and
airtrafficwasslowedasflightsintoaffected
airportswerehalted.Approximately50
millionpeoplewereaffectedbytheoutage.
Thechangeinthenighttimecitylightsis
apparentinthispairofDefenseMeteorologicalSatelliteProgram(DMSP)satellite
images.Thetopimagewasacquiredon14
August,about20hoursbeforetheblack-
burningbiomassintheformofwood
(largelyanon-renewableresource)generates70to90percentoftheenergyneeded
anddisregardforthefateofnon-renewableresourcesisprevalent.IntheUnited
States,forexample,72percentofthe
country’selectricityisgeneratedusingnonrenewableresources.Onlyabout10per
centcomesfromrenewableresources,with
nuclearpowerprovidingtherest.
Currently,85percentofworldenergy
consumptioncomesfromtheburningof
fossilfuels—oil,coal,andnaturalgas(BP
2003).Althoughnoimmediateshortages
ofthesenon-renewableenergyresources
exist,suppliesarefiniteandwillnotlast
forever.Whattookmillionsofyearsto
out,andthebottomimageshowsthesame
areaon15August,roughlysevenhours
aftertheblackout.Inthebottomscene,
noticehowthelightsinDetroit,Cleveland,
Columbus,Toronto,andOttowaareeither
missingorvisiblyreduced.Previousmajor
blackoutsincludethe9November1965
outagecausedbyafaultyrelayatapower
plantinOntario,whichaffectedalarge
swathoflandstretchingfromTorontoto
NewYork.Anotheronefollowedon14
July1977,theresultofalightningstrike,
affectingNewYorkCity.Thepowersupply
14August2003beforepowerfailure
inninewesternstateswasalsoaffectedin
August1996asaresultofahighdemand
forelectricity,aheatwave,andsagging
electricalpowerlines.
Source:NASA2002,http://earthobservatory.nasa.gov/
NaturalHazards/natural_hazards_v2.php3?img_id=11628;
GlobalSecurity.org2003,http://www.globalsecurity.org/eye/
blackout_2003.htm
15August2003afterpowerfailure
CreditImagecourtesyChrisElvidge,U.S.AirForcehttp://earthobservatory.
nasa.gov/NaturalHazards/Archive/Aug2003/NE_US_OLS2003227_lrg.jpg
4444
CaseStudy:SWERA,theSolarandWind
EnergyResourceAssessment
TheSolarandWindEnergyResourceAssessment
(SWERA)—co-financedbytheGlobalEnvironmentFacility(GEF)—isaprojecttoassist13developingcountriesidentifyoptimallocationsforpotentialsolarandwindenergyproduction.SWERA
assistsbycreatingaglobalarchiveofinformation
gatheredthroughanetworkofinternationaland
nationalagencies.Theseagenciescollectand
analysedataonsolarandwindenergyresources,
energydemand,andelectrification.Usinginputs
derivedfromsatelliteandsurfaceobservations,
SWERApartnersmodelwindandsolarenergyresourcepotentialandproducemapsofwindpower
densityandmonthlyaverageanddailytotalsolar
radiationofagivenarea.Thisinformationcan
thenbeusedtofacilitateinvestmentsandcreate
policiesintheparticipatingcountriesfordevelopingsolarandwindenergy.
Source:UNEP/GRID–SiouxFalls
Credit:NREL
Credit:NCAT/UNEP/NREL
Credit:EnergyNorthwest/UNEP/NREL
4545
producewillbeconsumedinthetime
frameofacenturyortwo(Hawken1994;
Tilford2000).
Thisrapid,large-scaleconsumptionofa
fuelsourcethattookmillenniatoproduce
hasgeneratedunforeseencomplications,
severalwithglobalimplications.Burning
fossilfuelsproducesatmosphericpollutants
suchasoxidesofsulfurandnitrogenand
unburnedhydrocarbons.Fossilfuelcombustionalsoaddsoneofthemostprevalent
greenhousegases—carbondioxide—tothe
atmosphere.Asaresult,worldenergyuse
hasemergedatthecenteroftheclimate
changedebate.Worldcarbondioxideemissionsareprojectedtorisefrom
23900millionmetrictonnesin2001to
27700millionmetrictonnesin2010and
37100millionmetrictonnesin2025(EIA
2004b).TheEarth’satmosphereandbiospherewillnotremainunchangedbythe
combustionofsuchenormousamountsof
thesefuels.Therelativelysuddenreleaseof
massiveamountsofcarbonhasthepotentialnotonlytodisrupttheEarth’sheat
balanceandclimate,butotherpartsof
theglobalcarboncycleaswell,andin
unpredictableways.
TheEarthcannotsustainexistinglevels
ofresourceconsumption.Furthermore,
resourceextractionmethodsareoften
environmentallydestructive.Theimpact
ofenvironmentaldegradationhitsthose
whoarepoorestthehardest.Manyofthe
world’senergysourcesandothernatural
resourcescomefromdevelopingcountries.
Extractingandharvestingtheseresources
canresultinair,soil,andwaterpollution.
Italsogenerateswaste;theamountofwaste
associatedwithextractingminerals,for
instance,canbeenormous.Disposingof
wastesinenvironmentallyfriendlywaysis
adaunting,ifnotimpossible,taskinmany
developingnations.
Amajorchallengeforthe21stcentury
istodevelopmethodsofgeneratingandusingenergythatmeettheneedsofthepopulationwhileprotectingtheplanet(HarrisonandPearce2001).Yetmostoftheworld
isstillwithoutenergypoliciesthatdirector
restrictconsumptionpatterns.
Onlythroughconservationandresource
recoverystrategiescanwehopetoreacha
sustainablebalancebetweenavailableresourcesandtheirconsumption.Theutiliza-
SourcesofEnergy
Coal
Coalistheworld’slargestsourceoffuelfor
electricityproduction.Thebyproductsofcoal
combustionarealsoamajorsourceofenvironmentaldamage.
Credit:Unknown/UNEP/Freefoto.com
Oil
Althoughusedprimarilyintheproduction
oftransportationfuels,oilisalsousedfor
generatingelectricity,forheating,andinthe
productionofchemicalcompoundsandsyntheticmaterials.
Credit:Unknown/UNEP/Freefoto.com
NaturalGas
Comparedtocoalandoil,naturalgasisa
relativelyclean-burningfossilfuel.Itisused
primarilyforheatingandforpoweringmany
industrialprocesses.Increasingly,naturalgas
isburnedtodriveturbinesusedintheproductionofelectricity.
Credit:Unknown/UNEP/Freefoto.com
Biomass
Plantandanimalmaterial,orbiomass,isa
richsourceofcarboncompounds.When
burnedtoreleaseenergy,biomassdoesnot
addadditionalcarbontothenaturalcarbon
cycleasdofossilfuels.Fast-growingplants,
suchasswitchgrass,willow,andpoplarcan
beharvestedandusedas“energycrops.”
Biomasswastes,includingforestresidues,
lumberandpapermillwaste,cropwastes,
garbage,andlandfillandsewagegas,canbe
usedforheating,astransportationfuels,and
toproduceelectricity,whileatthesametime
reducingenvironmentalburdens.According
totheWorldBank,50to60percentoftheenergyusedindevelopingcountriesinAsia,and
70to90percentusedindevelopingcountries
inAfrica,comesfromwoodorotherbiomass;
halftheworldcookswithwood.
Credit:VolkerQuaschning/UNEP
Sources:
www.freefoto.com,http://www.topfoto.co.uk/,Prof.Dr.-Ing.habil.VolkerQuaschninghttp://www.volker-quaschning.de
46
Nuclear
Nuclearpowerharnessestheheatofradioactivematerialstoproducesteamfor
electricitygeneration.Theuseofnuclear
powerisexpectedtodeclineasaging
plantsaretakenoutofoperation.
Credit:Unknown/UNEP/Freefoto.com
Hydroelectric
Credit:VolkerQuaschning/UNEP
Hydroelectricpowerusestheforceofmovingwatertoproduceelectricity.Alarge
partoftheworld’selectricityisproducedin
hydroelectricplants.Manyoftheseplants,
however,areassociatedwithlargedamsthat
disrupthabitatsanddisplacepeople.Smaller“runoftheriver”hydroelectricplants
havelessenvironmentalimpact.
Geothermal
Geothermalenergyisenergycontainedin
intenseheatthatcontinuallyflowsoutward
fromdeepwithintheEarth.Geothermal
energyistypicallyusedtoheatwater,which
isthenusedtoheatbuildingsdirectlyorto
driveturbinestoproduceelectricity.
Credit:Lupidi/UNEP/Topfoto
Solar
Credit:AnthonyKarbowski/UNEP/Topfoto
Solarenergy—powerfromthesun—is
readilyavailableandinexhaustible.Humanshaveusedsunlightforheatingand
dryingforthousandsofyears.Converting
thepowerofsunlightintousableenergy
forms,suchaselectricity,isnotwithout
cost,butthesunlightitselfisfree.Solar
cells,orphotovoltaics,aredevicesusedto
transformsunlightintoelectriccurrent.
Wind
Windpowerisanancientenergysource
thathasmovedintothemodernera.Aerodynamicallydesignedwindturbinescan
produceelectricitymorecheaplythancoalburningpowerplants.
Credit:SanjaySingh/UNEP/Topfoto
tionofnon-renewableresourcesis
theoreticallynotsustainable.Butifused
wisely,somenon-renewableresourcescan
beconservedandrecycledforaverylong
time.Torecyclemeanstomakenewproductsfromoldones.Recyclingmaterials
suchaspaper,aluminum,andglasssaves
energy,reducespollution,andconserves
naturalresources(EPA2003).Everynation
mustassumeresponsibilityforrecycling
itsownwastes.SomeindustrializedWesterncountries“dispose”oftheirelectronic
wastesbyshippingthemtoAsia—anincreasinglycommonpractice(FOEE2004).
Toinsurethatrenewableresources
canbereplenishedatasustainablerate,
peoplemustswitchtomoreenvironmentallyfriendlyenergysourcesandemploy
newtechnologiesthatcanhelpmakesuch
sustainabilityareality(Ernst2002).Indeed,
newtechnologies—coupledwitheffective
andefficientuseofexistingtechnologies—
areessentialtoincreasingthecapabilities
ofcountriestoachievesustainabledevelopmentonmanyfronts,aswellassustainingtheworld’seconomy,protectingthe
environment,andalleviatingpovertyand
humansuffering(HayandNoonan2000).
MostchangesintheEarth,including
changesbroughtaboutbyincreasingenergyconsumption,canbeobservedthrough
suchtoolsasremotesensing.Remote
sensingisthecollectionofinformation
aboutanobjectwithoutbeinginphysical
contactwiththeobject.Aircraftandsatellitesarethecommonplatformsfromwhich
remotesensingobservationsaremade.
Satelliteimagery,acrucialcomponentof
thispublication,isespeciallyusefulfor
studyingchangesinourEarth’senvironment.Mostsatelliteimageryiscollected
usingmultispectralscanners,whichrecord
lightintensitiesindifferentwavelengthsin
thespectrumfrominfraredthroughvisiblelightthroughultravioletlight.Satelliteimageryisusefulbecauseofitsstable
nature(sameresolution,sametime,same
datacharacteristics).Aidedbytheglobal
positioningsystem(GPS),thesesatellites
knowtheirorbitalpositionprecisely.Thus,
satelliteimageryisideallysuitedforapplicationsrequiringlarge-areacoverage,suchas
agriculturalmonitoring,regionalmapping,
environmentalassessment,andinfrastructureplanning(Krouseetal.2000).
47
48
MINING
THEBLACKTRIANGLE,EUROPE
48
48
The so-called Black Triangle is an area bordered by Germany, Poland, and
the Czech Republic and is the site of extensive surface coal mining operations. In the 1975 satellite image above, the gray areas are surface mines
located primarily in the Czech Republic. Air-borne pollutants from coal
extraction activities tended to become trapped by the mountainous terrain to the northeast and were concentrated in the area around the mines,
eventually causing severe deforestation along the border between the Czech
Republic and Germany. In the 2000 image, this deforestation is very obvious, appearing as large brownish patches. Interestingly, the 2000 image also
reveals somewhat improved vegetation cover—a slight “greening” of the
landscape—as compared to conditions in 1975. Some of this improvement
may be attributable to actions taken by the three countries bordering the
Black Triangle to reduce pollutants produced by the mining operations. The
implementation of anti-pollution technologies, including circulating fluidized-bed boilers, clean coal technology, and nitrous oxide emission burners,
appears to have reversed some, albeit not all, of the environmental damage
experienced by the region as a result of the mines.
49
49
In one year up to 67 000 tonnes of sulfur dioxide, 500 tonnes of lead, 400
tonnes of zinc and 4 tonnes of cadmium can be released by the city’s two active smelters. The affected area is huge: in excess of 180 000 hectares (445 000
acres) of land are affected by air pollution and 150 000 hectares (371 000 acres)
of agricultural land are untenable. 31 000 hectares (77 000 acres) of forest are
also unacceptably polluted.
Credit:LorantCzaran/UNEP
MINING
50
50
¸ MICA,ROMANIA
COPSA
¸ Mica is a large industrial city located in the very center of
Copsa
Romania and is classified as an “environmental disaster area.” The environmentally damaged area covers hundreds of square kilometres of
¸ Mica are non-ferrous metalworking
land. The main industries in Copsa
and chemical processing plants, and their effect on the environment
has been devastating. Air pollution by heavy metals is 600 times
the allowed levels. To make matters worse, a lead-smelting facility emitted
fumes containing sulfur dioxide, lead, cadmium, and zinc on the town and
surrounding area for 50 km2 (19 square miles). The entire town and much of
the surrounding area were covered with a blanket of black soot daily until the
facilities were forced to close in 1993.
In 1989 Copsa
¸ Mica was exposed as one of the most polluted places in
Europe. It has the highest infant mortality rate in Europe, 30.2 per cent of
children suffer reduced “lung function” and 10 per cent of the total population of 20 000 suffer “neurobehavioral problems.” The soil and the local food
chain probably will remain contaminated for at least another three decades.
51
51
MINING
ESCONDIDA,CHILE
52
52
Located at an elevation of 3 050 m (10 006 ft), Chile’s Escondida Mine
is an open-pit copper, gold, and silver mine and also the largest copper mine in the world. Isolated in the barren, arid Atacama Desert in
the country’s far north, the Escondida Mine relies heavily on external
well fields for the water used in its mining operations. Unlike similar
mining operations, however, Escondida has a redeveloped tailings
impoundment, which appears on the 1989 image as a white patch in the
lower left corner. Impoundments of this type help reduce water consumption and enhance water conservation, two areas where mining activities
typically fall short. The Escondida Mine also minimizes the impact of its
operation on the environment by means of a 170-km-long (106 miles) underground pipeline that carries copper concentrate slurry from the mine to
the port of Coloso. This underground scheme is efficient and ecologically
sound, as the copper travels downhill without disrupting the environment.
The 2003 image shows how the Escondida Mine has grown and expanded
while at the same time continues to minimize negative impacts from its
mining operations on the environment.
53
53
M
INING
E
C
KATI ,
54
54
ANADA
As of 2001, the Ekati Mine was North America’s only operating diamond mine. Located in the north central Northwestern Territories
(NWT) of Canada, the mine yields raw diamonds from a sparsely
inhabited sub-arctic region. Air transport connects mine personnel
and supplies year-round, while a single winter ice road provides the
only vehicular access just ten weeks per year.
Expanded mining exploration in the 1990s began a new era for this otherwise undeveloped region. Wildlife officials have collared and tracked caribou,
in a herd ranging from 350 000 to half a million, to monitor their movement
and behavior in proximity to the mines. Historical information about the
herds comes from Dogrib and Inuit knowledge obtained from elder natives
who still inhabit the NWT, and who have depended on the caribou
for centuries.
These two images compare the same area, pre-mining and after mine operations have commenced. The white patch in the northwest portion of the
2000 image represents the mine and the associated infrastructure.
55
55
MINING
OKTEDIMINE,PAPUANEWG
56
56
The controversial Ok Tedi copper mine is located at the
headwaters of the Ok Tedi River, a tributary of the Fly River,
in extremely rough terrain in the rainforest-covered Star
Mountains of Papua New Guinea’s western province. Prior
UINEA to the opening of the mine in 1984, this area was very
isolated, sparsely inhabited, and ecologically pristine. This
pair of satellite images reveals the tremendous environmental impact the
mine has had in 20 years. The uncontrolled discharge of 70 million tonnes of
waste rock and mine tailings annually has spread more than 1 000 km (621
miles) down the Ok Tedi and Fly rivers, raising river beds and causing flooding, sediment deposition, forest damage, and a serious decline in the area’s
biodiversity. In the 1990 image, both the mine and the township of Tabubil—developed east of the river in support of the mine—are clearly visible.
Lighter patches of green show disturbance of the original forest cover from
subsistence agriculture, road clearing, and other infrastructure development.
57
57
M
INING
P
R
B
OWDER
58
58
IVER
ASIN ,
UNITEDSTATES
The Powder River basin, located in northeast Wyoming
and southeast Montana, is a core area of coal and natural
gas production in the United States. Coal mining activities
in the basin date back to 1975.
In recent years surface mining in Wyoming has mushroomed, making it the leading coal producer in America
at almost 300 000 tonnes per year. Similarly, coal bed methane gas development in this region is unrivaled in the U.S.
The images show areas under coal exploitation. Notable is the remarkable
increase in mining operations in the 2001 image. Reasons for the expansion
include improvements in the area’s rail network, the high grade of the coal
deposits, and the depletion of high-grade deposits in other major coal mining areas such as West Virginia and Kentucky.
The open cast coal mines appear as white-purplish while the reddish
brown areas are bare ground. Vegetated areas are green.
59
59
MINING
WEIPABAUXITEMINE,AUSTRALIA
60
60
Mining of bauxite (aluminum ore) began at Weipa, on the Cape York
Pennisula in Queensland, Australia, in 1963. The mine produces 8.5
metric tonnes of ore annually, making it one of the world’s largest
open-cut bauxite mines.
Under current mining practices, vegetation is cleared and the
topsoil is removed and either stockpiled for later use or immediately
The total lease covers an area of approximately 2 590 km2 (1 000 square miles) of
which 68 km2 (26 square miles) have been
mined. Approximately four km2 (1.5 square
miles) of the mined land is revegetated each
year, and over 50 km2 (19 square miles) of
land has been revegetated to date.
replaced on previous mined areas. After topsoil removal, the bauxite is removed, resulting in a lowering of the entire landscape to a depth equivalent
to the thickness of the orebody, often several meters. If the topsoil can be
returned to a mined-out area after only a short time, it still contains most of
the original soil fungi, bacteria and micro fauna. In addition, the seeds from
the original plant community are likely to be viable. On slopes, rigorous
soil conservation measures are implemented, and the area is then normally
planted with suitable native species so that it gradually reverts to bushland.
Some of the profits generated by the mining operation are being placed in
a trust for cultural protection, development and long-term investments to
compensate for the disruption of local Aboriginal inhabitants and
their environment.
61
61
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63
DaylightMapoftheWorld
Credit:UNEP/NASA
64
65
66
Credit:HuZongHuu/UNEP/Topfoto
3
Human Impacts on the Planet
Visualising Change over Time
Humaninteractionswiththeenvironment
leavemanytraces.Formuchofhuman
history,humanimpactontheEarth’s
surfacehasbeenrelativelyminor.Inthe
lastseveralhundredyears,however,that
impacthasgrowntremendously.Change
broughtaboutbyhumanactivitiescannow
beobjectivelymeasured;itcanevenbe
seenfromspace.AstudybytheNational
AeronauticsandSpaceAdministration
(NASA2003a)knownasTheHumanFootprint(Figure3.1)isaquantitativeanalysis
ofhumaninfluenceacrosstheglobethat
illustratestheimpactofpeopleandtheir
activitiesontheEarth.
MapoftheHumanFootprint
Evidenceofchangeisnotalwaysvisibleonthelandscape.Changealsooccurs
intheatmosphere,inthesoil,andinthe
oceansandotherwaterbodies.Inthese
environments,evidenceofchangecan
stillbe“seen,”however,bydetectingand
measuringthingssuchasrisingaverage
globaltemperatures,theconcentrationsof
certaingasesintheatmosphere,andvariouschemicalcontaminantsinwater.
Figure3.1:TheHumanFootprintisaquantitativeanalysisofhumaninfluenceontheEarth’ssurface.Inthis
map,humanimpactisratedonascalefrom0(minimum)to100(maximum)foreachterrestrialbiome.The
colorgreenindicatesareasofminimalimpactwhilepurpleindicatesareasofmajorimpact.Credit:Scott,Michon
Changealoneisnottheonlyproblem.
Itisthedegreetowhichhumanactivities
arechangingtheEarththatisalsocause
2003.TheHumanFootprint.NASA:SocioeconomicDataandApplicationsCenter.Source:http://earthobservatory.nasa.gov/Newsroom/
NewImages/Images/human_footprint.gif
forgrowingconcern.Forinstance,the
resultsofarecentten-yearstudyconcerningtheecologicaleffectsofindustrialized
fishingintheworld’soceansrevealsthat
largepredatoryfishspeciesincluding
tuna,marlin,sharks,cod,andhalibuthave
declinedbyanestimated90percentfrom
pre-industriallevels(MyersandWarm
2003).Furthermore,theaveragesizeof
survivingindividualsamongthesespecies
isonlyone-fifthtoone-halfwhatitwas
previously.
ThecompositionoftheEarth’satmosphereisalsoundergoingrapidchange.
SincelifebeganonEarth,changesin
climatehaveorderedthedistributionof
Credit:ApolloMbabaz/UNEP/Topfoto
67
Credit:PaiboonPattanasitubol/UNEP/Topfoto
organismsandtheirbehavior.Today,
increasesinatmosphericconcentrations
ofgreenhousegasesareexpectedtocause
morerapidchangesintheEarth’sclimate
thanhavebeenexperiencedformillennia
(Figure3.2).Atleastsomeoftheincrease
globallyisduetohumanactivity,and
certainly,localimpactssuchasurbanheat
islandshaveprofoundeffectsonregional
climaticconditions.AsshowninFigure3.2,
wastegenerationanddisposalisoneofthe
waysinwhichhumanscontributegreenhousegasestotheatmosphere.
Anemergingglobalimpactissueisthat
ofelectronicorE-waste—acollectiveterm
fordiscardedelectronicdevices.Overthe
pastdecade,E-wastehasbecomeoneof
theworld’sfastestgrowingwastestreams
and—duetothepresenceoflead,merFigure3.2:Thedisposalandtreatmentofwastecan
produceemissionsofseveralgreenhousegasesthat
contributetoglobalclimatechange.Eventherecyclingofwasteproducessomeemissions,although
theseareoffsetbythereductioninfossilfuelsthat
wouldberequiredtoobtainnewrawmaterials.Both
wastepreventionandrecyclinghelpaddressglobal
climatechangebydecreasinggreenhousegasemissionsandsavingenergy(EnvironmentalProtection
Agency).Source:http://www.grid.unep.ch/waste/html_file/4243_climate_change.html
68
cury,brominatedflameretardants,and
otherhazardoussubstances—oneofthe
mosttoxic.Thedisposalofcomputerwaste
inparticularisbecomingadifficultissueas
millionsofcomputersandotherelectronic
devicesarerapidlybecomingobsoleteas
eachyeartheindustryproducesever-greaterquantitiesofless-expensiveequipment.
Thereareanestimated300millionobsoletecomputersintheUnitedStates,with
fewerthattenpercentdestinedforrecy-
clingeachyear.Evenwhenacomputeris
soldtoasecondhandpartsdealer,however,
thereisagoodchanceitwillendup
inadumpinthedevelopingworld
(Figure3.3).
TheEarth’sforestsarealsounder
pressure.Tropicalforestsarenowbeing
subjectedtothesameheavyexploitation
asweretemperateforestsafewgenerationsago.Pressuresfromlogging,mining,
hydropower,andahungerforlandare
leadingtolargeareasofforestbeingconvertedtoserveotherpurposes.Theintegrityofforestecosystemsisbeingaffected
asthetimberandpaperindustriesremove
vastareasofmaturetropicalandtemperate
forests.Asaconsequence,forestecosystemslosetheirabilitytosupportcomplex
biodiversityandthousandsofplantand
animalspeciesdisappearforever.
Severalgloballysignificantenvironmentaltrendsthathaveoccurredbetween
1980and2000mayalsobecontributingto
lossofforestecosystems,includingglobal
warming(thetwowarmestdecadeson
recordarethe1980sand1990s),threeintenseElNiñoevents,changesincloudiness
andmonsoondynamics,anda9.3
percentincreaseinatmosphericCO2.Althoughthesefactors,alongwithothers,are
thoughttoexerttheirinfluenceglobally,
theirrelativerolesarestillunclear.
Anobserveddeclineintropicalcloud
coverisprobablyoneofthemoreimportantrecentclimaticchanges,although
noneoftheexistingclimatemodelscan
accuratelysimulatethiseffect.Itisknown
thatcontinuedreductionsintropicalcloud
cover,ifaccompaniedbyreducedrainfall,
willhaveprofoundimplicationsfortropical
ecosystemsintermsofwaterstress,productivity,ecologicalcommunitycomposition,
anddisturbancepatterns.
ImagesofChange
Varioustypesofground-basedinstruments,
togetherwithinsitusurveysandanalyses,
canmeasuremanyofthechangesbeing
broughtaboutontheEarthasaresultof
humanactivities.Butsuchchangescan
alsobeobserved—inmoredetailandwith
a“bigpicture”perspective—fromspaceby
Earth-orbitingsatellitesthatgatherimages
oftheEarth’ssurfaceatregularintervals.
TheLandsatseriesofEarth-observing
satelliteshascompiledadatarecordofthe
planet’slandsurfacesthatspansthepast
thirtyyearsandcontinuestoday.
Bycomparingtwoimagesofthesame
areatakenten,twenty,oreventhirtyyears
apart,itisofteneasytoseehuman-induced
changesinaparticularlandscape.Few
placesremainonourplanetthatdo
notshowatleastsomeimpactfrom
humanactivities.
Thefocusofthischapterisasetof
specificcasestudiesinwhichsatelliteimages,takenatdifferenttimes,arepaired
soastorevealchangesandhumanimpacts
ontheatmosphere,oceansandcoastal
zones,freshwaterecosystemsandwetlands,
forests,croplands,grasslands,urbanareas,
andthetundraregions.
Thechangesthatweseeinpairsof
satelliteimagesshouldmakeuscautious.
Somearepositivechanges.Butmanymore
arenegative.Theseimagescouldbeseen
aswarningsigns.Attheleasttheyshould
provideuswithfoodforthoughtand
promptustoaskpointedquestions:How
canwebemoreprotectiveofourenvironment?Howcanweusetheenvironmentin
waysthatwillnotreducetheabilityofthe
Earthtosupportusinperpetuity?
Figure3.3:ThehightechboomhasbeenaccompaniedbyE-waste,whichrepresentsthelargestandfastest-growingtypeofmanufacturingwasteproduct.
RecyclingE-wasteinvolvesmajorproducersandusers,andtheshippingof
obsoleteequipmentandotherproductstoAsia,EasternEurope,andAfricawhere
recyclers,suchasthepeopleinthisphoto,areexposedtotoxicsubstances.Source:
http://www.grid.unep.ch/waste/html_file/36-37_ewaste.html
Credit:Unknown/UNEP/BaselActionNetwork
69
70
Credit:Unknown/UNEP/MorgueFile
71
3.1 Atmosphere
T
heEarth’satmosphereisacollecExosphere
tionofgases,vapor,andparticu400 km altitude
latesthattogetherformablanket
300 km
of“air”thatsurroundstheplanet.The
Thermosphere
atmosphereextendsover560km(348
50 km
Mesosphere
miles)fromthesurfaceoftheEarthout
40 km
Stratosphere
towardspace,andcanberoughlydivided
10 km
Troposphere
intofivemajorlayersorsections(Figure
3.4).Theprimarycomponentsoftheatmospherearethreegases:nitrogen(N2,78
percent),oxygen(O2,21percent),and
argon(Ar,1percent).Othercomponents,
presentinsmalleramounts,includewater
vapor(H2O,0-7percent),ozone(O3,0Figure3.4:TheEarth’satmosphereCredit:UsedwithpermissionfromCentreforAtmosphericScience,UniversityofCam0.01percent),andcarbondioxide(CO2,
bridge,UK.Source:http://www.atm.ch.cam.ac.uk/tour/atmosphere.html
0.01-0.1percent)(Phillips1995).
HumanactivitiesimpacttheEarth’s
OzoneDepletion
TheEarth’satmosphereplaysmany
atmosphereinmanyways.Someactivities
Ozoneisarelativelyunstablemolecule,
vitalrolesessentialtosustaininglifeon
produceaquitedirecteffect,suchasgenmadeupofthreeoxygenatoms(O3).In
theplanet.Theairwebreathecirculates
eratingandreleasingpollutantsthatfoul
theatmosphere,ozoneisformednaturally
throughitslowestlevel.Thechemicaleletheair,andaddingcarbondioxideand
inthestratosphere.Itisconcentrated
mentscarbon,nitrogen,oxygen,andhyothergreenhousegasestotheatmosphere
thereasan“ozonelayer”thatactsasa
drogen,whichareconstituentsofallliving thatinduceglobalwarmingandclimate
protectiveshieldagainstharmfulultraviothings,arecycledandrecycledintheatmo- change.Otherhumanimpacts,suchas
let(UV)radiationcomingfromtheSun.
sphere.Organismsconverttheseelements waterpollution,landdegradation,and
Thelossofstratosphericozoneallows
intocarbohydrates,proteins,andother
human-inducedlossofbiodiversity,can
moreUVradiationtoreachtheEarth’s
chemicalcompounds.Theatmosphere
indirectlyaffecttheatmosphere,aswellas
surface,whereitcancauseskincancerand
alsoshieldslifeontheplanet’ssurface
thewaterandland.
cataractsinpeopleandnegativelyaffect
fromharmfulsolarradiation,and—forthe
Inthissection,fourmajorissuesthatin- otherlivingthingsaswell.
mostpart—fromthethreatofmeteorites,
volvehumanimpactsontheatmosphere—
whichtypicallyburnupastheygothrough
Ozoneisalsofoundinthetroposphere,
ozonedepletion,globalwarming,climate
theatmosphere(UNEP1999a).
thelayeroftheEarth’satmospherethatis
change,andairpollution—areaddressed.
closesttotheplanet’ssurface.Ozonecan
Credit:ImageAnalysisLaboratory/UNEP/NASAJohnsonSpaceCenter
72
Credit:ImageAnalysisLaboratory/UNEP/NASAJohnsonSpaceCenter
beformednaturallyinthetroposphere—
forexample,bylightning.However,
troposphericozoneisalsoabyproductof
certainhumanactivities.Vehicleexhaust
contributeslargequantitiesofozonetothe
troposphereeachyear.
Dependingonwhereozoneresides,
itcanprotectorharmlifeontheEarth
(Figure3.5).Inthestratosphere,ozone
is“good”asitshieldslifeonthesurface
fromharmfulsolarradiation.Inthetroposphere,ozonecanbe“bad”asitbecomes
atypeofairpollution.Changesinthe
amountofozoneineitherthestratosphere
orthetropospherecanhaveserious
consequencesforlifeontheEarth.For
severaldecades,“bad”troposphericozone
hasbeenincreasingintheairwebreathe,
while“good”stratosphericozonehasbeen
decreasing,graduallyerodingtheEarth’s
protectiveozoneshield(Thompson1996).
Sincethelate1970s,scientistshave
detectedaslowbutsteadydeclineinthe
amountofozoneinthestratospheric
ozonelayer.Thisozonedestructionresultsfromthepresenceofcertaintypes
ofchemicalsintheatmosphere,especiallychlorofluorocarbons(CFCs)and
otherchlorine-andbromine-containing
compounds,coupledwithfluctuationsin
stratospherictemperature.
Inpolarregions,particularlythearea
oftheatmospherethatoverliesAntarctica,
ozonedepletionissogreatthatan“ozone
hole”formsinthestratospherethereevery
Stratosphere:
Earth
Troposphere:
In this region, ozone
is “good.” It protects
us from the sun’s
harmful ultraviolet
radiation.
In this region, ozone is
“bad.” It can damage
lung tissure and plants.
Mesosphere
Ozone in the Earth’s Atmosphere
Figure3.5:OzoneinthestratosphereformstheprotectiveozonelayerthatshieldstheEarth’ssurfacefromharmfulsolarradiation.Ozoneinthetroposphere,thelowestpartoftheatmosphere,
canbeaformofairpollution.Source:http://www.atmos.umd.edu/~owen/CHPI/IMAGES/ozonefig1.html
73
24 Sep 2003
06 Sep 2000
Ozone • Total Ozone Mapping Spectrometer (TOMS)
Figure3.6:Everyaustralspring,anareaofseverestratosphericozonedepletion—an“ozone
hole”—formsintheatmosphereoverAntarctica.Theozoneholesthatformedin2000and2003
werethelargestandsecondlargestonrecord,respectively.Source:http://www.gsfc.nasa.gov/gsfc/earth/
pictures/2003/0925ozonehole/still_hires_24Sept2003.tifandhttp://www.gsfc.nasa.gov/ftp/pub/ozone/ozone_still_2000_09_06.tif
(NASA2004a)
australspring(lateAugustthroughearly
October).Inthepastfewyears,theAntarcticozoneholehasbeenaboutthesize
ofNorthAmerica.In2000,theAntarctic
ozoneholewasthelargestonrecord,
covering29.6millionkm2(11.4million
squaremiles).Intheaustralspringof
2003,itwasalmostaslarge,covering28.9
millionkm2(11.1millionsquaremiles)
(Figure3.6).
lostduringthewinterandearlyspringof
1999-2000(Shah2002).
Someozone-depletingchemicals,such
asCFCs,alsocontributetoglobalwarming.Likecarbondioxideandmethane,
CFCsarepowerfulgreenhousegases
thattrapheatradiatingfromtheEarth’s
surfaceandpreventitfromimmediately
escapingintospace.Thiscausesthepart
oftheatmospherenearesttheEarth’ssurSeasonalozonedepletionisalso
facetowarm,resultinginglobalwarming.
noticeablearoundtheNorthPole.More
Thiswarminginthetroposphere,howthan60percentofstratosphericozone
ever,leadstocolder-than-normaltemperanorthoftheArctic turesinthestratosphere.This,inturn,
enhancestheformationofcertaintypesof
Circlewas
stratosphericcloudsthatfosterozone-de
stroyingchemicalreactionsinthestrato
sphere(Shanklinn.d.).
Fortunately,bansagainsttheproductionanduseofCFCsandotherstratosphericozone-destroyingchemicalsappeartobeworkingtoreversethedamage
thathasbeendonetotheozonelayer.In
thepastfewyears,theAntarcticozone
holehasnotincreasedsignificantlyinsize
Figure3.7:GrowthoftheAntarcticozone
holeover20years,asobservedbythesatellite-borneTotalOzoneMappingSpectrometer
(TOMS).Darkestblueareasrepresentregions
ofmaximumozonedepletion.Atmospheric
ozoneconcentrationismeasuredinDobson
Units.A“normal”stratosphericozonemeasurementisapproximately300DobsonUnits.
Measurementsof220DobsonUnitsandbelow
representsignificantozonedepletion.Source:
http://www.gsfc.nasa.gov/topstory/2004/0517aura.html
1979
1988
1982
1986
1984
74
Credit:JohnBortniak/UNEP/NOAA
orintensity.Someresearcherspredictthat
ifatmosphericconcentrationsofozone-destroyingchemicalsdroptopre-ozone-hole
levels,theAntarcticozoneholeshoulddisappearinapproximately50years(Figure
3.7)(WMO-UNEP2002).
GlobalWarming
Atmospherictemperatureandchemistry
arestronglyinfluencedbytheamount
andtypesoftracegasespresentinthe
atmosphere.Examplesofhuman-made
tracegasesarechlorofluorocarbons,such
asCFC-11,CFC-12,andhalons.Carbon
dioxide,nitrousoxide,andmethane(CH4)
arenaturallyformedtracegasesproduced
bytheburningoffossilfuels,
releasedbylivingand
deadbiomass,
andresultingfromvariousmetabolic
processesofmicroorganismsinthesoil,
wetlands,andoceans.Thereisincreasing
evidencethatthepercentagesofenvironmentallysignificanttracegases(greenhousegases)arechangingduetoboth
naturalandhumanfactors,andcontributingtoglobalwarming.
Globalwarmingisrecognizedasoneof
thegreatestenvironmentalthreatsfacing
theworldtoday.Globalwarmingisthe
gradualriseoftheEarth’saveragesurface
temperaturecausedbyanenhancingofthe
planet’snaturalgreenhouseeffect.Radiantenergyleavingtheplanetisnaturally
retainedintheatmospherethankstothe
presenceofcertaingasessuchaswater
vaporandcarbondioxide.Thisheat-trappingeffectis,infact,whatmakeslifeonthe
Earthpossible.
effect.TheEarth’saveragesurfacetemperature,whichhasbeenrelativelystable
formorethan1000years,hasrisenby
about0.5degreesCelsiusinthepast100
years(Figure3.8).Theninewarmest
yearsinthe20thcenturyhavealloccurred
since1980;the1990swereprobablythe
warmestdecadeofthesecondmillennium
(IPCC2001).
Globalwarminghasoccurredinthedistantpastastheresultofnaturalinfluences.
However,sincetheindustrialera,theterm
ismostoftenusedtorefertothecurrent
warmingpredictedasaresultofincreases
intheatmosphericconcentrationsofcertainheat-trappinggreenhousegasesgeneratedbyhumanactivities(Figure3.9).
Mostscientists
Globalwarming,bycontrast,isan
intensificationoftheEarth’sgreenhouse
1990
1999
1997
1992
1994
75
Figure3.8:SatellitedataofArcticregionsshow
warmingistakingplacethereatanacceleratingrate.Thesetwomapsshowtemperature
anomaliesintheArcticin1981andin2003.
Theanomaliesrangefrom7ºC(12.6ºF)below
normalto7ºC(12.6ºF)abovenormal.Shades
76
oforangeandredshowareasofwarming;
shadesofblueshowsareasofcooling;white
representslittleornochange(mapadapted
fromComiso).Thedatarevealthatsomeregionsarewarmingfasterthan2.5ºC(4.5ºF)per
decade(NASA2003b).
Source:http://svs.gsfc.nasa.gov/vis/a000000/a002800/
a002830/
believethatmuchofthisglobaltemperatureincreaseisduetoincreaseduseof
fossilfuels,whichwhenburned,release
carbondioxideintotheatmospherewhere
itabsorbsinfraredradiationthatnormally
wouldpassthroughtheatmosphereand
traveloutintospace(Brehm2003).
Theplanetisnotaswarmasitwasapproximately1000yearsago(Figure3.10).
Nevertheless,CO2currentlyaccountsfor
thegreatestproportionofgreenhousegas
emissions.MuchoftheCO2addedtothe
atmospherecomesfromtheburningof
fossilfuelsinvehicles,forheating,
andfortheproductionofelectricity
(Figure3.11).
Figure3.9:Humanactivitiesdirectlyinfluencetheabundanceofgreenhousegasesandaerosolsin
theatmosphere.Carbondioxide,nitrousoxide,methane,andsulfuraerosolshaveallincreased
significantlyinthepast50years.Source:IntergovernmentalPanelonClimateChange,IPCC(2001)
Figure3.10:VariationsintheEarth’stemperatureforthepast140years(global)andforthepast
1000years(NorthernHemisphere).Source:IPCC(2001)
Inadditiontocarbondioxide,risinglevelsofmethaneintheatmosphere
arealsoofconcern.Therelativerateof
increaseofmethanehasgreatlyexceeded
thatofcarbondioxideinthelastseveral
decades.Methaneisreleasedintothe
atmosphereinmanyways:asaresultofagricultureandranchingactivities;through
thedecayoforganicmatter,including
wastedumps;throughdeforestation;and
asaby-productofthehydrocarboneconomy.Noneofthesesourcesareanticipated
todecreaseinthefuture.Onthecontrary,
methaneemissionsareexpectedtoincrease,aseachyearanadditional100millionpeoplerequirefoodandfuelasworld
populationexpands(Figure3.12).
Mostscientistsbelievethatrecent
globalwarmingismainlyduetohuman
activitiesandrelatedincreasesinconcentrationsofgreenhousegases(Figure3.13),
primarilyCO2,CH4,nitrousoxide(N2O),
hydrofluorocarbons(HFCs),perfluorocarbons(PFCs),andsulfurhexafluoride
(SF6).Thesechangesaredrivenbyworldwidepopulationandeconomicgrowth,
andtheunderlyingproductionand
consumptionoffossilfuels,aswellasby
theintensificationofagriculturalactivity
andchangesinlanduseandlandcover.
Energyproductionanduse,thelargest
solesourceofCO2emissionsandalarge
contributorofCH4andN2Oemissions,accountedfor81.7percentofemissionsin
industrialisedcountriesin1998
(UNFCCC2000).
Fromfaroutinspace,instruments
carriedaboardsatellites,suchasNASA’s
77
ModerateResolutionImagingSpectroradiometre(MODIS)sensor,aretakingthe
temperatureoftheEarth’ssurface.SatellitedataconfirmthattheEarth’saverage
surfacetemperaturehasbeenslowlyrising
forthepastfewdecades(Figure3.14).
Satelliterecordsaremoredetailedand
comprehensivethanpreviouslyavailable
groundmeasurements,andareessential
forimprovingclimateanalysesandcomputermodeling.
Oneofthemorepredictableeffectsof
globalwarmingwillbeariseinsealevels
(Figure3.15).Itisalreadyunderwayat
apaceofaboutamillimetreayear—a
consequenceofbothmeltinglandiceand
thethermalexpansionoftheoceans(HarrisonandPearce2001).Predictionsasto
howmuchglobalsealevelsmayriseover
thenextcenturyrangefromhalfametre
(1.5feet)(Houghtonetal.2001)tobetween1and2m(3to6feet)(Nichollset
al.1999).Suchanincreasewoulddrown
manycoastalareasandatollislands.Unlesscountriestakeactiontoaddressrising
sealevels,theresultingfloodingisexpectedtoimpactsome200millionpeople
worldwidebythe2080s.Inaddition,
around25percentoftheworld’scoastal
wetlandscouldbelostbythistimedueto
sea-levelrise(DETR1997).
Globalwarmingmayhavesomepositiveimpacts.Itcould,forexample,open
Figure3.11:Between1971and1998,energyuseandcarbondioxideemissionsbothincreased
significantly,contributingtothelikelihoodofglobalwarming.Source:IPCC(2001)
Figure3.12:Methaneisthesecondlargestcontributortoglobalwarminganditsatmospheric
concentrationhasincreasedsignificantlyoverthelasttwodecades.Methaneemissionsfrom
human-relatedactivitiesnowrepresentabout70percentoftotalemissions,asopposedtoless
than10percent200yearsago.Source:IPCC(2001)
Figure3.13:Theroleofdifferentgasesandaerosolsinglobalwarming.Source:IPCC(2001)
Figure3.14:Globalwarmingisanincreasein
theEarth’saveragesurfacetemperature.These
graphsillustratehowashiftinthemeantemperatureanditsvariancecanaffectweather.Source:
IPCC(2001)
78
Figure3.15:ReasonsforsealevelchangeSource:IPCC(2001)
newlandsforagricultureandforestryin
thefarnorth.Duringthepast30yearsin
Iceland,oldfarmlandshavebeenexposed,
andarebeingused,astheBreidamerkurjökullGlacierhasreceded.Alltold,
however,thenegativeimpactsofuncheckedglobalwarmingoutweighany
positivebenefits.
ClimateChange
Climateisthestatisticaldescriptionin
termsofthemeanandvariabilityofrelevantmeasuresoftheatmosphere-ocean
systemoverperiodsoftimerangingfrom
weekstothousandsormillionsofyears.
Climatechangeisdefinedasastatistically
significantvariationineitherthemean
stateoftheclimateorinitsvariability,
persistingforanextendedperiod(typically
decadesorlonger).Climatechangemaybe
duetonaturalinternalprocessesortoexternalforcing(Figure3.16).Volcanicgases
anddust,changesinoceancirculation,
fluctuationsinsolaroutput,andincreased
concentrationsofgreenhousegasesinthe
CaseStudy:EuropeanHeatWave
July2003
Thisimageshowsthedifferences
indaytimelandsurfacetemperatures
(temperatureanomalies)collectedover
EuropebetweenJuly2001andJuly2003
bytheModerateResolutionImaging
Spectroradiometer(MODIS)onNASA’s
Terrasatellite.Ablanketofdeepredacross
southernandeasternFrance(leftofimagecenter)revealsthattemperaturesin
thisregionwere10ºC(18ºF)hotterduring2003thanin2001.Temperatureswere
similarinwhiteareasandcoolerinblue
areas.Althoughmodelspredictanoverall
increaseinglobalaveragetemperatures,
regionaldifferencesmaybepronounced,
andsomeareas,suchasmid-continental
zonesinNorthAmericaandAsia,may
actualyexperiencesomedegreeofcooling
(NASA2003c).
EuropeanHeatWave,July2003Credit:NASA—
SatelliteThermometersShowEarthHasaFever(2004)
79
atmospherecanallcauseclimatechanges
(USCCSP2003).
Globalwarming,whateveritsunderlyingcauses,isexpectedtohaveadverse,
possiblyirreversibleeffectsontheEarth’s
climate,includingchangesinregionaltemperatureandrainfallpatternsandmore
frequentextremeweatherevents.Climate
changewillaffecttheecologyoftheplanet
byimpactingbiodiversity,causingspecies
extinctions,alteringmigratorypatterns,
anddisturbingecosystemsincountless
ways.Climatechangewillimpacthuman
societiesbyaffectingagriculture,water
supplies,waterquality,settlementpatterns,
andhealth.
Overall,climatechangeislikelytointensifythealreadyincreasingpressureson
varioussectors.Althoughtheimpactofclimatechangemay,insomecases,besmaller
thanotherstressesontheenvironment,
evenrelativelysmallchangescanhaveseriousadverseeffects,especiallywherethere
maybecriticalthresholds,where
Figure3.16:Climatechangeistheresultofcomplexinteractionsamongmanyfactors.Source:IPCC(2001)
developmentisalreadymarginal,orwhere
aregionislessabletoimplementadaptabeingputonwaterresourcesbyagrowing elsindicatethattheremaybeanadditional
tionmeasures(DETR1997).
globalpopulation,particularlyinAfrica,
100millionpeoplelivingincountrieswith
CentralAmerica,theIndiansubcontinent, extremewaterstressduetoclimatechange
Forexample,climatechangeislikely
andsouthernEurope.Bythe2050s,modalone(DETR1997).
toexacerbatealreadyincreasingpressure
Credit:Unknown/UNEP/Topfoto
80
Carbondioxide,thegaslargelyblamed
forglobalwarming,hasreachedrecordhighlevelsintheatmosphere(Hanley
2004).Carbondioxidelevelshaverisen
by30percentinthelast200yearsasa
resultofindustrialemissions,automobiles,
andrapidforestburning,especiallyinthe
tropics.Muchofthisincreasehasoccurred
since1960.ThisincreaseinCO2isthought
toenhancetheEarth’snaturalgreenhouse
effectandthusincreaseglobaltemperatures(Figure3.17).
TheIntergovernmentalPanelonClimateChangeprojectsthat,ifunchecked,
atmosphericcarbondioxideconcentrationswillrangefrom650to970ppmby
2100.Asaresult,thepanelestimates,averageglobaltemperaturemayriseby1.4ºC
(2.5ºF)to5.8ºC(10.4ºF)between1990and
2100(Hanley2004).
Interestingly,increasedlevelsofatmosphericCO2maystimulatethegrowthof
somekindsofplants.Researchersinthe
Amazonhavenotedincreasedgrowthrates
inseveralspeciesoftrees(Lauranceetal.
2004).Theforestsarealsobecomingmore
dynamic,withexistingtreesdyingandbeingreplacedbynewtreesatamorerapid
pace.Inaddition,thespeciescomposition
oftheforestischanging.RisingatmosphericCO2concentrationsmayexplainthese
changes,althoughtheeffectsofthisand
otherlarge-scaleenvironmentalalterations
remainuncertain.
Figure3.17:Formorethan40years,researchersatMaunaLoaObservatory,Hawaii,havetrackedthesteady
increaseofatmosphericcarbondioxide(concentrationexpressedinpartspermillion,orppm).Source:SIO
(2004)andSeaWiFS:NASACarbonCycleInitiative,NASA/GoddardSpaceFlightCenterScientificVisualizationStudio(2004).
Source:NASA(2004b)
burningoffossilfuelsandthealterationof
naturallandcover,alsogenerateaerosols.
Averagedovertheglobe,human-generatedaerosolscurrentlyaccountforabout
tenpercentoftotalatmosphericaerosols.
Mostofthoseaerosolsareconcentrated
intheNorthernHemisphere,especially
downwindofindustrialsites,slash-andburnagriculturalregions,andovergrazed
grasslands(Figure3.18).
AsthecompositionofEarth’satmospherechanges,sodoesitsabilitytoabAirPollution
sorb,reflectandretainsolarenergy.GreenAirpollutionisthepresenceofcontamihousegases,includingwatervapor,trap
nantsorpollutantsubstancesintheairthat
heatintheatmosphere.Airborneaerosols
interferewithhumanhealthorwelfare
fromhumanandnaturalsourcesabsorbor
orproduceotherharmfulenvironmental
reflectsolarenergybasedoncolour,shape,
effects(EEA2004).Theterm“smog”—first
size,andsubstance.Theimpactofaerosols,
coinedinLondon,England,todescribe
troposphericozone,anduppertropospheracombinationofsmokeandfog—isnow
usedinreferencetoaspecificcombination Figure3.18:Aerosolparticleslargerthan1micrometrearecomposedprimarilyofwindblowndust
ofairborneparticles,gases,andchemicals
andseasaltfromseaspray.Aerosolssmallerthan
1micrometrearemostlyformedbycondensation
thattogetheraffectpeoples’healthand
processes,suchastheconversionofSO2gasreleased
theirnaturalenvironment(Health
byvolcaniceruptionstosulfateparticlesandbyformationofsootandsmokeduringburningprocesses.
Canada2003).
Aerosolsaretinyparticlessuspended
intheair.Someoccurnaturally,originatingfromvolcanoes,duststorms,forest
andgrasslandfires,livingvegetation,and
seaspray.Humanactivities,suchasthe
icwatervaporonEarth’sclimateremains
largelyunquantified(NASA1989).
About25percentoftheworld’spopulationisexposedtopotentiallyharmful
amountsofSO2,O3,andparticulatematter
insmog(Schwela1995).Globally,some50
percentofcasesofchronicrespiratoryillnessarenowthoughttobeassociatedwith
airpollution(UNEP1999b).
Somepollutantstravellongdistances
onthewind,causingaciddepositionin
thesurroundingcountrysideandevenin
neighboringcountries.Inthe1980s,“acid
rain”wasidentifiedasamajorinternationalenvironmentalproblem,movingfrom
Afteraerosolsform,theyaremixedandtransported
throughouttheatmospherebywindandweather;they
areremovedfromtheatmosphereprimarilythrough
cloudformationandprecipitation.Source:http://earthobservatory.nasa.gov/Library/Aerosols/(NASA2004c)
81
Fig.3.19:Aerosolsaffectclimatebothdirectlybyreflectingandabsorbingsunlightandindirectlybymodifyingclouds.TheTotalOzoneMappingSpectrometer
(TOMS)aerosolindexisanindicatorofsmokeanddustabsorption.Thisfigureshowsaerosols—thehazygreen,yellow,andredpatches—crossingtheAtlanticand
PacificOceans.DustfromtheSaharaDesertiscarriedwestwardtowardtheAmericasandprovidesnutrientsforAmazonforests.Asiandustandpollutiontravelto
thePacificNorthwest.Source:NASA(http://www.gsfc.nasa.gov/topstory/2004/0517aura.html)(NASA2004a)
heavilyindustrializedareasofbothEurope
andNorthAmericaintoprimeagricultural
areasthatlaydownwind.Mountainregions
sufferedthemostbecausetheirhigher
rainfallincreasedthevolumeofaciddepositionandtheiroftenthinsoilscouldnot
neutralizetheacid.Lakesandstreamsin
pristinepartsofScandinaviaandScotland
becameacidified,andfishpopulations
weredecimatedinsomeareas.Themost
intenseacidrainfalloutoccurredinthe
so-calledBlackTriangleregionbordered
byGermany,CzechRepublic,andPoland
(HarrisonandPearce2001)(Figure3.19).
Acidprecipitationdecreasedthroughoutthe1980sand1990sacrosslargeportionsofNorthAmericaandEurope.Many
recentstudieshaveattributedobserved
reversalsinsurface-wateracidificationat
nationalandregionalscalestothisdecline(Stoddardetal.1999;Larssen2004).
82
Decreasesinacidprecipitationhavebeen
achievedlargelythroughimprovedfluegas
treatments,fuelswitching,useoflow-sulfur
fuelsinpowerstations,anduseofcatalytic
convertersinautomobiles.Since1985,
internationaltreatiesandheavyinvestment
indesulphurizationequipmentbypower
stationoperatorshavecutsulfurpollution
inEuropeandNorthAmericabyasmuch
as80percent(HarrisonandPearce2001).
thosemadeinEuropeandNorthAmerica
overthepast20years(Downing1997;
WRI1998).
Nitrogendioxideistheorangegasthat
isthemostvisiblecomponentofmostair
pollution.Inmanycities,NO2andother
pollutantsaresuspendedintheairtoform
abrownishhazecommonlycalledsmog.
Nitrogendioxideisformedwhenoxygen
intheaircombineswithnitricoxide.
Althoughsignificantprogresshasbeen Nitricoxidecomesfromautomobiles,
madeincontrollingacid-formingemissions aerosols,andindustrialemissions,and
insomecountries,theglobalthreatfrom
contributestotheformationofacidrain.
acidprecipitationstillremains.Infact,the Inaddition,thispollutantcancauseawide
problemisgrowingrapidlyinAsia,where
rangeofenvironmentaldamage,including
1990s-levelSO2emissionscouldtripleby
eutrophicationofwaterbodies—explosive
2010ifcurrenttrendscontinue.Curtailing algaegrowththatcandepleteoxygenand
thealreadysubstantialacidprecipitation
killaquaticorganisms.
damageinAsia,andavoidingmuchmore
severedamageinthefuture,willrequire
investmentsinpollutioncontrolsimiliarto
CaseStudy:EmissionsinParis
1999-2003
Paris,France,liesonarelativelyflatplain.
Mostofthetime,Parisbenefitsfromawet
andwindsweptoceanicclimatethatencouragesthedispersalofairpollutionand
thuscleanstheair.However,undercertain
meteorologicalconditions(anticyclones
andalackofwind),pollutantscanremain
trappedintheatmosphereabovethecity,
wheretheybecomeconcentrated,resulting
insignificantlyhigherlevelsofpollution.
Thus,forequivalentpollutantemissionsin
termsoflocationandintensity,thelevelsof
pollutantsrecordedintheatmospherecan
varybyafactorof20accordingtometeorologicalconditions.
AnnualSO2emmissionsintheParisregion
AnnualNOxemmissionsintheParisregion
AnnualCOemmissionsintheParisregion
AnnualVOCemmissionsintheParisregion
Thisexplainswhypeaksinsecondary
pollutantsoftenaffectwiderareasthan
peaksinprimarypollutants.Forexample,
whenthewindblowsfromthecityina
ConcentrationsofSO2,NOx,CO,andVOCoverParis.Source:http://www.airparif.asso.fr/english/polluants/default.htm
certaindirection,theruralareasurroundingtheParisregionisalsosubjecttoozone
pollution.Indeed,ozonelevelsregistered
Regionalcartographyoftheannuallevelof
intheseareasareoftenmuchhigherthan AnnualaveragesofSO2inIle-de-Francefrom
1999to2003
benzeneevaluatedwithintheframeworkofthe
thoseinthecentreofParisitself.
EuropeanprojectLIFE“RESOLUTION”
In1994,accordingtotheCentre
InterprofessionnelTechniqued’Etude
delaPollutionAtmosphérique(CITEPA,
Inter-professionalTechnicalCentrefor
ResearchintoAirPollution)SO2emissions
intheParisregioncorrespondedtoeight
percentofnationalemissions(mainland
Franceandoverseasterritories),oxides
ofnitrogen(NOx)emissionsto10
percent,VolatileOrganicCompound
(non-methane)(VOCNM)emissionsto12
percent,carbonmonoxide(CO)emissionsto15percent,andCO2emissionsto
14percent.Giventhat19percentofthe
populationlivesintheParisregion,emissionsperinhabitantinthisareaareless
thanthenationalaverageforallsubstances
(CITEPA1994).
Existingair-quality-monitoringtools
inthegreaterregionofParisprovidea
constantindicationofairpollutionlevels
atspecificbackgroundandroadsidelocations.Inadditiontostandardmonitoring,
specificmodelingapplicationsgiveextensivedescriptionsofair-qualitypatterns
forseveralsignificantpollutants.Despite
AirqualitydynamicsovertheregionofParis,France,from1999to2003.Source:http://www.airparif.asso.fr/eng-
lish/polluants/default.htm
theinvolvementofthetransportsectorin
monitoringlocalatmosphericemissions,
thereisnodirectandconstanttraffic
datafeed.Recently,aprojectknownas
HEAVEN(HealthierEnvironmentthrough
theAbatementofVehicleEmissionsand
Noise)wasimplementedinParis.Itsmain
objectivewastointegratereal-timetraffic
informationwiththeairqualitymonitoring
tools.HEAVENhelpeddevelopanddemonstratenewconceptsandtoolstoallow
citiestoestimateemissionsfromtrafficin
near-realtime.Thisenhancedtheidentificationandevaluationofthebeststrategies
fortransportdemandmanagement.
Souce:http://heaven.rec.org
83
CaseStudy:PollutionfromWildFires
2003–2004
ferentseasonscanbeeasilyidentifiedand
trackedovertimeonsuchimages,leading
tobetterunderstandingofsourcesofCO
Whetherstartedbypeopleornatural
pollutionanditstranscontinentaltransevents,firesaddlargequantitiesofpollutport(NASA2004d).Forexample,inthe
antstotheatmosphereeveryyear,primarilyintheformofCOandaerosols.Satellite summerimageofthisseries,averyhigh
concentrationofCOappearsoverwest
sensorscanhelpresearchersdistinguish
centralAfrica,largelyduetoforestfires.
betweenwildfiresandurbanorindustrial
WildfiresinsouthernAfricaareamafires.Somecanalsodistinguishdifferent
jorsourceofcarbonmonoxidepollution.
typesoffire-generatedpollutants.For
instance,twosensorsaboardNASA’sTerra EveryAugustinsouthernAfrica,thousandsofpeopleequippedwithlightersor
satellite—theMeasurementsofPollution
torchestraveloutontothesavannaand
intheTroposphere(MOPITT)instruintentionallysetthedrygrasslandsablaze.
mentandtheModerateResolutionImagBurnedgrassessenduptendernewgrowth
ingSpectroradiometer(MODIS)instruthatisidealforcattleconsumption.The
ment—gatherdataonCOandaerosols,
firestypicallyscorchanareathesizeof
respectively.
Montana,Wyoming,Idaho,andtheDakoCarbonmonoxideisoneofthemore
tascombined.Longplumesofsmokerise
easilymappedairpollutants.Inthe
likehundredsofbillowingsmokestacks,
MOPITT-generatedseriesofmapsshown
andherdsofanimalsaresentscurrying
below,globalseasonalvariationsinCO
acrossopengrassland.
concentrationareclearlyvisible(highestconcentrationsofCOappearasred).
MajorconcentrationsofCOduringdif-
Duringthisfireseason,athickpallof
smokecloudstheskyformanyweeks.The
smokeislacedwithanumberofpollutants,includingnitrogenoxides,carbon
monoxide,andhydrocarbons.Someof
thesesubstancesreactwiththeintense
heatandsunlighttoformozone.Groundlevelozonecontributestorespiratory
diseasesandcanseriouslydamagecrops.
Athigherlevelsinthetroposphere,ozone
moleculestrapthermalradiationemanatingfromtheEarth’ssurfaceinthesame
wayascarbondioxideandothergreenhousegasesdo.Infact,upto20percent
oftheglobalwarmingexperiencedbythe
Earthoverthepast150yearsisthoughtto
befromozone.
Inthespringof2003,theMODISand
MOPITTinstrumentswereusedtomonitorfiresandfire-producedairpollutants
inSiberia,especiallyintheBaikalregion.
Thesefiresproducedlargeamountsoffine
carbonaerosolsthatspreadoutoverthe
PacificOceanandremainedsuspended
intheatmosphereforafewdays.Carbon
monoxidewasalsoproducedbythefires,
NorthernHemisphereseasonalvariationinatmosphericcarbonmonoxideanditsglobaldistribution.Source:http://svs.gsfc.nasa.gov/vis/a000000/a002100/
a002150/(NASA2004d)
84
butunliketheaerosols,remainedairborne
foramuchlongerperiodoftime,allowing
ittocrossthePacificOceanandreduceair
qualityoverNorthAmericabeforecontinuingonaroundtheglobe.
Gasandparticleemissionsproduced
asaresultoffiresinforestsandother
vegetationimpactthecompositionofthe
atmosphere(WHO2000).Thesegasesand
particlesinteractwiththosegeneratedby
fossil-fuelcombustionorothertechnologicalprocesses,andaremajorcausesofurbanairpollution.Theyalsocreateambient
pollutioninruralareas.Whenbiomassfuel
isburned,theprocessofcombustionisnot
completeandpollutantsreleasedinclude
particulatematter,carbonmonoxide,oxidesofnitrogen,sulfurdioxideandorganic
compounds.Onceemitted,thepollutantsmayundergophysicalandchemical
changes.Thus,vegetationfiresaremajor
contributorsoftoxicgaseousandparticle
airpollutantsintotheatmosphere.These
firesarealsosourcesof“greenhouse”and
reactivegases.Particulatepollutionaffects
morepeoplegloballyonacontinuing
basisthananyothertypeofairpollution.In1997/98,forestfiresinSoutheast
Asiaaffectedatleast70millionpeoplein
BruneiDarussalam,Indonesia,Malaysia,
thePhilippines,Singapore,andThailand.
Thousandsofpeoplefledthefiresand
smokeandtheincreaseinthenumberof
emergencyvisitstohospitalsdemonstrated
theseverityofthefiresandpollutionthey
caused(WHO2000).
CaseStudy:AfricanFires
2002
Wildfires—fromforestfiresandbrushfires
tograssfiresandslash-and-burnagriculture—canbesweepinganddestructive
conflagrations,especiallyinwildernessor
ruralareas.Asbiomassburns,particulates,
blackcarbon,andgasesincludingCO2,
CO,NOx,CH4,andCH3Clareproduced
ingreatquantities.Allofthesepollutants
canbeloftedrelativelyhighintheatmosphereduetotheconvectiveheatingofa
ragingfire(GraedelandCrutzen1993).
Theimageatrightshowsfireactivityin
Africafrom1January2002to31December2002.Thefiresareshownastinydots
witheachdotdepictingthegeographicregioninwhichfirewasdetected.Thecolor
ofadotrepresentsthenumberofdays
sinceasizableamountoffirewasdetected
Pollutionoutflowfromspring2003firesinSiberiacanbeseeninthetopandmiddleimage.
ThesefiresproducedlargeamountsoffinecarbonaerosoldetectedbyMODISinstrument
(brightcolours)ontheTerrasatellite,whichspreadoverthePacificOceanbutlastedonlyafew
days.Theyalsoproducedcarbonmonoxide,whichwasdetectedbytheMOPITTinstrumenton
theTerrasatellite(bottomimage).Thisgascanlastoveramonth,whichallowedittocrossthe
PacificOceanandreduceairqualityoverNorthAmericabeforecontinuingonaroundtheglobe.
Credit:DavidEdwards,TheNationalCenterforAtmosphericResearch(NCAR)(NASA2004e)
inthatregion,withred-orangerepresentinglessthan20days,orangerepresenting
20to40days,yellowrepresenting40to60
days,andgraytoblackrepresentingmore
than60days.Thesedataweregathered
bytheMODISinstrumentontheTerra
satellite.MODISdetectsfiresbymeasuring
thebrightnesstemperatureofaregionin
severalfrequencybandsandlookingfor
hotspotswherethistemperatureisgreater
thanthesurroundingregion.
Globalstatisticsontheamountofland
burnedworldwideeveryyearvaryconsiderably.Ithasbeenestimatedthatfrom
7.5millionto8.2millionkm2(4.6million
to5.1millionsquaremiles)areburned
andbetween1800millionand10000
millionmetrictonnesofdrybiomassare
consumedinfiresannually.Globalchange
scenariospredictanincreaseintotalarea
AfricanFiresduring2002Credit:http://svs.gsfc.nasa.
gov/vis/a000000/a002800/a002890/index.html(NASA2004f)
burned,withanincreaseinverylargeand
intensefires.
85
CaseStudy:PollutioninChina
2001and2004
DuringFebruary2004,aconsiderableoutflowofpollutionstemmedfromChinaand
SoutheastAsia.Theimageatrightshows
atmosphericconcentrationsofcarbon
monoxideatanaltitudeofroughly3km
(1.9miles)overthisregionthatweremovingacrossthePacificOceanandatsome
pointsreachingthewesterncoastofthe
UnitedStates.
Carbonmonoxideisagoodindicator
ofairpollutionsinceitisproducedduring
combustionprocesses,suchastheburning
offossilfuelsinurbanandindustrialareas,
aswellasbywildfiresandbiomassburninginmoreruralareas.Industrialemis-
sionsweremainly
responsibleforthe
highlevelsofcarbonmonoxideover
Chinainthisimage,
whereasemissionsin
SoutheastAsiawere
dueprimarilytoagriculturalfires.
Naturalprocessesandeventscan
alsobeasourceof
transcontinentalairpollution.In2001,a
largeduststormdevelopedoverChina(see
below).Prevailingwindssweptparticulates
fromthisstormallthewaytotheeastern
coastofNorthAmerica.
ThisimagewasdevelopedfromacompositeofcarbonmonoxidedatacollectedoverChinaandSoutheastAsiafrom1-25February2004,bytheMeasurementsofPollutionintheTroposphere(MOPITT)
instrumentaboardNASA’sTerrasatellite.Thecolors
representthemixingratiosofcarbonmonoxidein
theair,giveninpartsperbillionbyvolume.The
greyareasshowwherenodatawerecollecteddueto
persistentcloudcover.Source:http://earthobservatory.nasa.
gov/Natural(NASA2004g)
7April2001-Bluerepresentsjustslightlyhigher-than-normalaerosolsandredrepresentsthehighestconcentrationofaerosols.
6April2001normalaerosollevelsareapparentonthefirstdayoftheduststorm.
10April2001-Theaerosolimpactfromtheduststormcanclearlybeseenover
China,Mongolia,Russia,Korea,Japan,andthePacificOcean.
13April2001-Theaerosolimpactfromtheduststormcanclearlybeseenover
Japan,thePacificOcean,Alaska,andtheUnitedStates.
14April2001-Theaerosolimpactfromtheduststormcanclearlybeseeninthe
PacificOcean,andtheUnitedStates.
17April2001-HighlevelsofaerosolsarevisibleovertheEastCoastoftheUnited
States,especiallyMaine.
AlargeduststormdevelopedoverChinaon6-7April2001.Thisseriesofimagesshowsair-bornedustfromthestormmovingoverChina,Russia,Japan,
thePacificOcean,Canada,andultimatelyovertheUnitedStateson17April2001(NASA2004g).VisualizationCredit:NASA/GoddardSpaceFlightCenterScientific
VisualizationStudioSource:http://svs.gsfc.nasa.gov/vis/a000000/a002900/a002957/index.html
86
Credit:Chia/UNEP/MorgueFile
87
88
Credit:DarrenH.Holto/UNEP/Topfoto
89
3.2 Coastal Areas
O
ceanscoverroughly70percentoftheEarth’ssurfaceand
makeupsome90percentofspacehabitablebyliving
things.Theycontainavast,andlargelyunexplored,diversityoflife,fromthesmallestofmicroorganismstobluewhales,
thelargestmammalsontheEarth.Oceansareessentialforthe
ecologicalfunctionsandresourcestheyprovide,includingfood,
medicines,andenergyformillionsofpeopleworldwide(UNEPWCMC2003).
Theworld’soceanshaveagreateffectonglobalclimate.
Waterhasahighcapacityforretainingheat.Becausesomuchof
theEarth’ssurfaceiscoveredbyoceans,thetemperatureofthe
atmosphereiskeptfairlyconstantandwithintherangenecessarytosupportlife.Currently,theoceansalsomoderateclimate
changebyabsorbingathirdofthecarbondioxide(CO2)emitted
intotheairbyhumanactivity(HarrisonandPearce2001).However,globalwarmingmayreducetheocean’scapacitytoactasaCO2
sinkby10to20percentoverthenextcentury
(Houghtonetal.2001).
Differentpartsoftheglobal
oceanaffectclimatein
differentways.The
IndianOcean/West
PacificWarmPool,
forexample,isan
enormousexpanseofwarm
surfacewater.
Itextends
almosthalf
wayaround
theEarth,
stretchingalong
theequatorsouth
ofIndia,
throughthe
watersoff
Sumatra,Java,
Borneo,and
NewGuinea,
andintothecentralPacificOcean.
Thewatersofthe
WarmPoolarewarmer
thananyotherareaofopen
oceanontheEarth.Because
thesewatersarewarmtoenoughtodrivemoisturehighintotheatmosphere,theWarmPoolhasalargeeffecton
theclimateofthelandsthatsurroundit.Theslowfluctuationsin
sizeandintensityoftheWarmPoolmaybelinkedwiththeintensityoftheElNiñophenomenon.
Inadditiontotheocean’sclimate-bufferingcapacity,itssalty
waterscontainbillionsoftinyalgaeandotherplanktonicorganisms.Theselifeformscarryoutalargepartoftheoxygen-generatingphotosyntheticprocessesthatoccurontheplanet(Biomes
Group1996).Forpeople,oceansrepresentoneofthegreatest
sourcesoffoodontheEarthaswell.Globalfishproduction
exceedsthatofcattle,sheep,poultry,oreggs.Itrepresentsthe
largestsourceofwildordomesticproteinintheworld(UNEPWCMC2003).Marinefishcatchrosefrom51millionmetric
tonnesin1975tonearly70millionmetrictonnesin1999
(UNEP2002).
90
90
Coastalzones,whichincludebays,tidallands,estuaries,marinewetlands,mangroves,andcoralreefs,formaninterfacebetweenthelandand
theocean.Thetotallengthofalltheworld’scoastlinesisestimatedtobe
roughly1.6millionkm(1millionmiles)(Burkeetal.2000).
Manycoastalmarineecosystemsareamongthemostproductive
intheworld,richinlivingandnonlivingresources.Mangroves,for
example,extendover18millionhectares(44millionacres)worldwide,coveringaquarteroftheworld’stropicalcoastlines(Choudhury1997).Mangrovesprotectcoastlinesbyabsorbingtheforce
ofstorms.Theyprovidelargequantitiesoffoodandfuel,buildingmaterials,andevenmedicines.Mangrovesarealsocharacterizedbynutrient-richwatersthatsupportlargenumbersof
marineorganismsand,inmanycases,formnurserygrounds
forfishandothermarinespecies.Becauseoftheirtremendous
productivity,mangrovesandothercoastalecosystemsprovide
foodandlivelihoodformillionsofpeople.
Inmanywarm-oceanregionsoftheworld,coralreefsare
alsoassociatedwithcoastalzones.Coralreefsoccupylessthan
onetenthofonepercentoftheoceans(UN2002),yettheyare
amongthemostbiologicallydiverseecosystemsontheEarth,
hometomorethanamillionspecies.Thetotalareaofthemost
biologicallyproductivenearsurfacereefshasbeen
estimatedataround
255300km2
(98572square
miles)(Bryantet
al.1998).About
aquarterofthe
world’sfish
feed,reproduce,andlive
onornear
coralreefs
(Harrison
andPearce
2001).Coral
reefsarea
majorglobal
biological
andeconomic
resourcefor
bothfisheriesand
tourism,because
theyprotectvulnerablecoastlinesfrom
waveactionandstorms
(Bryantetal.1998).
Landadjacenttotheoceanis
atremendouslyvaluableresource.Coastalzonesareeconomically,
politically,andsociallycriticaltomanynations.Theyarehubsof
commerceandhometomanymajorcorporationsandtransportationnetworks.
Coastallandscapesofferfertilesoils,flatlandforurbandevelopment,andsheltered,deep-waterbaysforharborsandports.
Coastsareusedbymillionsofpeopleannuallyforrecreationand
theysupportagrowingtouristtrade.Althoughcoastalzonesaccountforonly20percentoftheworld’slandarea,amajorityof
theworld’shumanpopulationinhabitthem.Halfoftheworld’s
population—some3000millionpeople—liveswithin200km
(124miles)ofacoast.By2025thatfiguremaydouble,risingto
sixbillionpeople(Cohenetal.1997).
Theoceansareaseeminglylimitlessandenduringresource.
Butthey,andthecoastalzonesthatencirclethem,arecurrentlyat
riskalongmanyfronts.In1995,FAOreportedthat52percentofthe
91
Credit:Chansareek/UNEP/Topfoto
oceans’wildfishstockswerebeingexploitedatthemaximumsustainablelimit,
16percentwerealreadyoverexploited,
andsevenpercentweredepleted.Only
23percentwillbeabletosustainfurther
expansion.(FAO2005).In24countriesfor
whichsufficientdatawereavailable,trawlinggroundsencompass8.8millionkm2
(3.4millionsquaremiles),ofwhichabout
5.2millionkm2(2millionsquaremiles)
arelocatedoncontinentalshelves.This
representsabout57percentofthetotal
continentalshelfareaofthesecountries
(Burkeetal.2000).
However,notallofthedeclinein
oceanfisheriesmaybeattributedtofish-
ing.Globalwarmingmayalsobepartlyto
blame(Beaugrandetal.2003).Thedepletionofnaturalfishstockshasprompted
expansionofaquaculture—thefarmingof
fish—inmanyareas,areactiontoocean
degradationthatdoesprovideemployment
andfood,butalsocarrieswithitthepotentialforpollutionandotherconcerns.
CaseStudy:DumpingofRadioactive
WasteatSea
TheReportoftheUnitedNationsConferenceonHumanEnvironmentheldin
Stockholmin1972definedtheprinciples
forenvironmentalprotection,specifically
fortheassessmentandcontrolofmarine
pollution.Thesewereforwardedtoan
Inter-GovernmentalConferenceheldin
Londonlaterthatyear,wheretheConventiononthePreventionofMarinePollution
byDumpingofWastesandOtherMatter
(alsoknownastheLondonConventionof
1972)wasadoptedandwhichenteredinto
forceon30August1975.
ThecontractingpartiestotheLondon
Conventionagreedtopromotetheeffectivecontrolofallsourcesofpollutionof
themarineenvironmentandtotakeall
practicablestepstopreventthepollution
oftheoceanbydumpingofwasteandothermatterthatisliabletocreatehazardsto
humanhealthandtoharmlivingresources
andmarinelife.TheInternationalAtomic
EnergyAgency(IAEA)wasdesignatedas
theinternationalbodythatshouldoversee
mattersrelatedtothedisposalofradioactivewastesintheocean.
92
ThefigureshowsthegeographicaldisThefirstreportedoceandisposaloperationofradioactivewastewascarriedoutby tributionofdisposaloperations.
Source:Modifiedfromhttp://www.oceansatlas.org/servlet/CDSSe
theUSAin1946intheNorth-EastPacific
Oceanandthelatestwascarriedoutbythe rvlet?status=ND0xNDExMyY3PWVuJjYxPSomNjU9a29z.Figure
hasbeenmodifiedfromhttp://www.oceansatlas.com/unatlas/
RussianFederationin1993intheJapan
about/physicalandchemicalproperties/radiosp/index.htm.
Sea/EastSea.Duringthe48yearhistoryof
seadisposal,14countrieshaveused
morethan80sitestodisposeofapproximately85PBq(1PBq=1015Bq)of
radioactivewaste.
GlobalMapofDeadZones
Oceanpollutionisagrowingand
seriousproblem.Mostofthewastesand
contaminantsproducedbyhumanactivitieseventuallyendupintheoceans.
Chemicalcontaminationandlitterexist
fromthepolestothetropicsandfrom
beachestooceandepths.Somepollutants
aredirectlydrainedordumpedintothe
oceans,eitherintentionally,oraccidentally
asinthecaseofoilspills.Currently,the
oceansmustabsorbanestimated3million
tonnesofoilspilledannuallyfromships
and,predominantly,fromsourcesonland
(HarrisonandPearce2001).Otherocean
pollutantsfirstentertheatmosphereand
latersettleonoceanwaters.Riversthat
flowintooceanscarryrunofffromcity
streets,sewage,industrialwastes,pesticides
andfertilizersfromcropland,andsiltfrom
land-clearingandconstructionprojects.
Becauseoftheirproximitytoland,coastal
waterstendtohavefarhigherconcentrationsofpollutantsthantheopenocean
(UNEP-WCMC2003).
Pollutedwaterscanupsettheecological
balanceamongspeciesinmarinesystems.
Forexample,thenumberofpoisonous
algalspeciesidentifiedbyscientistshas
nearlytripledsince1984,increasingfish
kills,beachclosures,andeconomiclosses.
LargepartsoftheGulfofMexicoarenow
consideredbiologicaldeadzonesdue
toalgalblooms(UN2002).Deadzones
arecoastalareasinwhichbottomwaters
(thoseneartheoceanfloor)containvery
littledissolvedoxygen.Thiscondition
iscalledhypoxia,meaning“lowoxygen”
(ESA2003).Veryfeworganismsare
abletosurviveinoceandeadzones(Figure3.20).ThedeadzoneintheGulfof
Figure3.20:Themapaboveshows58reportedocean
deadzonesin1995.Theoldestandmostwell-studied
marinedeadzonesarefoundintheGulfofMexico,
theBlackSea,andtheBalticSea.In1995,themost
severecaseofhypoxiawasintheBalticSea,inwhich
aboutone-third,or98800km2(38000squaremiles),
ofthebodyofwaterwasreportedlifeless.Source:
Modifiedfrom:http://daac.gsfc.nasa.gov/CAMPAIGN_DOCS/
OCDST/dead_zones.html
Mexicoisthelargesthypoxiczoneinthe
WesternHemisphereandisalsooneof
thelargestintheworld(Downing1999;
Greenhalgh2003).Inmanyplaces,the
hypoxicwatersofdeadzonesaregradually
spreadingouttocoverlargerandlarger
areasofoceanfloor(Kempler2000).
Marinebio-invasionshavealsobecome
majorglobalenvironmentalandeconomicproblems.Atanyonetime,several
thousandspeciesareestimatedtobein
CaseStudy:MississippiDeadZone
2004
Recentreportsindicatethatthelargeregion
ofoxygen-depletedwater—adeadzone—
spreadsacrossnearly15080km2(5800
squaremiles)oftheGulfofMexicoinwhat
appearstobeanannualevent.NASAsatellites
monitorthehealthoftheoceansandspotthe
conditionsthatleadtoadeadzone.Thephoto(right)showssediment-chokedwaterfrom
theNeuseRiverflowingoutintotheGulfof
Mexiconearthecoast(NASA2004h).
Winter
Source:MississippiDeadZone,2004
http://www1.nasa.gov/vision/earth/environment/dead_zone.html
Summer
Credit:Unknown/UNEP/NASA
93
PhytoplanktonbloomoffDenmark,2004(showninlightbluecolor).Source:http://rapidfire.sci.gsfc.nasa.gov/gallery/?2004153-0601/Denmark.
A2004153.1145.1km.jpg
Theoceanisfilledwithlife.Oneofthemostimportantvarietiesfoundthereare
photosyntheticphytoplankton,tinyorganismsthatformthebaseoftheoceanicfood
web.Source:http://www1.nasa.gov/vision/earth/environment/dead_zone.html
CaseStudy:RedTides
CoccolithophorebloomoffBrittany,France,2004.Source:http://rapidfire.sci.
gsfc.nasa.gov/gallery/?2004167-0615/France.A2004167.1335.148.1km.jpg
theballasttanksoftheworld’sshipping
fleet,enroutetootherpartsoftheworld.
TheAtlanticboxjelly,believedtohave
beenreleasedinaship’sballastwater,has
wroughtecologicalhavocintheBlackSea.
ScientistsestimatethatinSanFrancisco
Bay,anewforeignspeciestakesholdevery
14weeks(UN2002).
Theproblemsarenotconfinedto
oceanwaters.Manycoastalecosystems
havebeendestroyed,andmanymore
degraded,oftenasaresultofhumanactivities.Mangroves,wetlands,seagrassbeds,
andcoralreefsarealldisappearingatan
alarmingrate.Anywherefrom5to80
percentoforiginalmangroveareainvariouscountrieshasbeenlost,particularly
inthelast50years(Burkeetal.2000).A
majorcontributortothislossistheconversionofmangrovestoricepaddiesand
shrimpfarms.Withcoastalregionssetto
doubletheirhumanpopulationsoverthe
next25years,coastalecosystemsarecom-
Throughouttheoceans,thereare
placeswherestrongcurrentsbring
nutrient-richdeepwaterstothe
surface.Theseupwellingnutrients
nourishtiny,free-floatingmicroscopicalgaeandotherphotosynthesizingplanktonicorganisms
collectivelyknownasphytoplankton.
Mostspeciesofphytoplanktonare
notharmful.Rather,theyformthe
baseofthemarinefoodweb.Occasionally,however,phytoplankton
growandreproduceveryquickly—they“bloom”—andaccumulate
intodense,visiblepatchesnearthe
water’ssurface.Somephytoplanktonbloomsarecalled“redtides,”
especiallywhenthespeciesinvolved
containredpigmentsandsocause
thewatertoturnpinkorredwhena
bloomisinprogress.Phytoplankton
blooms,however,havenothingtodo
withtides.
Whenphytoplanktondie,they
sinktotheoceanfloorwheretheir
remainsarebrokendownbydifferentkindsofbacteria.Someofthese
bacteriaemithydrogensulfidegasas
aby-productofdecayreactions.The
gascollectsontheoceanflooruntil
itbubblesuptowardthesurfaceand
combineswithoxygentoyieldwater
andsulfur.Thesulfurprecipitatesas
awhitesolid.
Hydrogensulfidegasbyitselfis
toxictofish.Butitsabilitytobind
withoxygenalsodepletesthatessentialgasfromthewatercolumn.If
enoughoxygenisremoved,deadly
low-oxygen(hypoxic)conditionsare
createdintheocean.
ingunderincreasingthreat(Harrisonand
Pearce2001).
Coralreefsareparticularlyvulnerable
toenvironmentalchangeanddamage
fromhumanactivities.Nearlytwothirds
ofalltheworld’scoralreefsaredeteriorating(Pomerance1999).Theyaredismemberedbysouvenir-seekingdivers,mined
forbuildingmaterials,anddamagedbythe
anchorsofcruiseships.Siltfromdredging,
deforestation,andurbansewagesmothers
andkillscoral,orfostersthegrowthofsuffocatingandsometimestoxicalgae(HarrisonandPearce2001).Coralreefsare
alsosubjecttoremotethreats.Dustcarried
aloftbystormsinAfrica(Figure3.21),and
thenspreadacrosstheAtlanticonprevailingwinds,mayhaveintroducedbacterial
infectionstoCaribbeanreefs(USGS2003).
Globalwarmingisalsoathreattocoral
reefs.Higherconcentrationsofcarbon
dioxideintheairmakesurfacewaters
moreacidicandreducecoralgrowthrates
Credit:Shoukyu/UNEP/Topfoto
94
(Kleypasetal.1999).Theriseofocean
temperaturesbyhalfadegreeormorein
recentdecadeshasalreadyplacedmany
reefsatthetopendofthetemperature
rangestheycantoleratewithoutundergoing“bleaching”(HarrisonandPearce
2001).Ascoralsreachthelimitsoftheir
heattolerance,theyexpelsymbioticalgae
fromtheirbodiesandbecome“bleached.”
Epidemiccoralbleachinginthe1990s,
whichpeakedwiththeElNiño-induced
warmingof1998,isbelievedtohavekilled
morecoralinthelastfewyearsofthe20th
centurythanfromallhumancausestodate
(Pearce1999).Continuedwarmingcould
causesealevelstoriseataratethatcoral
reefscannotmatch.
Coastallandshavebeengreatlyimpactedbyhumanactivities.Fifty-onepercent
oftheworld’scoastlinesareunder“moderate”or“high”threatfromdevelopment
activities(Bryantetal.1995).Nineteenper
centofalllandswithin100km(62miles)
ofthecoast(excludingAntarcticaand
waterbodies)areclassifiedas“altered,”
havingbeenturnedintoagriculturalor
urbanareas;10percentare“semi-altered,”
involvingamosaicofnaturalandaltered
vegetation;and71percentfallwithin
the“leastmodified”category.Alargeper
centageofthecoastallandsinthisleast
27 Mar 2004
modifiedcategory,however,includesmany
foundinuninhabitedareasinnorthern
latitudes(Burkeetal.2000).
Thedestructionofcoastalecosystems
andthedeteriorationinthequalityof
oceanwaters,togetherwithoverexploitationofresources,areseriouslyimpacting
thesurvivaloftheecosystemsandthe
peoplethatdependonthem(SIDAn.d.).
9 Jun 2004
Figure3.21:WhileSaharandustprovidescoral
reefswithessentialnutrientslikeironandcopper,
Saharandustalsointroducesbacterialinfections
tocoralreefs.TheimagetotheleftisaSaharan
duststormspreadingoutovertheMediterraneanin
2004.Theimagetotherightisoflargedustplumes
offNamibiain2004.Source:http://rapidfire.sci.gsfc.nasa.
gov/gallery/?2004125-0504/Libya.A2004125.0940.1km.jpg,
http://rapidfire.sci.gsfc.nasa.gov/gallery/?2004161-0609/Namibia.A2004161.0930.1km.jpg
Credit:DenjiroSato/UNEP/Topfoto
95
CaseStudy:Africa’sKipiniWildlifeand
BotanicalConservancy
ChristianLambrechts
ThecoastalregionofKenyaisfamousforits
naturalbeauty,richculture,diversecommunities,andasarecreationalresource.Thishas
ensuredeconomicbenefitsforKenyafrom
mainlynon-consumptiveutilizationofitsnaturalresourcesthroughtourism.Yetthisdevelopmenthasnottakenplacewithoutconsiderable
environmentalcost.Excessiveconstruction
alongthecoastline,uncontrolledaccessto
marineenvironments,factoryfishingoperations,andpoorplanninghaveledtoadecline
inthequantityandqualityofbothlandand
marineresources.Thishasbeenreflectedin
lossofbiodiversity,dwindlingfish
stocks,anddecliningemployment
andtourismfigures,althoughthe
latterarealsoattributabletorecent
securityconcerns.
TheKipiniWildlifeandBotanicalConservancyislocatedalong
thecoastofeasternKenya.Itlies
withintheLamuandTanaRiver
districts,butisconnectedecologicallytotheIjaraDistrict.It
isawell-preservedareawithhigh
biodiversity,althoughfewconservationprojectshaveeverbeenimplementedandcurrentprotectionis
inadequatewithwildlifereserves
onlyonpaper.Withincreasing
Credits:ChristianLambrechts/UNEP/UNEP-GRIDNairobi
96
Credit:ChristianLambrechts/UNEP/UNEP-GRIDNairobi
Location of the Conservancy
populationpressuresonthenaturalresources
thereisaneedforpromptaction.
TheKipiniConservancyinitiallyfocuseson
whatwasonceknownasNairobiRanch,anarea
approximately16000hectares(40000acres)
insizethatissituatedbetweenthehistorical
townsofKipini,WituandLamu.TheSwaleh
Nguru(Sherman)familysecuredtheland
underafreeholdarrangementandhasmaintaineditevenatalossunderlivestockoperations.Developmentoftheranchisnecessary,as
Kenyacanillaffordidleland.Butdevelopment
isbeingundertakenwithconsiderablecareto
ensureadequateenvironmentalconservation.
Bycreatinganeasementonthisfreeholdland,
theSwalehNgurufamilyhasputitintrustfor
futuregenerationsofKenyansaswellasvisitors
tothecountry.Theconservancywillneedtobe
vigorouslymanagedandwillinvolveatransitionfromacattle-basedranchingsystemtoa
morenaturallandscapepopulatedbynative
species.Incomegenerationwillbebasedon
heritagevalueanddonorsupportintheshort
term,withincreasingrelianceoneco-tourism.
Inthefuture,theKipiniConservancyisexpectedtobeexpandedtoincludetherangeof
criticallyendangeredspecies.Inarecentstudy
fundedbytheFinnishEmbassy,Ader’sduiker,
anextremelyraremammaloncethoughtto
bevirtuallyextinctinKenya,wasfoundinthe
areaneartheConservancy.Expansionofthe
Conservancywillalsohelptopreservehighly
diversehabitatcorridorsbetweenthecoastand
theinteriorandwillinvolvesurroundingcommunitiesinconservationefforts.
Thecoastalmarineecosystemadjacentto
theConservancyispartoftheGlobal200ecoregion.Itsupportsagreatdiversityofanimal
andplantlifeandisknownasaturtlenesting
area.Severalspeciesofwhalesanddolphinsare
foundinthewatersoffshore,aswellasthegloballythreateneddugong(Dugongdugon).The
partoftheConservancythatborderstheTana
Riverdeltaisastop-overandwinteringgrounds
formanymigratorybirdpopulations.Thearea
alsoprovideshabitatforthreatenedshorebirds
andseabirds(UNEP/GRID–Nairobi).
Credit:Unknown/UNEP/Topfoto
97
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ULF OF ONSECA ,
98
ONDURAS
Honduras is second only to Ecuador in the production
and export of cultured shrimp from Latin America. Vast
areas of the delta have been converted into farms for
the cultivation of shrimp.
The rapid growth of shrimp aquaculture in Honduras has caused both environmental and social
ShrimpaquacultureinHondurasbeganintheearly1970s
andcontinuedinthe1980s
inthehandsofbothnational
andinternationalenterprises.
Credit:Unknown/UNEP/Topfoto
problems. Shrimp farmers are depriving fishers, farmers and others of access
to mangroves, estuaries and seasonal lagoons; destroying mangrove ecosystems, altering the hydrology of the region, destroying the habitats of other
flora and fauna and precipitating declines in biodiversity; contributing to
degraded water quality; and exacerbating the decline in Gulf fisheries
through the indiscriminate capture of other species caught with the shrimp
post larvae that are used to stock ponds.
These two images provide a visual comparison of the increase in coverage
by shrimp farms in the Gulf of Fonseca over time. It is evident from the images that between 1987 and 1999, a period of about 12 years, the total area
under shrimp farming has increased tremendously.
99
C
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G
E
ULF OF
100
UAYAQUIL , CUADOR
Guayaquil is Ecuador’s largest city and primary sea
port. It is located on the Guayas River, which empties
into the huge Gulf of Guayaquil along the country’s
southern coastline. Throughout the Gulf, mangroves
have been steadily converted to shrimp aquaculture
ponds for producing farmed shrimp. In a 15-year pe-
riod, coastal area developed for shrimp aquaculture grew by approximately
30 per cent, from 90 000 hectares (222 395 acres) in 1984 to 118 000 hectares
(291 584 acres) in 2000 (CLIRSEN 2000). Roughly 70 per cent of Ecuador’s
shrimp farming activities are located in the Gulf of Guayaquil.
In this pair of satellite images, the loss of mangroves and growth of the
aquaculture industry can be seen along the coast and in the altered dendritic
patterns (branching like a tree) of coastal waterways, especially those on the
large island of Puna. Mangroves provide fish breeding grounds and wildlife
habitat, act as natural barriers against storm surge, and filter groundwater.
Converting mangroves to aquaculture ponds has wide-reaching environmental implications.
101
HuangHeDelta
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H D
C
UANG
102
E
ELTA ,
HINA
The Huang He (Yellow River) is the muddiest river on
Earth and is China’s second longest river, running 5 475
km (3 395 miles) from eastern Tibet to the Bohai Sea.
The Huang He’s yellow color is caused by its tremendous load of sediment, composed primarily of mica,
quartz, and feldspar particles. The sediment enters the
water as the river carves its way through the highly erodable loess plateau in
north-central China. (Loessial soil is called huang tu, or “yellow earth,”
in Chinese.)
Centuries of sediment deposition and dike building along the river’s
course has caused it to flow above the surrounding farmland in some places,
making flooding a critically dangerous problem. Where the Huang He flows
into the ocean, sediments are continuously deposited in the river delta,
where they gradually build up over time. Between 1979 and 2000—as these
satellite images show—the delta of the Huang He expanded dramatically.
Several hundred square kilometres of newly formed land were added to
China’s coast during this period.
103
Dike
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N
JSSELMEER,
104
ETHERLANDS
The Zuiderzee is a large body of water along Holland’s
northeastern coast. Between 1927 and 1932, a 30 km
(19 miles) dam, known as the Afsluitdijk, was built
across the Zuiderzee, separating it into the outer
Waddenzee, which is open to the North Sea, and the
inner IJsselmeer (Lake IJssel) where areas of reclaimed
land—called polders—are used for agriculture and as villages. Dikes built
since that time created additional polders that were drained using pumps
and, at one time, wind mills.
These images, from 1964, 1973, and 2004, show the transformation of polders into useable farming land. The 1973 image shows a partially completed
dike that, when completed allowed for the creation of the southernmost
polder visible in the 1973 image. At that time, draining of the land had been
completed and soil cultivation began. By 2004, this area of reclaimed land
was covered with farms. The area of lighter blue water visible in the left of
the 1973 and 2004 images is the Markermeer—a polder that was created
but not drained. It forms a freshwater reservoir that acts as a buffer
against floodwaters.
105
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B J
SAHAYA
106
AY , APAN
Land reclamation began in Japan’s Isahaya Bay in
1989 to separate approximately 3 000 hectares (7 413
acres) of tidal flats from the Ariake Sea and turn what
was Japan’s largest area of tidal lands into farmland.
As these three satellites images show, the project has
steadily progressed. In the 2001 image, the straight line
of a 7-km (4 mile) sea wall is visible separating areas
of light- and dark-colored water. Behind the sea wall, tidal flats can be seen
drying as water is slowly drained away. In the 2003 image, that area has been
fully reclaimed from the sea.
The Isahaya Bay Reclamation project has been fraught with controversy.
Environmental groups have criticized the project for its destruction of wetland habitat. The Isahaya Bay area is known for its production of nori
(seaweed), and local farmers have complained that the reclamation project
has negatively impacted the quality and abundance of the nori growing in
the bay. The Isahaya project prompted the formation of the Japan Wetlands
Action Network, a group of grassroots and national conservation organizations who are protesting the project and recommending that the sea wall
gates be opened to restore ecological balance.
107
C
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D
C
NIFE
108
IVER
ELTA ,
ANADA
Snow geese migrate each spring to the shores of Hudson Bay, Canada, to breed and to raise their chicks. Over
the past few decades, the numbers of geese descending upon the Bay’s Knife River delta area have increased
substantially. Their impact on coastal vegetation can
clearly be seen in this pair of satellite images.
In the image on the right, notice how the vegetation (green) has receded
from the shoreline north of the delta. Snow geese have overgrazed this area
and turned the shoreline into an enormous mudflat. Having denuded the
shoreline of vegetation, the geese have also moved inland in search of food
on the tundra, where overgrazed soil quickly becomes barren and develops
a crust of salt due to evaporation. The salty layer prevents the regrowth of
plants, and ultimately leads to erosion. Some researchers have suggested
lifting restrictions on the hunting of snow geese in an attempt to reduce their
numbers and control the overgrazing problem. Others believe such measures
are “too little, too late.”
109
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P
C
HNOM ENH ,
110
AMBODIA
Phnom Penh (pronounced p-NOM PEN) is the capital
city of Cambodia. It is just west of the four-way river
intersection, which is called the Chattomukh (“Four
Faces”). From the northwest and northeast, respectively, flow the Tonle Sap and Mekong Rivers. These waters
merge and split into the Basak River and the Mekong,
which flow southeast to the South China Sea. The Mekong River is the 12th
longest in the world, flowing from western China to the Mekong Delta in
southern Vietnam. Every autumn, monsoon rains are too great for the Mekong to carry, and it floods a large area of Cambodia. This flood even reverses
the flow of the Tonle Sap River, northward to the Tonle Sap (“Great Lake”)
which can expand to ten times its normal size.
This pair of images show the extent of flooding associated with the two
rivers. The 2000 image was taken during a period of flooding while the 2001
image was taken after the flood waters had receded. Visible also in the images, especially in the south-central area of the 2001 image, are extensive
ditches and canals that are used in irrigation.
111
C
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I
B
UNDARBAN , NDIA /
112
ANGLADESH
Sundarban, the largest mangrove forest of the world, is
situated in the southwestern part of Bangladesh and in
the West Bengal of India. Guarded by the Bay of Bengal,
Sunderban is an excellent example of the coexistence
of human and terrestrial plant and animal life. Despite
high population pressure and environmental hazards such as siltation, cyclone flooding and sea level rise, the aerial extent of the mangrove forest has
not changed significantly in the last 25 years. In fact, with improved management, the tiger population has increased from a mere 350 in 1993 to 500-700
in 2000 and ecotourism is progressing well. However, while sufficient data is
not available, several reports suggest that forest degradation has been occur-
ring in many parts of Sundarban. The Sundarban’s mangrove forests are also
becoming more vulnerable due to the significant rise of shrimp farming in
the region. The increase of shrimp farming has negatively affected agriculture
and also contributed to the loss of mangrove forests during the past
two decades.
113
Shrimpfarm
Credit:H.GydeLund/UNEP
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B
T
HON
114
URI ,
HAILAND
As the city of Bangkok, Thailand, has grown, the need
to provide food and an additional economic base for
its burgeoning population has been a primary concern.
Parts of the Thai coastline, including those near Bangkok, offer conditions favorable to aquaculture,
Mangrovetrees
Credit:H.GydeLund/UNEP
especially shrimp aquaculture. Over time, as these satellite images from 1978
and 2002 reveal, the mangroves that once lined the coast near Bangkok, as
well as the rice paddies that lay further inland, have been replaced by aquaculture ponds (blue patches inland) and urban structures (light purple). The
promotion and development of aquaculture has led to the current situation,
where farmed shrimp and fish production now exceeds that of shrimp and
fish capture by traditional methods. The development of this coastal industry
has raised environmental concerns, as extensive areas of mangroves have
been destroyed to make way for aquaculture ponds. The challenge of balancing the needs of people living in coastal areas versus the welfare of the
coastal areas themselves is ongoing, and repeated along many coastlines
worldwide.
115
116
Credit:Laurent/UNEP/Topfoto
117
3.3 Water
W
aterisfundamentaltoalmostalllivingthingsontheEarth.
Humanhealth—andsurvival—dependsonacleanand
reliablesupplyoffreshdrinkingwater,aswellaswater
forcropirrigationandsanitation(UNESCO2000).Freshwateris
waterthathasaverylowsaltcontent—usuallylessthanone
percent.Onlyabout2.5percentofallwaterontheplanetis
fresh.Ofthatamount,onlyabout0.5percentissurfacewater
(foundinlakes,rivers,wetlands)oraccessiblegroundwater.
Rainfallisalsoasourceoffreshwater.Butrainfallisunpredictableandamountsvarydramaticallyfromplacetoplaceand
seasontoseasonaroundtheworld(UNFPA2001).
Duringthepastcentury,worldpopulationhastripled.
Overroughlythesameperiodoftime(1900to1995)water
useworldwidehasincreasedsix-fold.Expertspredictthatby
2025,globalwaterneedswillincreaseevenmore,with40per
centmorewaterneededforcitiesand20percentmorewater
forgrowingcrops(Paden2000).Yetwhileneedsincrease,the
amountofavailablefreshwaterisdwindlingworldwide.
Waterwithdrawalsfrom
riversandunderground
reserveshavegrown
by2.5to3percent
annuallysince
1940,significantlyahead
ofpopulation
growth.So
muchwater
iswithdrawnfrom
severalof
theworld’s
major
rivers,
including
theColoradoRiver
intheUnited
States,theNile
RiverinEgypt,
andtheYellow
RiverinChina,that
thereislittletonowaterleftbythetimethese
riversmeetthesea(Postelet
al.1996).Demandsongroundwater
areequallygreat;watertablesarefallingoneverycontinent.
Overthenexttwodecades,itisestimatedthattheaverage
supplyofwaterperpersonwilldropbyone-third.Annually,lack
ofcleandrinkingwatercanbelinkedtoroughly250millioncasesofwater-relateddiseaseandbetween5and10milliondeaths
worldwide.Thus,watershortagesindirectlycondemnmillions
ofpeopletoanavoidableprematuredeatheachyear.
Watershortagesarealsoimpactingglobalgrainmarkets,as
aridcountriesthatrelyonirrigationforcropproductionswitch
fromgrowinggraintoimportingit(HarrisonandPearce2001).
Irrigationaccountsfor70percentofdirectwaterconsumption
worldwide.Ithasbeenestimatedthatpracticessuchasdripirrigationandinexpensivemoisturemonitorscouldcutagricultural
waterusebyasmuchas40percent(Wall2001).
118
Theexploitationoftheworld’swaterresourceshasoccurredatnosmall
costtotheenvironment.Worldwide,allmajorrivershavewaterworks
thatchangeflowregimestosomeextentandthereforeimpactriparian
ecosystems.Manyendemicriparianspeciesaredisappearing(Ramsar
ConventionBureau1998),andtwentypercentofallfreshwaterfish
arecurrentlyendangered.Fewaquaticecosystemshavebeenas
severelyimpactedaswetlands,however.Duringthe20thcentury,halfoftheEarth’swetlandecosystems—suchasmarshes,
fens,swamps,andestuaries—disappeared(UNESCO2003).
Approximately40000hectares(98842acres)ofwetlandsare
destroyedeachyearastheresultofhumanactivities(Center
forEnvironmentalResourceManagementn.d.).Drainagefor
agriculturalproductionistheprincipalcauseofwetlandloss.
Atthesametimethatglobalwatersuppliesaredeclining,
soisthequalityofthewaterthatremains.Waterpollutionis
thepresenceofharmfulandobjectionablematerial—such
assewage,industrialwastesandchemicals,andrun-offfrom
landdevelopmentoragriculture—insufficientconcentrations
astomakewaterunfitforuse(EEA2004).Waterpollutionisa
seriousthreattotheworld’swatersupply.
Itisalsoagrowingthreattothe
oceansthatcovermorethan
70percentoftheplanet.
Peoplehavelongviewed
theseimmensebodies
ofwateraslimitless
dumpinggrounds
forwastes.Over
time,however,
rawsewage,
garbage,industrialwastes,
andoilspills
havebegun
tooverwhelm
thediluting
capabilities
oftheoceans.
Mostcoastal
watersarenow
polluted,often
severely(Revenga
andMock2000,
Revengaet
al.2000).
The21stCentury
bringswithitaglobalwater
crisis.Unlesscorrectiveand
conservationmeasuresaretaken,it
isestimatedthatby2030globaldemands
forfreshwaterwillexceedthesupply(NSWEPA2003,UNESCO
2000).Seriouswaterandfoodsecurityproblemsalreadyexist
insomedevelopingcountriesandregions,andthesedemand
urgentattention(FAO2003).
Growingpopulationinurbanareasisexertinggreatpressureonwaterresources.Eveniftheworldmaintainedthe
paceofthe1990sinwater-supplydevelopment,thiswould
notbeenoughtoensurethateveryonehadaccesstosafe
drinkingwaterbytheyear2025.Theimpactsofclimate
change—includingchangesintemperature,precipitation
andsealevels—areexpectedtohavevaryingconsequences
fortheavailabilityoffreshwateraroundtheworld.Current
indicationsarethatifclimatechangeoccursgradually,theimpactsby2025maybeminor,withsomecountriesexperiencing
positiveimpactswhilemostexperiencenegativeones.Climate
changeimpactsareprojectedtobecomeincreasinglystrongduringthedecadesfollowing2025.
119
Credit:MarioHernanValencia/UNEP/Topfoto
120
W
ATER
KBG T
,
The Caspian Sea, seen in this 2004 image, is the largest
inland body of water in the world, often categorized
as a large salt lake. It is salty because rivers (especially
the Volga) flow into it, but none flow out. Water leaves
URKMENISTAN
121
121
through evaporation, and the dissolved salts remain. Changes in water
levels are common in the sea, resulting both from changing climatic factors and water diversion by humans. The 2004 image highlights the area
of change—the Kara-Bogaz-Gol (KBG). KBG is a large, shallow lagoon of
the Caspian Sea, normally about 18 200 km2 (7 000 square miles) and a
122
few metres deep. The Caspian’s changing water level has been a concern
since the 1970s. The KBG’s water flows in from the Caspian Sea, and its
fluctuations have affected the KBG dramatically.
In the 1980s, a dam blocked the KBG’s inflow, resulting in the formation of a “salt bowl” that caused widespread problems of blowing salt,
In1980,inresponsetotherapidlydroppingsea
level,adamwasconstructedtopreventwaterfrom
flowingintotheshallowandrestrictedKara-BogazGolbasin,resultinginthedryingupofthebay.
Thedamwaspartiallyopenedafewyearslater,
andcompletelyopenedin1992whenCaspianwaterlevelsstartedtorisequickly.Credit:NASAJohnson
SpaceCenter
reportedly poisoning soil, and causing health problems for people
living hundreds of kilometers downwind to the east. While the dam
was in place, not only did the KBG’s water level rapidly drop by 2 m (7
ft) or more, but the lagoon’s shallow bottom also rose 0.5 m (2 ft), due
to the accumulation of salts.
The dam was partially opened in 1985, and completely opened in
1992 when Caspian Sea water levels started to rise quickly. Today, sea
levels are more than 2.6 m (9 ft) higher than the 1978 levels and water
flows freely into the salty waters of the Kara-Bogaz-Gol.
123
W
ATER
A S K
RAL EA ,
124
AZAKHSTAN
The name “ Aral Sea “ comes from the word “aral” meaning island. The sea’s name reflects the fact that it is a
vast basin that lies as an island among waterless deserts. The Aral Sea was once the world’s fourth-largest
inland sea. Its problems began in the 1960s and 1970s
with the diversion of the main rivers that feed it to provide for cotton cultivation in arid Soviet Central Asia. The surface of the Aral Sea once measured
66 100 km2 (25 521 square miles). By 1987, about 60 per cent of the Aral
Sea’s volume had been lost, its depth had declined by 14 m (45 feet), and its
salt concentration had doubled, killing the commercial fishing trade. Wind
storms became toxic, carrying fine grains of clay and salts deposited on ex-
posed sea floor. Life expectancies in the districts near the sea are significantly
lower than in surrounding areas.
The sea is now a quarter of the size it was 50 years ago and has broken
into two parts, the North Aral Sea and the South Aral Sea. Re-engineering
along the Syr Darya River delta in the north will retain water in the North Aral
Sea, thereby drying the South Aral Sea completely, perhaps within 15 years.
125
Thepower-generatingstationattheAtatürkDamalreadyprovides8.9billionkilowatthoursofelectricity—roughly22per
centoftheelectricitythecountryisexpectedtoneedby2010.
Credit:Unknown/UNEP/USDA-FAS
W
ATER
A
D
TATÜRK
126
AM ,
TURKEY
Built in 1990, the Atatürk Dam on the Euphrates River
in southeastern Turkey is the centrepiece of the Southeastern Anatolia Project. The Atatürk Dam is the largest
in a series of 22 dams and 19 hydroelectric stations
built on the Euphrates and Tigris Rivers in order to provide irrigation water and electricity to this arid region
MainHarrancanal
Credit:Unknown/UNEP/USDA-FAS
of the country. When the project’s entire system of reservoirs, power generation stations, and irrigation channels is operational (projected to occur in
2010), the irrigation of approximately 1.7 million hectares (4.2 million acres)
of land will be possible..
In these two Landsat images, acquired in 1976 and 1999, respectively, the
transformation of the region around the dam is strikingly apparent. The dam’s
reservoir reached capacity in 1992 and has supplied sufficient water for irrigation to turn a once-arid landscape into a green one. This is especially obvious
in the lower right-hand corner of the 1999 image, where irrigated fields completely surround the town of Harran. The development of the Harran region
could not have occurred without the Atatürk Dam project, especially since
the town is many kilometres from the river.
127
Credit:Combs/UNEP/AfricaFocus
Vegetablecropsofonionsandsweetpotatoescangrowin
fieldsmaintainedbyirrigation.
W
ATER
C
G
HALLAWA
128
ORGE
DAM,NIGERIA
The Challawa Gorge Dam, completed in 1993 on the
Challawa River, is the second-largest of the 23 dams
along rivers in Nigeria’s Hadejia-Jama’are River Basin.
Though the dam has improved the water supply for
irrigation, heavy rains cause the river to break its banks
Credit:Combs/UNEP/AfricaFocus
SoilturnedwithhandtoolinnorthernNigeria.
upstream from the dam; farmers are driven out as the rising water floods their
farms and adjoining lands. Areas downstream from the dam, on the other
hand, do not receive enough water to maintain the wetlands that border the
river. Under these conditions, the soil dries out and overgrazing occurs, which
in turn leads to wind erosion of the topsoil.
This satellite image pair gives a comparison of the area before and after
construction of the dam. The 1999 image shows the degree to which flooding upstream from the dam impacts the landscape, and how the lack of water
downstream negatively affects riverine wetlands and cropland. The colour of
the water in the flooded area is also indicative of high-sediment content.
129
W
ATER
D S J
EAD EA , ORDAN
130
For decades, heavy demands have been placed on the
land-locked Dead Sea to meet the needs of growing
populations in the countries that border it. Both Israel
and Jordan draw water from rivers that flow into the
Dead Sea, reducing the amount of water that would
naturally replenish it. The amount of area devoted to evaporation ponds for
producing salt has greatly expanded over the past three decades. The creation of salt works tends to accelerate evaporation, further contributing to
the reduction in water level. Currently, it is estimated that the water level of
the Dead Sea is dropping at a rate of about one metre (3 feet) per year.
These two images, from 1973 and 2002, reveal dramatic changes in the
Dead Sea over a period of about 30 years. Declining water levels, coupled
with impoundments and land reclamation projects, have greatly increased
the amount of exposed arid land along the coastline. The near-complete closing off of the southern part of the Sea by dry land (2002 image) reveals the
severity of water level decline.
131
Aerialviewofurbandevelopementinthe
Everglades.
Credit:Unknown/UNEP/SFWMD
WATER
EVERGLADES,UNITEDSTATES
132
These two Landsat images of southern Florida in the
United States reveal some of the changes that have occurred in this region over the past 30 years. One of
the most obvious is the growth of the Fort LauderdaleMiami urban area. Urban expansion has led to the con-
TheFloridapanther.
Credit:Unknown/UNEP/SFWMD
version of what were once farmlands to cityscapes. The city of Miami has also
expanded greatly to the southwest. The advance of urban areas westward
across the peninsula threatens the continued existence of the vast wetlands
area known as the Everglades. The Everglades ecosystem naturally filters
groundwater and helps to recharge the Biscayne Aquifer. It is also home to
a remarkable collection of plants and animals for which southern Florida is
famous. As urban areas encroach upon the Everglades, water resources and
wildlife habitat are placed at serious risk. Protecting the Everglades to maintain its essential water filtering capacity and remarkable biodiversity is part
of the mission of the Federal “Smart Growth” Task Force, which is working to
better manage urban sprawl and its negative consequences.
133
FormerDanuberiverbottomexposedaswaterisredirectedintothediversioncanal.Credit:PeterBardo-Déak/UNEP/WWF-DCP
W
ATER
G
S
ABCIKOVA , LOVAKIA
134
The Gabcikova-Nagymoros hydraulic project on the
Danube River was started in order to generate electric
power, create an inland waterway, help manage water
supplies, and aid in the region’s economic development. The river was to be dammed and its water diverted into a canal. Four decades after it was initiated the
AdamontheDanubeRiver
Credit:PeterBardo-Déak/UNEP/WWF-DCP
Cunovo Dam began operation in Slovakia in October 1992. The dam diverted
80 to 90 per cent of Danube River water down a diversion canal to support a
hydroelectric power station.
This pair of images from 1973 and 2000 reveal the striking changes the
massive re-channeling of river water has brought to the region. The dam
altered the hydraulic regime of the Danube River valley from a natural water-
way to a controlled patchwork of channels and islands. The diversion of water
by the dam brought an end to the natural, beneficial flooding that added
moisture and nutrients to the soil. It also reduced the ability of wetlands and
marshes to filter surface water and trap sediments. Consequently, water quality and soil nutrients levels in the region have declined. Generation of electricity has come with significant environmental cost.
135
W
ATER
L
H
ESOTHO
136
IGHLANDS
WATERPROJECT
The Lesotho Highlands Water Project (LHWP) is one of
the largest infrastructure projects ever undertaken on
the African continent. The project is designed to divert
water from Lesotho’s Maloti Mountains to South Africa’s
urban and industrial Gauteng Province. While South
Africa is set to benefit from an increased supply of
much-needed water, Lesotho would gain through the generation of hydroelectric power and profits from the sale of water. An 82-km (51-mile) water
transfer-and-delivery system is already in place for delivering water to South
Africa. On completion of the full project, a total of four dams will be placed in
key locations. However, many questions remain unanswered about the social
and environmental impacts the completed dams will have. The first dam in
the multi-dam scheme, called Katse, located on the Orange River, closed its
gates in 1995, creating an enormous reservoir along with serious social and
environmental concerns.
These two images provide a comparison of the area before and after
completion of the Katse dam. The effects and extent of the Katse Dam can
clearly be seen in the 2001 image.
137
W
ATER
L B
AKE
138
ALKHASH ,
KAZAKHSTAN
Located in Kazakhstan, Central Asia, Lake Balkhash is
replenished from the Ili River catchment area, most of
which is located in northwestern China. The lake is a
very important resource for the surrounding population. Water from the lake and its tributary rivers is used
for irrigation and both municipal and industrial purposes, including supplying the water needs of the Balkhash Copper Melting Plant. Lake fish are also
an important food source. However, artificially low water prices have encouraged excessive use and waste of lake water. The United Nations has warned
that Lake Balkhash, which is the second largest lake in Central Asia after the
Aral Sea, could dry up if current trends are not reversed.
These two satellite images reveal an alarming drop in the lake’s water
levels in just over twenty years. Smaller, neighboring lakes, to the southeast
of Balkhash, have become detached from the main water body; they have
dramatically decreased in size and appear to be drying up.
139
WATER
140
LAKECHAD,AFRICA
Lake Chad, located at the junction of Nigeria, Niger,
Chad, and Cameroon was once the sixth-largest lake in
the world. Persistent droughts have shrunk it to about
a tenth of its former size. The lake has a large drainage
basin—1.5 million km2 (0.6 million square miles)—but
almost no water flows in from the dry north. Ninety
per cent of lake’s water flows in from the Chari River. The lakebed is flat and
shallow; even before the drought, the lake was no more than 5-8 m (16-26
ft) deep. Considered a deep wetland, Lake Chad was once the second largest
wetland in Africa, highly productive, and supporting a diversity of wildlife.
The lake is very responsive to changes in rainfall. When rains fail, the lake
drops rapidly because annual inflow is 20-85 per cent of the lake’s volume.
Human diversion from the lake and from the Chari River may be significant at
times of low flow, but rainfall is still the determining factor in lake level.
This image set displays a continued decline in lake surface area from
22 902 km2 (8 843 square miles) in 1963 to a meager 304 km2 (117 square
miles) in 2001.
141
W
ATER
L C
AKE
142
142
HAPALA ,
MEXICO
Mexico’s Lake Chapala, lying in the heart of an extremely arid region, is the country’s largest natural lake.
The lake is one of the most important wetlands in the
region and home to more than 70 endemic species.
Since the 1950s, Lake Chapala has undergone many
changes as a result of water abstraction for agricultural
use both inside and outside the region and for a rapidly growing population.
The level of the lake has declined, and there have been noticeable decreases
in surrounding wetland areas as well as changes in the hydrological system
connecting various springs.
Some of these changes are visible in this pair of satellite images, including
alterations in the contours of the shoreline, obvious extensions of land near
various townships around the lake, and the appearance of remarkably large
areas of reclaimed land at the lake’s eastern end. Like all arid areas, the land
around Lake Chapala is prone to salinization. If the lake continues to shrink,
researchers predict both a decrease in water availability and an increase in
the salt content of the region’s soil.
143
W
ATER
L H
AKE
144
I
AMOUN , RAN
Iran’s Lake Hamoun is fed primarily by water catchments in neighboring Afghanistan. In 1976, when rivers
in Afghanistan were flowing regularly, the amount of
water in the lake was relatively high. Between 1999 and
2001, however, the lake all but dried up and disappeared, as can be seen in
the 2001 satellite image above.
The “dry phase” of Lake Hamoun is a striking example of how competition
for scarce water resources can transform a landscape. When droughts occur in Afghanistan, or the water in watersheds that support Lake Hamoun is
drawn down by other natural or human-induced reasons, the end result is a
dry lakebed in Iran. In addition, when the lake is dry, seasonal winds blow fine
sands off the exposed lakebed. The sand is swirled into huge dunes that may
cover a hundred or more fishing villages along the former lakeshore. Wildlife
around the lake is negatively impacted and fisheries are brought to a halt.
Changes in water policies and substantial rains in the region saw a return of
much of the water in Lake Hamoun by 2003.
145
FlamingosonLakeNakuruCredit:GrayTappan/UNEP
W
ATER
L N
K
AKE
146
AKURU ,
ENYA
Lake Nakuru is located in the Eastern Rift Valley in
southwest Kenya. Lake Nakuru National Park is the
second most visited protected area in Kenya. It hosts
the world’s largest concentration of flamingos, as well
as many of the animal species that make Kenya a highly
valued tourism destination, including lions, leopards,
VegetationaroundLakeNakuru
Credit:GrayTappan/UNEP
rhinoceros, and water buffalo. In its total area of 188 km2 (73 square miles),
there are over 450 bird species and 56 mammal species. Recognized as a
wetland of international importance, Lake Nakuru was declared a Ramsar Site
in 1990.
The threat of land cover degradation in the catchments of the lake is likely
to increase flow fluctuation and decrease water quality. These images show
the land cover degradation in the lake’s catchment between 1973 and 2000.
In 2001, the Government of Kenya announced its intention to excise 353
2
km (136 square miles) of forest in the Eastern Mau Forest Reserve (area with
white boundary in the 2000 image). As a result, most of the forest cover in the
upper catchment of the main rivers that feed Lake Nakuru will disappear.
147
W
ATER
L V
AKE
148
ICTORIA ,
UGANDA
Shared by Kenya, Tanzania, and Uganda, Lake Victoria
is the second largest freshwater lake in the world. The
infestation of Lake Victoria by water hyacinth in the
1990s disrupted transportation and fishing, clogged
water intake pipes for municipal water, and created
habitat for disease-causing mosquitoes and other
insects. This led to the initiation of the Lake Victoria Environmental Management Project in 1994. The focus of the Project was to combat hyacinth infestations on the lake, particularly the region bordered by Uganda, which was one
of the most severely affected areas.
The 1995 image shows several water-hyacinth-choked bays: Murchison
Bay near Gaba; large parts of Gobero and Wazimenya Bays; an area outside
Buka Bay; and near Kibanga Port (yellow arrows).
Initially, water hyacinth was controlled by hand, with the plants being
manually removed from the lake. But re-growth quickly occurred. A more
recent control measure has been the careful introduction of natural insect
predators of water hyacinth. As the 2001 image shows, this approach seems
to have been successful, as the floating weeds have disappeared from all the
locations noted above.
149
1973
W
ATER
M
M
ESOPOTAMIA
150
150
I
ARSHLANDS , RAQ
Located at the confluence of the Tigris and Euphrates
rivers, the Mesopotamian marshlands are one of the
world’s great wetlands covering an estimated original
area of 15 000 - 20 000 km2 (5 792 - 7 722 square miles)
The marshlands are an important center of biodiversity,
play a vital role in the intercontinental migration of
birds, and have long supported unique human com-
munities. Upstream damming as well as drainage activities in the marshlands
themselves have significantly reduced the quantity of water entering the
marshes. Together these factors have led to the collapse of the ecosystem.
Restoration of the marshlands, mainly through reflooding by breaching of
dykes and drainage canals has begun. As a result of these activities, vegetation and wildlife have returned to some parts of the marshes.
This set of images provides a synoptic illustration of the changes. While
the 1973 image (inset left) shows the extent of the original marshlands, the
2000 image (inset right) reveals the area after being drained, with most of the
wetlands having disappeared. On the other hand, the 2004 image illustrates
recovery in progress with major portions in the central and western sections
having been restored to some extent.
151
W
ATER
T
G
HREE
152
ORGES
DAM,CHINA
The Three Gorges Dam on the Chang Jiang (Yangtze)
River in China is one of the largest single construction
projects ever attempted on the planet. The dam was
constructed to supply approximately one-ninth of
China’s electricity—as much power as could be gener-
ated by at least fifteen nuclear power plants. It is a relatively environmentally
clean option compared to coal burning or nuclear power plants. It is also
hoped that the dam will help control flooding on a river where seasonal
floods during the past century has caused death of over one million people.
However, the Three Gorges Dam project has also had negative environmental
and social impacts as a result of the massive construction efforts and the sub-
mergence of land along the river above the dam. The former village of Zigui
(top center of image) has already been submerged.
The 1987 image shows the nature of the river and surrounding landscape
before work on the dam was begun. In the May 2004 image, the enormous
Three Gorges Dam is clearly visible, as is the reservoir of impounded river
water that has been created behind it.
153
154
Credit:IIguchi/ÜNEP/Topfoto
155
3.4 Forests
M
uchoftheEarth’sabovegroundbiomassandbiodiversityisheldwithinitsforests.Forestsaresourcesof
food,fuel,constructionmaterials,fibers,andbiologicaldiversity.Forestsarealsoimportantinwaterandairfiltration,
carbonsequestration,soilstabilization,andtourism(Williams
1994,1990).Ithasbeenestimatedthatroughlythree-fourthsof
ahectareofforestlandisnowneededtosupplyeachpersonon
theplanetwithshelterandfuel(LundandIremonger1998).
Aroundtheglobe,thereareanumberofdifferenttypesof
forests.Theyareclassifiedaccordingtoaschemethatislargely
determinedbyclimateandlandformandthatdistinguishesevergreenanddeciduousforestsaswellasbroadleafandneedle-leaf
forests.
Deciduousbroadleafforests,forexample,tendtobefound
intemperatezoneregionsthathavedistinctseasonsandmoderateprecipitation.Lowlanddeciduousbroadleaf
forests—asourceofgreatbiodiversity—alsotendtogrowonsoils
consideredtobehighly
suitableforagriculture.
Consequently,manyof
thelowlandforestsin
theNorthernHemispherehavebeen
cutdownand
thelandthey
onceoccupied
convertedto
cropland.Lowlandforests
arecurrently
facingthe
samefatein
SouthAmerica
andAfrica.
Evergreen
broadleafforests—oftencalled
“rainforests”—
tendtooccurin
tropicalclimateswith
highlevelsofprecipitation.Deciduousneedle-leaf
forestsoccupyregionswith
climatescharacterizedbysevere
temperaturevariationssuchaseasternSiberia,
aregionwithextremelycoldwintersandtheSahel,aregionwith
extremelyhot,drysummers.Evergreenneedle-leafforestsoccur
throughoutpolar,temperate,andsubtropicalregions.Mixed
forestsoccupytransitionzones.Swampforestsandmangroves
existinareaswheresoilsaresaturated,oreveninundatedwith
freshwateroroceanwater,respectively.
Likeanytypeofecosystem,forestsundergochanges,both
naturalandhuman-induced.Attemptstodeterminehowforests
havechangedovertime,however,areoftencomplicatedbythe
factthatthereisnosingledefinitionastowhatconstitutesa
“forest.”Landparcelsmaybeclassifiedaccordingtotheircur-
Severaldifferenttermsareoftenassociatedwithforestsandthechangestheymay
undergo.Deforestationistheremovaloftreecoverandtheconversionoftheresultingdeforestedlandtosomeotheruse.Reforestationreferstore-establishingtreecoveronpreviouslyforestedland.Afforestationisthecreationofforestcoverwhereitdidnotpreviously
existorwhereitexistedonlyinthedistantpast.Forestdegradationreferstochanginga
foresttosuchadegreethatthespeciesthatinhabitthatforestcannolongercompetefor
survival;degradationtypicallyleadstolongtermchangesinspeciescomposition.
156
Forests
Br o ad l eave d everg r een
Br o ad l eave d d eci d u o u s
N eed l e- l eave d everg r een
N eed l e- l eave d d eci d u o u s
Mixed f o r es t
Sw amp f o r es t ( f r es h w ater )
Man g r ove ( s al t w at er )
Source: Global land cover 2000 (GLC 2000)
rentlandcover,potentiallandcover,currentuse,administration,ora
combinationofthesecriteria(Lund2002).TheUnitedNationsFood
andAgricultureOrganization(FAO),whichisresponsibleforglobal
forestresourceassessments,classifies“forests”usingadefinitionthat
combinesbothlandcoveranduse(FAO2001).Thiscanleadto
somelandsthatarewithouttreesduetofiresorclear-cuttingactivitiesbeingclassifiedas“forest,”whileotherlandsthatarecovered
withtrees,suchasorchardsandcoffeeplantations,areclassified
asagriculturallandorcroplandsratherthanforests.
Despitesuchcaveats,itisclearthattherehavebeensignificant
changesovertimeinthecharacterandspatialdistributionofforestsworldwide.Itisestimatedthatabout8000yearsago,forests
occupiedsome6200millionhectares(15320millionacres),or
approximately50percent,oftheEarth’slandsurface(Bryantet
al.1987).Today,lessthan4000millionhectares
(9884millionacres),or28percent,ofthattotalremains(FAO
2001).Thisreductioninforestcovercontinues.From1990to
2000,theglobalnetrateofdeforestationwasapproximately
94000km2(36294squaremiles)per
year.(Thisfigurerepresentsa
grosslossofsome123000
km2(47491squaremiles)
offorestperyearoffset
byanetgain,through
reforestationor
afforestation,of
roughly
29000to
30000km2
(11197to
11583square
miles)offorestperyear.)
Firesare
anatural
eventin
mostecosystems,includingforests.
Firesareoften
usedtoclear
landonforest
margins;occasionally,firesare
employedtobring
aboutachangeinland
use.Sometimesfiresare
simplytheoutcomeofincreasingnumbersofpeoplecominginto
contactwithforests.Mostforestlanddisappearanceisattributabletoconversiontopasture,cropland,or
urbanization.Forestecosystemsarealsodegradedbyfuel-wood
collectionandthegrazingofcattleandotherlivestock.
Gainsinforestareacomefromafforestationprojects,reforestation,firesuppression,andtheabandonmentofcroplands.
Amajorconcernofconservationistsistheconversionofnative
foreststotreeplantations.Theconversiontomonoculturaltree
plantationsisparticularlyharmfultothebiodiversityoftheoriginal,naturalforestecosystem.
Approximately12percentoftheworld’sforestsareprotected.
Butthisprotectionisunevenlydistributedaroundtheglobe.Itis
estimatedthatonehectareofnatural,once-inaccessibleforestin
Asia,SouthAmerica,AfricaandtheformerSovietUnionislost
forevery20hectares(49acres)offorestsetasideandprotectedin
NorthAmericaandEurope(Sohngenetal.1998).Justhowwell
theseforestsareprotectedoverecologicallysignificanttimescales
157
Br o adleaved evergreen
M an gr ove
Swam p fo r est
WorldDistribution
ofForestTypes
M ixe d f ore s t
Br o adleaved ever gr een
Broa dle ave d
eve r g re e n
Ne e dle -le ave d
de c iduous
Br o adleave d deciduo us
Needle-leave d ever gr een
Needle-leave d deciduo us
M ix ed fo r es t
Ne e dle -le ave d
eve r g re e n
Swamp fo r es t ( fr es h wat er )
Broa dle ave d
de c iduous
M angr ove ( s alt wat er )
Source:GLC2000
isalsoacontinuingissue.Thehistorical
trendisforpeopletocontinuetoconvert
moreandmoreofanyforestedlandscape
forotheruses.Often,theseconverted
landsendupaslow-gradepasture,withthe
resultthatforestecosystemsaredestroyed
forwhatamountstoonlytransienteconomicorsocialbenefit.Unfortunately,this
trendislikelytocontinueuntileitherthe
Br o adleave d dec iduo us
humanpopulationstabilizesordemands
Needle- leave d evergreen
forforestgoodsandservicesbecomesustainable—orboth.
Needle- leave d dec iduo us
Whateverthefutureholds,manyofthe
Mixed fo r est
imagesinthissectionshowtheprofound
Swamp fo r est (fresh water )
effectthathumanshavehad,andcontinue
tohave,ontheEarth’sforests.
Man gr ove (salt water)
ForestFire
Wildfirescanhavebothpositiveandnegativeeffectsontheenvironment.Insome
ecosystems,firesplayanecologicallysignificantroleinmaintainingbiogeochemical
cycles.Thebiologicaldiversityofplantand
animallifeintheworld’sforests,prairies,
andwetlandspartlydependsontheeffects
offire.Someplants,forexample,can-
notreproducewithoutfire;intenseheat
isneededtoopenconesorruptureseed
coatssothatseeddispersalandgerminationcantakeplace.Firesnaturallyshape
manytypesofecosystemsincludingtheborealforestsofCanada,Alaska,andRussia
andthechaparralinsouthernCalifornia.
Inadditionto“natural”fires,people
haveusedfireforthousandsofyearsto
clearland.Whethercausedbynatureorby
people,wildfiresareasignificantforcefor
environmentalchange,onethatcanradicallyalteralandscapeinaveryshorttime
(seeboxbelow).
TheEarth’sburgeoninghumanpopulation,coupledwithintensifiedeconomic
development,hasledtotheseriousdegradationofmanyoftheworld’sforests.
Degradedforestsareoftenhighly
CaseStudy:Rodeo-ChediskiFires
2002
Ontheafternoonof18June2002,afirebrokeoutneartheRodeoFairgroundsontheFortApacheReservationinArizona.Bymid-morningon
20June,theso-calledRodeofirehadexpandedto12000hectares(30000
acres).Meanwhile,asecondblazebeganburningnearChediskiPeakabout
24km(15miles)fromtheRodeofire,wherealosthikerhadstartedasignal
fire.Twodayslater,on24June,thetwofiresmergedtoencompassmore
than94000hectares(235000acres).Overthesubsequenttwoweeks,thefire
burnedanadditional80000hectares(200000acres),makingitthelargest,
mostseverewildfireinArizona.Beforetheblazewasbroughtundercontrol,
over30000peoplewereevacuatedand400homeswere
destroyed.Source:TheWildernessSociety2002
RodeoFire
Rodeo-Chediski
BurnedArea
24 June 2002
ChediskiFire
20 June 2002
158
The20June2002satelliteimagepicturedleftshowstheRodeoand
Chediskifiresburningseperately.The
24June2002imageaboveshowsthe
burnedareasofthetheRodeo-Chediski
fire.Areaswherefireswereburning
whentheimageswerecapturedappear
brightred;alreadyburnedareashave
adarkerredcoloration.Source:USGS
2002,NASA2002
Credits:Unknown/UNEP/USDAForestryService
Credit:UNEP/NASA
susceptibletofire.Loggingandlarge-scale
landclearing,forexample,disturbthe
microclimateofforestecosystems,increasingtheirfuelloadandthusthepotential
intensityofresultingforestfires.Changes
intheEarth’sclimate,characterizedby
extendeddroughts,higherglobalsurface
temperatures,andmoreviolentthunderstorms,hurricanesandothertypesof
severeweather,canfurtherintensifythe
riskofforestfires(RemoteSensingServicesGmbH1998).Concomitantly,fires
themselvesmayplayanimportantrolein
climatechangebyemittingbothgreenhousegasesandsmokeparticles(aerosols)
intotheatmosphere.
In2000,morethan350millionhectares
(865millionacres)offorestwereburned
worldwide—anareaequaltothesizeof
India(Northoff2003).However,whenfire
sweepsthroughaforest,manyofthetrees
maysurvive.Insomecases,thefiremay
burnonlythelow-growingvegetation.
completelyburningsmalltrees,vinesand
shrubs.Thedeadanddyingtreescollapse,spillingfirewoodandkindlingtothe
groundandcreatingopeningsintheforest
canopy.Logginghasasimilareffect.The
intensetropicalsun,previouslydeflected
AmazonForestsandFire
bythegreencanopy,heatstheforestfloor,
Beforewidespreadhumansettlement
pushingfiredangerevenhigher.Inthis
begantoencroachonthebordersofSouth damaged,fragmentedlandscape,theonset
America’sAmazonforests,therewasno
ofthenaturaldryseasonbringswithitan
suchthingasanAmazonfireseason.Now, ominousthreatoffire.Thatthreatgrows
firemayposethebiggestthreattothesurevengreaterwhenElNiño-drivendroughts
vivaloftheAmazonforestecosystem.
occurseveraltimesperdecade.
Slash-and-burnagricultureconverts
foresttofarmland,butthatobviousdestructionisonlythebeginning.Intentionallysetfiresoftenexpandoutofcontrol
andburnthroughtheunderstoryinareas
ofsurroundingforest,killing,butnot
CaseStudy:Pará,Brazil
2004
Onceextremelyrareevenduringdryseasons,fireisnowacommon
occurrenceintheAmazonrainforestaspeopleuseitasalandmanagementtool.Althoughlandmanagementfiresmaynotbeimmediatelyhazardous,itisnotuncommonforthemtoescapecontroland
becomeconsiderablymoredestructive.Forestfirescanalsoimpact
weather,climate,humanhealth,andnaturalresources.
Thesetwosatelliteimagesshowanareaoftherainforestinthe
stateofPará,Brazil,atthepointwheretheTapajósRiver(anglingup
fromthebottomofeachimage)joinstheAmazonRiver(running
acrosseachimage).Inthisregion,forestedlandisbeingclearedfor
logging,ranching,andfarming.Clearedareasarevisiblealongthe
riverbanks,extendingintotheforest.Deforestedareasappearlightgreen,whileundisturbed
forestisdarkgreen.
18 Nov 2004
Theimagedated18
November2004revealsthe
locationsofanumberof
fires(reddots)burningin
differentpartsoftheforest.
Roughlythreeweekslater,
firesarestillburningandthe
entirescenehasahazyappearance,theresultofsmoke
suspendedintheairoverthe
forest.Firesburnedoffand
oninthisregionformore
thanamonth.
Source:NOAA2004
7 Dec 2004
Credits:Unknown/UNEP/NASA
159
CaseStudy:DemilitarizedZone
TheKoreanDemilitarizedZone(DMZ),which
separatestheRepublicofKorea(ROK)tothe
southandtheDemocraticPeople’sRepublic
ofKorea(DPRK)tothenorth,represents
anopportunitytopreserveanenvironment
relativelyuntouchedbyhumanssincetheUN
establishedthepoliticalbufferin1953.
TheDMZcontainsfiverivers,andmany
ecosystemtypes:forests,mountains,wetlands,
prairies,bogs,andestuaries.In2001,theROK
governmentcompletedasixyearstudyof
theecosystemintheDMZ,the250-km-long
(155-mile-long),4-km-wide(2.5-mile-wide)
no-man’slandthatseparatestheKoreanPeninsula.Ithousessomeoftheworld’srarestspeciesoffloraandfauna.SouthKoreanofficials
beganpushingaheadwithaprojecttoregister
partoftheDMZwithUNESCOasaTransboundaryBiosphereReserve(TBR).Theidea
ofanearly100000hectares(247105acres)
preserveinsuchalocationisquiteintriguing
andunique.
SatelliteimagesrevealsignificantburnscarsintheDMZ.
ReportsstatetheburningistheresultofmilitarysurveillanceoperationsperformedbybothROKandDPRK.
Militaryofficialsreported19majorfireswithintheDMZin
2000,burningnearly400km2(154squaremiles)ofland.
AgreementsinFebruary2001tostoptheburningforpreservationofthefloraandfaunadissolvedwithincreased
tensio