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Waiting for the water to come?
Dr. Fabian Scholtes, ZEF
Dr. Anna-Katharina Hornidge (Case study Indonesia), ZEF
EDITOR:
CARE DEUTSCHLAND-LUXEMBURG, CENTER FOR DEVELOPMENT RESEARCH (ZEF) 2009
Waiting for the water to come?
Foreword 4
Abstract 6
I. Introduction: climate change and poverty reduction are inseparable 7
II. Climate change 9
II.1 Climaticeffectsofglobalwarming 9
II.2 Physicaleffectsbeyondclimatechange 11
II.3 Consequencesandextremeeffectsofclimatechange:feedbackandtippingelements 13
II.4 Economicandhealthimpacts 14
III. What climate change impacts are anticipated in future? 15
III.1 Globalprojections:impacts 18
IV. Climate change and poverty reduction 18
IV.1 Climatechange,povertyandpovertyreduction:howaretheyrelated? 18
IV.2 Adaptingtotheimpactsofclimatechange 21
IV.3 Supportingresilience 22
IV.4 Criteriaforsuccessfuladaptationmeasures 23
IV.5 Measures 25
V. Poverty reduction and strategies to secure livelihoods: case studies and lessons learned 27
V.1 SmallholderfarmersinTanzania:specialisingandreducingdependenceonagriculture 27
V.2 MicroinsuranceinIndia:thepoorprotectthemselvesagainstrisks 29
VI. Case study West Timor, Indonesia 31
VI.1 Impactsofclimatechangein(East)Indonesia 31
VI.2 Toineke,WestTimor:economyandsociety 31
VI.3 Perceptiblelocalimpactsofclimatechange 32
VI.4 Copingandadaptationstrategies 35
VI.5 Toineke:anexampleoflifeinpovertyinconditionsofclimatechange 41
VII. Recommendations: poverty reduction in times of climate change 42
Bibliography 44
Imprint 46
limatechangeisaglobal riskforhumanity,asUlrichBeck, well-knownGerman sociologist and
globalizationexpert,hassaid;itwilldetermineourpresentandfutureonascalenotyetforeseen.
Itisprimarily causedbythecountriesoftheNorth,yetthecountries of the Southaremoreseverely
impactedbysomeoftheconsequences.Thisdisproportionateeffectispartlyduetothefactthatlarge
numb ers of pe ople in d eveloping countr ies are highly depend ent on th e natural environment. A s a
result,thepopulationswhobearthebruntofparticularrisksarethosewhohaveneithercausedclimate
change, nor benefitedfrom the achievementswhich contribute to it. Poorpopulations in developing
countriesareforcedtoreacttoenvironmentalproblemssuchasdroughtsandflooding,watershortages
andchangingrainyseasons:problemswhichtheycanhardlypredictandwhicharecausinganincreasing
senseofuncertainty.Allthisleadstoagrowingneedforinterdisciplinaryandtransdisciplinaryresearch,
whosefindingscanprovideabasisforplanning.
TheCenterforDevelopmentResearch(ZEF)attheUniversityofBonncarriesoutinterdisciplinaryresearch,
aimingtocontributetopovertyreductionandsustainabledevelopment.TheZEF’sgoalistofindlocal
solutions to problemscaused globally andtocombine current researchfindings withthe experience
oflocalpeople.Thispaperfocusesonpreciselythisintegrationofinterdisciplinaryresearchinadevel-
opment context (ZEF) and pract ical, poverty- oriented cooperative development (C ARE).It ef fectively
presentsthecurrentstateofresearchonclimatechangeandpovertyreductionandcombinesthiswith
thelocalknowledgeandinnovationsdevelopedbythepeopleofEastIndonesia.
CAREandZEFaimtopointthewayforfutureresearchincollaborationwithorganisationswhichtackle
poverty.Onlyifpracticalandscientific,localandcross-borderknowledgecanbebroughttogetherwill
theinevitableadaptationstoclimatechangeimpactshaveachanceofsuccess.
Prof.Dr.SolvayGerke
DirectorZEF,DepartmentofPoliticalandCulturalChange
C
C
limat e change is tak ing pla ce world wide; i ts impa cts ar e direc t and se vere – es pecial ly for th e
poorest,whoareleastresponsiblefor thecauses.Climatechange acceleratedbyhumanactivity
isalteringtherhythmofnaturalweathereventssuchasdroughts,floodsandhurricanes.Itisgenerally
assumedthatclimatechangeisexacerbatingpoverty,butwhatistheevidenceforthisassumption?How
exactlyare thesephenomenarelated and whatdoes that mean for an organisationlike CARE, which
combatspovertyworldwide?
Thispaperaimstoprovide anoverview ofthestateofthedebate onpovertyreductioninthe faceof
climatechange.Theauthorshaveinvestigatedthelinksbetweenpovertyandclimatechangeinpractice
andexaminedtheissuesinthelightofacasestudyinIndonesia.Theyhavedeliberatelyselectedacoun-
trywhichisbothparticularlyaffectedbyclimatechangeandalsooneofthosecausingglobalwarming.
Thefindingsareclear:climatechangedoesmaketacklingpovertymoredifficult.Anditseemsthatmore
andmorepeopleareindangerofslippingintopovertyduetochangingenvironmentalconditions.
Thecentralthemeofthispaperisthehumanitariantaskofsecuringpeople’slivelihoods,sinceindividuals
andtheirimmediateenvironmentarethelowestcommondenominatorofglobalclimatechangeandits
consequences.Allovertheworld,inAsia,AfricaorLatinAmerica,thepoorestofthepoorareaffected
by climate change andare forced to adapt to the consequences. Their success will dependpartly on
theirknowledge,theircapitalandontheassistancetheyreceive.ForanorganisationsuchasCARE,the
challengeofsustainablepovertyreductionintheeraofclimatechangewilldemandallourstrength.
CAREsupportsmillionsaroundtheworldwhoaresufferingtheeffectsofclimatechange.Forthem,itis
aquestionofsurvival.Thisdailyexperienceshouldremindusthatclimatechangehasahumanface.
Dr.AntonMarkmiller
NationalDirector,CAREDeutschland-Luxemburg
Itisthe poorwho suffermost underthe impactof climate
change.Theyareoftendirectlydependentonthenaturalen-
vironmentandhavefewoptionstoescapetheconsequences
ofchangesuchaspoorharvests,watershortagesandillness.
Theirsurvivalstrategiesandlivelihoods are endangered,in
somecasesacutely.
Climatechangemakespovertyreductionmoredifcult.First,
itishardertohelppeopleoutofpovertywhenconditionsare
increasinglyuncertain:butclimateprojectionsareoftenun-
certain,makingitdifculttoassessthe effectivenessofad-
aptationmeasures.Second,thereisthedangerthatclimate
change willreduce morepeople to poverty,increasing the
numbersofthosewhoneedassistancewhiletheresourcesof
thosetacklingpovertyarelimited.
Thispaperpresentstheconsequencesofclimatechange,the
waysclimatechangeisanticipatedtodevelopinfutureand
aspectswhichmakethepoorparticularlyvulnerable.Thefo-
cusisonthemeasurespeoplethemselvescantaketomain-
tain and adapt their livelihood strategies to the changing
climateconditions.
Weshowhowpovertyreductionislinkedtoclimatechange,
thefundamentalgoalsandcriteriaofpovertyalleviationand
concrete examples of how it can include adaptati on tocli -
mate change impacts. Various case studies from Tanzania,
India and Indonesia illustrate in detail how both people’s
ownadaptationstrategiesandtheworkoforganisationslike
CAREcanconstitutesuccessfulreactionstotheconsequences
ofclimatechange.Finally,conclusionsaredrawnintheform
ofrecommendationsfororganisationslikeCARE.
RECOMMENDATIONS FOR ORGANISATIONS ON
POVERTY REDUCTION
Povertyreductionshouldprioritizeadaptationtochang-
ing climatic conditions (not merely coping with them)
andbebasedonexistinglocalstrategies.
Local knowledge of relations between climate change
eventsandlocaladaptationoptionsshouldbesystemati-
callyincluded;localpopulationsshould alsobeencour-
agedtodeveloptheirknowledge.
However, existing practices as well as new strategies
should be crit ically examined applying ve criteria (ef-
fectiveness, exibility, fairness, efciency and sustain-
ability).
Tackling poverty should promote awareness of and in-
dependentlocaladaptationtothoseclimatechangeim-
pactswhichhavesofarattractedlessattention.
Theactualimpactsofclimatechangeareextremelyhard
topredict. This fact should not beignored andcurrent
projectionstakenas“certain”whenplanningadaptation
measures.
Theurgencyofadaptationtoclimatechangeshouldnot
beusedtojustifymeasures(suchasforcedresettlement)
withouttheagreementofthelocalpopulation.
Poverty reduct ion measures should be realistic and or-
ganizationsshouldconcentratetheirenergies,aimingto
preservethepoorestpeople’sgeneralresilienceandca-
pacitytoact.
Profound,broad-basedandcriticalanalysisoftheextent
ofclimatechangeimpactsandadaptationmeasuresises-
sential.Common recommendationssuchas diversifying
incomehavesometimesprovedunproductiveorcounter-
productiveintacklingpoverty.
THE POOR ARE PARTICULARLY AFFECTED BY CLIMATE
CHANGE AND VULNERABLE TO ITS IMPACTS
Thepoorarebothparticularlyexposedtotheeffectsofcli-
matechange and havefewresourcestocombatit.Thisisa
frequenttopicintheclimatechangediscourse.Butwhatex-
actlydoesitmean?Andhowdoesthisfactaffecttheworkof
organisationswhichtacklepoverty?Thesethoughtswerethe
startingpointforthispaper.Theauthorsassumethefollow-
inghypotheses:
I. Climate change and poverty reduction are inseparable
Howfarclimatechangeanditsconsequencesactuallyaffect
individual lives depends on how vu lnerable they are to its
impacts.Severalfactorsinuencethis:
Globalclimatechangeimpactsvaryaccordingtolocality.
Theimpactonpeopledepends onlocal climaticeffects
such as rising temperatures or changing precipitation
patterns.Local climatic changes such as heatwaves can
haveanimmediate,directimpactonthepopulation.
Localecologicalandsocialsystemsarenotequallysensi-
tivetolocalclimaticchanges.Alterationstotheenviron-
mentaffect peopledirectly:if the ground driesoutbe-
cause of rising temperatures,agricultural production is
moredifcult.Therobustnessofthelocalinfrastructure
isalsoasignicantfactor–forexample,whetherroads
canwithstandheavyrainfall.Theseeffectscanreinforce
eachotherandcreateaviciouscircle.
Theextenttowhichindividualsareactuallyharmedby
these effects depends on how exposed they areto the
consequences(e.g.howdependent they are on agricul-
ture)and howthey resist, cope with or adapt to them.
These coping oradaptationcapacities may include fac-
torssuch as whetherthe localpopulation has accessto
thetechnologyrequiredtomaintainagriculture,wheth-
er they have sufcient cash to impor t food instead or
whethertheycanutilizeothersourcesofincome.
Tosumup,thegreater thescale oflocal climatechangeef-
fectsforthepopulationandthelesstheyareabletoadaptto
theimpacts,thegreaterthedamagethatcanbewroughtby
climatechangeontheirlives.Thepooroftenliveinparticu-
larlyvulnerableareas(regionswithextremeclimates,coastal
areas,regions affectedbyregularriverooding).Thelikeli-
hoodofbeingaffectedbyaclimatedisasterisaroundeighty
timeshigherin developingcountriesthaninmembercoun-
triesoftheOECD(HDR2008:20/21).Inaddition,itistheru-
ralpoorwhoselivelihoodsaredirectlydependentonnatural
resourcesandwhoaremostaffectedbyclimatechange.
Climatechangeisnotthesolecauseofpoverty,butitworks
withotherfactorstointensifytheviciouscirclewhichtraps
peopleinpoverty.Thismakesithardertohelppeopleoutof
thedownwardpovertyspiral.Itisalsolikelythatmorepeo-
plewillfallintopoverty ifclimatechangeunderminestheir
current livelihood strategy. The Stern report (Stern 2006)
statesthat145to220millionpeopleinAfricaandSouthAsia
couldbecomepoorby2100.“Climatechangeisundermining
internationaleffortstoreducepoverty“(HDR2008:10).
Thesetwofactors,theincreaseinnumbersofthepoordueto
climatechangeandtheincreaseddifcultyofassistingthem,
reinforceeachother;thisiswhyclimatechangehasasigni-
cantinuenceonaidorganisations’work.Thispaperdenes
climatechangemoreprecisely,tracesitsphysicalandsocio-
economiceffectsonpovertyandexamineswhatthismeans
foreffortstotackle poverty.Weshow how climate change
inuencespeople’s opportunities andlivelihood strategies,
soindicatinghowaidorganisationscanreacttoalterations
causedbyclimatechange.Thisisillustrated byexamplesof
howpeoplehaveattemptedtoadapttoclimatechange.The
casestudyofthevillageToinekeshowsverypracticalstrate-
giesandindividual cases and reveals how aid and develop-
mentorganisationscancontributetothereductionofpover-
ty.Thisprovidesabasisforrecommendationsforsuccessful
povertyreductioninthemoredifcultconditionscausedby
climatechange.
Anoutlinepapercannotcoverallaspectsofthetopic.Migra-
tionandconictovernaturalresourceshavebeendiscussed
indetaile.g.in the German Government’sAdvisory Council
onGlobalChange’sreport (WBGU2007)andtherefore are
not dealt with here. Technological advances such as early
warningsystemsarementionedbutnotdescribedindetail.
Thecasestudieswereselectedinviewofthefocusonliveli-
hoodstrategiesandpeople’sadaptationmeasures,especially
thoseofthepoor.
II. Climate change
CONSEQUENCES AND PROJECTIONS OF CLIMATE
CHANGE
Firstofall,thetermclimatechangereferstotherisingatmos-
phericandoceantemperaturesobservedinrecentdecades.
The global climate has alwaysbeen subject tochange, but
todaytheemissionofgreenhousegasescausedbyhumanac-
tivity–inparticularcarbondioxide,butalsomethaneandni-
trousoxide-reinforcesthenaturalgreenhouseeffectandso
causeglobalwarming.In2004,31%oftheseemissionswere
causedbyagricultureandforestry,40%byindustry,transport
andbuildingsand26%byenergysupply(IPCC2007c:29).The
natural greenhouse effect produces an air temperature at
groundlevelofapprox.15°C,thusenablinglifeasweknow
ittoexist. The additionalanthropogenic greenhouseeffect
iscausingadangerousincreaseinthistemperature.Thisoc-
cursbecauseastheconcentrationofgreenhousegasesinthe
atmosphereincreases, they areheatedby the earth’sinfra-
redradiation andthusproduce more radiation themselves.
This“atmosphericradiation“isreecteddowntoreachthe
earth’ssurfaceinadditiontothesun’senergy,soheatingthe
earthadditionally(Philiponaetal.2004).
II.1.CLIMATIC EFFECTS OF GLOBAL WARMING
Theinitialimpactofclimatechangeisthereforeglobalwarm-
ing.Thisislinkedtoprocesseswherebyclimatechangeaffects
thenaturalenvironmentandthehumanpopulation,particu-
larlyincausingalterationstoweatherpatterns.Climate,inthe
senseofthe“averageweather”inaregion,comprisesrstof
alltemperature,precipitationandwindconditions.
Not only are average air temperatures rising; temperature
extremesmay alsobecomemore frequent.Thereare more
extremely hot days, heat waves occur more often and
extremely cold perio ds will probably occur less frequently.
Risingtemperaturesarealreadyaffectingpeopledirectly,for
examplethosewithcoronaryorbloodpressureproblems.The
poorinhotcountriesareparticularlyaffectedandvulnerable;
they usually have no access to preventive technology
such as air conditioning. They are often malnourished or
undernourishedandcannotcopewiththeheat.
The indirect consequences of r ising temperatures can take
variousforms.Therhythmoftheseasonsalters,sothewarmer
seasons s tart earlie r and last lon ger. In many regions, this
iscoupled with changes in precipitationpatterns,resulting
inlongerdryperiodsandleadingtomorewatershortages,
curt ailment of grow ing seasons and reduced har vests. T he
people of Toineke, West Timor, are confronted w ith these
effects, as the case study shows. Geographically, climate
zones and thus vegetation zones are shifting; for example,
previouslytropicalareasarenowthreatenedwithentirelynew
regionalclimates.Theactualadvantagesanddisadvantages
thismay bringtothelocalpopulationareoftenimpossible
toestimate.However,itisalreadyclearthatthereplacement
of forest by savannah and savannah by desert will cause
particul ar problems for people whose livelihood is directly
dependentonnaturalresources.Thiscanbeseeninthearid
zonesofsouthernAfrica(Scholz/Bauer2006).
Climatechangealsoleadstochangingprecipitationpatterns.
Inawarmerclimate,globalprecipitationquantitiesincrease,
as rising temperatures cause more evaporation of water,
whichthenfallsasrain.Iftheraindoesnotfallasquicklyas
neartheequator,cloudscarrythewaterintohigherlatitudes.
ThiseffecthasreducedrainfallintheSahelregion,aroundthe
Mediterranean,insouthernAfricaandinpartsofsouthAsia
(IPCC2007a).Thisisleadingtoashiftinareasofrainfall,so
subtropicalregionsarebecomingdrierandhigherlatitudes
wetter.Rainfallwillincreasinglytendtobelessfrequentbut
more intensive. There will be fewer days wi thr ainfall, but
heavyrainfallwillbemorecommonanddryperiodslonger.
Thiscanleadtoextremeweatherconditionssuchasooding
orhighriverlevelsduetoheavyrainfall,orontheotherhand
todroughts.
These effec ts are very different in different locations. The
likelihood of drought is increasing in the Mediterranean,
in southern Africa and in the Brazilian Amazon region in
particular.However,inareaswhererainfallisincreasing,the
amountofsurfacewateravailabletothepopulationwillalso
decrease–becauseofhighlevelsofevaporation.Increasing
rainfallalso tends tooccurinthe rainy season,whichdoes
notimprove water availability in dry periods(Arnell 2004).
Thepooraremostaffected:theyarethersttoloseaccessto
reducedwatersupplies,arelessabletotreatcontaminated
waterandarethusmorevulnerabletodisease.
Thesechangingweatherpatternsliterallydeprivepeopleof
their economic base. Firstly, the dried- out ground is more
subject to erosion; heavier rainfall also contributes to this
effect. Deforestation and overgrazing make the land even
more vulnerable. Secondly, soil degradation will increase,
forexamplethroughsalination,inareaswhereirrigationis
overusedtocompensateformorerapidevaporation(WBGU
2007:74).Agriculturalproductionwillfallasaresult.People
who depend on subsistence farming will be particularly
affected,buttheurbanpoorwillalsofacerisingfoodprices
whentheamountofagriculturallandisreduced.
Changingprecipitationpatternsareveryhardtopredict.This
istypicalforthecentralproblem climatechange causes for
povertyreduction:ontheonehand,futuredevelopmentsare
predeterminedbecauseprocesseshavebeenirrevocablyset
in motion and people must cop e with them. On the other
hand, the future is dangerously uncertain, since previous
knowledge,forexampleaboutwateravailability,isnolonger
applicabletothefuture.Knowledgeofthenewsituationisstill
beinggatheredandisnotcertain;thepeopleaffectedoften
lackawarenessoftheglobalprocessesinvolved.Thisreduces
theircapacityfor action. Previously,variations occurredon
alimitedscaleandcouldbecopedwithbymeasuressuchas
watermanagement. However,climatechange haschanged
the scale to such an extent that these coping mechanisms
arenolongersufcient(Millyetal. 2008).Thecombination
ofinevitablityandunpredictabilitymakeitmoredifcultto
plan for the future. The people of Toineke, Indonesia, for
example, do not know whether the ooding will recur in
future,sotheychoosecheaper provisionalmeasuresrather
thanlong-term adaptations. Instead ofraising their houses
onstiltsasalong term solution,theysimplyraise sleeping
andcookingaccommodationandanimalquarters;however,
thisstillleavesthemvulnerabletoooding.Thecoreofthe
problemisthereforethe“deteriorationoftheplanningbase
inthenaturalenvironment”(WBGU2007:70)–bothforthe
people’sownlivelihoodstrategiesandfortheorganizations
workingtoreducepoverty.
Discussions about wind focus above all on the increasing
frequencyandintensityoftropicalhurricanescausedbyrising
seatemperatures.However,itisdifculttoestablishaclear
relationshipbetweenclimatechangeandincreasingnumbers
of storms (WMO 2006). Future temperature increases are
likelyto boosttherisein numbers ofstorms(WBGU2007),
butsomestudiesdisputeeventhispoint(Knutsonetal.2008).
Thepopulationsofendangeredcoastalareasareincreasing,
sothestormswillhaveincreasingsocietalimpacts.
II.2 PHYSICAL EFFECTS BEYOND CLIMATE CHANGE
Risingtemperaturesaffectnotonlytheclimatebutalsoother
systems,suchastheoceans.Thebest-knowneffectistherise
insealevels,causedbytwofactors:
the expansion of the water as it heats up and the increas-
ingquantityofwaterasglaciersandinlandicesheetsmelt.
Thisprocessendangerslow-lyingislands,coastalregionsand
riverdeltasinparticular.Floodserodethecoastline,damage
infrastructure and alter groundwater and drinking water,
sometimes als o causing disease through water contamina-
tion.Thiswillinevitablyaffectlargenumbersofpeople,be-
cause approx. 70% ofthe world’spopulationlive inthese
areas.Thepoorwillfeeltheeffectsevenmore,becausethey
tendtoliveinlessshelteredareasininadequatehousingand
aredependentonnaturalresourceswhicharedestroyedby
ooding. Even if they are able to move away from the af-
fected areas, they lose their livelihoods and do not always
succeedin nding newlivelihoodsevenincities(IISD2003:
14).An annualsea levelriseof only40 centimeters would
oodtheregionswhicharehometo95millionpeople,afth
ofwhomliveinsouth-eastAsia(Wassmannetal.2004).
Risingocean temperatures enablethe seas to absorbsome
oftheexcesscarbondioxideintheatmosphere;theyactas
carbonsinks,thuscounteractingclimatechange.However,as
theCO2isabsorbedbythewater,theoceansbecomemore
acidic,endangeringthecoralreefswhichatpresentsheltera
richvarietyofmarinelifeandtheminuteseacreaturesatthe
bottomoftheoceanfoodchains(WBGU2006).
Oceancurrentsarealsochanging.Uptonowtherehavebeen
fearsthattheconstantcirculationprovidedbytheNorthAt-
lanticDriftmightbeweakenedoreveninterruptedbyclimate
change.Thiswouldcausea massive drop in temperature in
western and northern Europe. However, it is also possible
thatoceancurrentswillbecomestronger(Toggweiler/Russel
2008). Both acidi cation and changing currents affec t sh-
ery,another areawhere thepoor arethe rst to suffer,as
their small boats do not allow them to follow the remain-
ing sh reserves. In the end, climate change w ill affect all
ecosystems.Ahugelossofbiodiversityislikely,thoughthis
effect w ill also vary from place to place. In polar regions,
warmingcouldincreasebiodiversity(Weller2007:1017).The
increasedspeedof change inbiodiversity,especiallyextinc-
tions,canunbalanceecosystems.Thisaffectsnotonlynature
lovers,butthewholeofhumanity,sincewearealldepend-
entonthesesystems.
BOX 1: CASCADE EFFECTS:
A DAM BURST SCENARIO
Apaper bytheFeinsteinInternationalCenter(2008)illus-
tratesthecascadeeffectwithadisasterscenarioinwhich
global warmin g causes the Tibet an glaciers to me lt. The
water combines with extreme rainfall to ll the Three
GorgesDamsothatthewatertriggersseismicactivity.The
earthquakesandwater pressure break thedam,ooding
citiesdownriverwith2.5millioninhabitants.Politicalun-
restfollows;investorswithdraw;theresultisaneconomic
crisis etc.Attheend of thecascade, 1 millionpeopleare
dead,4milliondisplacedandtheeconomiccostrunsinto
hundredsofbillionsofUSdollars.
Climate change also lies behind less dramatic chains of
eventswhichalso have disastrous effects, e.g.failedhar-
vests,leadingtomigrationofworkers,increasingpopula-
tionpressureinthecitiesanddepopulationofruralareas.
Thismaycausemorepressureonurbaninfrastructureand
thecollapseoftheruraleconomy.
Otherconsequenceswhichaffectpoorercountriesinparticu-
lararethe reductionofmonsoonrainfallinIndiaandWest
AfricaortheincreasingfrequencyandseverityoftheElNiño
phenomenon, which causes various effects including ex-
tremelyheavyrainfallinthecountriesontheeasternPacic
rim(Lentonetal.2008).
II.3 CONSEQUENCES AND EXTREME EFFECTS
OF CLIMATE CHANGE: FEEDBACK AND TIPPING
ELEMENTS
Risingtemperaturesdue toclimatechangenotonlycausedi-
rectalterationsintheweatherortheoceans.Feedbackeffects
also occur, where climate change impacts themselves affect
theclimate,oftenreinforcingtheeffects.
Forexample,themeltingoftheArcticicecapmeansthatless
solar energy is reected ba ck into space, so increasing at-
mospheric temperature. The ice b ecomes sea water, which
isdarker,absorbs more solarenergy,becomes warmer and
causestheicetomeltfaster–negativefeedback,infact.And
ifthehugemethane reserveslockedasgashydratesinthe
Siberianpermafrostordeepintheoceanshouldbereleased
by climate change, they will give the greenhouse effect a
massiveboost.
Theconsequencesaffectnotjusttheglobalclimatebutalso
havesocietaleffects.Achangeintheweathercantriggeran
uncontrollablecascadeofeconomicandsocietaleffects(see
box1).Oneofthedifcultieswithcascadeeffectsisthatitis
oftenunclearwhat willhappen next.Simultaneouseffects,
whereseveraleventsoccuratonetime,areanotherproblem.
Ifa heatwaveand ooding occursimultaneously, a society
maynotbeabletocopewiththesubsequentdoubledisrup-
tionofwaterreserves.
Climate change impacts are not all gradual: they can also
triggerdevelopmentswhichaltertheglobalsystemabruptly
anddrastically.Theclimatesystemhastippingpointswhere
eventsachieve anuncontrollable momentum; for example,
theAmazon rain forestwill dry out irreversibly once ithas
reached a certain threshold; the North Atlantic Drift may
weaken;theGreenland icesheetwillmeltirreversibly once
certaintemperatureshavebeenreached(WBGU2007:77ff).
II.4 ECONOMIC AND HEALTH IMPACTS
Theclimatechangeeffectsdescribedimpactthepoorinpar-
ticular.Around60–70%ofthepoorworldwideliveinrural
areas,mainly fromagriculture.This isthe economic sector
mostaffected(seeFig. 1, from:HDR2008:23).Subsistence
farmersaremostendangerediftheyhavenoalternativein-
comesources.
IItisimpossibletosayatpresenthowfarothereconomicsec-
torswillbeaffected(WBGU2007:75).Itisforeseeablethat
long-term energydemands willincrease as rising tempera-
turesleadtoincreasedcoolingrequirements,whichwillnot
be entirely compensated for by reduced heating d emands.
An upsurge in energy prices w ill have a corresponding ef-
fect on effor ts to reduce poverty. Extreme weather events
willalsoaffecttheinsuranceindustry,withconsequencesfor
attemptstogivethepooraccesstomicroinsurances,tohelp
themsafeguardthemselvesagainstlossesduetotheweather
(seealsothecasestudyonIndia,page29).Tourismmayalso
beaffectedwithknock-oneffectsonthepoor;itispredicted
thattourism,andthusasourceofincome,willshiftfromde-
velopingcountriestomorenorthernlatitudes.
Apartfromthesetrends,itisuncleartowhatextentindividu-
alsectorswillbeaffected.Discussionisfocussingincreasing-
lyonclimatechange’soveralleffectsonnationaleconomies.
Thebest-knowncalculationisprobablythatpresentedinthe
Sternreport(Stern 2006), where an inevitable lossof 5%,
possiblyupto20%,ofglobalgrossdomesticproduct(GDP)
ispredictedifclimatechangeisnotsloweddown.Theseare
controversialgures. According to theIPCC, however,most
calculationsagreethatariseofafewdegreescelsiusinglo-
baltemperatures would causeglobal GDPlosses of several
percent.This effect,too,willhitsomecountriesdispropor-
tionatelyhard,especiallythoseinlowerlatitudes.Reductions
ofupto30%insomesmallnationaleconomiesarealready
beingpredictedforaglobaltemperatureriseof2°C(WBGU
2007:76).Thepoorarenotonlygeographicallymorevulner-
abletonegativegrowth;anothereffectwillbethatshrinking
taxincomeswillleavestateswithevenlessfundingforsocial
anddevelopmentpolicy(Cordetal.2008).
Increasesinrainfall,oodinganddroughtarealsoaccompa-
niedby a higherincidence ofwater-borne diseases,in par-
ticulardiarrhoea,choleraandtyphus.Accordingtothepeo-
pleofToineke,diarrhoealillnessesspreadwithinweeks.The
incidenceofthesediseasesispredictedtoriseespeciallyin
East,SouthandSoutheastAsia,duetoacombinationoflack
ofcleanwater,pollutionofexistingwatersources, general
livingconditionsandlevelsofhygiene.Changesinthelocal
watersituationcanalsoleadtomosquito-bornediseases;the
insectsbreedwherever(contaminated)surfacewatercollects,
e.g.throughincreasedrainfallorthewideruseofirrigation
systems.Theregionsandperiodsaffectedbytheseillnesses
willexpand.SouthernAfrica,theHornofAfrica (Cordetal.
Global
Developing countries
Asia
Middle East and North Africa
Latin America
Africa
Industrialized countries
Changes in agricultural production potential
(2080s, in % of the potential of 2000)
2008)and Central Asia(IPCC2007b:408)arethreatenedby
thespreadofmalaria.Theincidenceofdenguefeverwillin-
creaseinurbanareaswherethelackofwastewaterdisposal
systemsprovidesmosquitoes with breeding grounds. Most
ofthe victims will be the urban poor,subsistence farmers,
groupswith weaker immune systems(theelderly,children)
andcoastaldwellers(WBGU2007:77).
Fig. 2 (after Cord et al. 2008) summarises some effects of
climatechangeandtheirdiverse,complexinteraction.Italso
illustrates the particul ar vulnerability of the poor to these
impacts.
At present it is hardly possible to predict how the climate
changeeffectsdescribedabovewill actuallyplay out inin-
dividualregions.Thisismainlyduetotwofactors(C.Müller
2009:9ff).First,theglobalclimateissocomplexthatallmod-
elsofitare verysimplied,i.e.only partialand/orapproxi-
mate.Retrospectivemodellingofglobaltemperaturesinthe
twentiethcenturyarerelativelygood;however,precipitation
patterns and regional detail s areina ccurately represented.
TemperaturerisesshowninhalfthemodelsforAfricawere
lowerthanwereactuallyobserved.Rainfallwas30%under-
or 79 % overestimated in the models compared to actual
III. What climate change
impacts are anticipated in
future?
Climatechangeand
climaticimpacts
Directimpacts
Degradationandlossof
naturalresources
Spreadofenvironmen-
tallycauseddiseases
Lossofnaturalhabitats
andbiodiversity
Reducedincomefrom
agriculture,fisheryandna-
ture-dependenteconomy
Deterioratinghealth;
decliningcapacitytoact
andadapt
Migrationtriggered
byenvironmental
developments
Alterationstorelativeprices:
foodpricesrise,affecting
thepoorinparticular
Slowergrowth:f iscal
marginfore.g.socialpolicy
declines
Growingriskofconflict
Impactsonhouseholds Socialimpacts
Renewed,additionalandworseningpovertyandpovertytraps
projected development of total CO2 emis-
sionsintheatmosphereduringthe21stcen-
turyaccordingtoeachofsixIPCCscenarios.
Italso illustrates the maximum total emis-
sions and the climate-friendly CO2 budget
requiredforthiscenturyifdisastrousclimate
change is tobe avoided.The conclusion is
thatdangerouslevelsofclimatechangecan
only be prevented if future emissions are
halvedby2050comparedto1990levelsand
subsequentlyreducedevenfurther.
amounts(ibid.,p.17).Projectionsbasedonthesemodelsare
correspondinglyunreliable.
Second,thedriversofclimatechange,aboveallgreenhouse
gasemissions,varydependingonhumandecisions–which
areunpredictable.Thisiswhyscenariosareusedtodescribe
alternative emissions processes. Another important func-
tionofthescenariosisthattheyalsoindicatewhatalterna-
tivecoursesofactionarenecessarytoavoidclimatechange
reachingdangerousproportions.TheIPCC’sscenariosshow
projected future situations with variations in population
growth, technological change, energy use, energy sources
andlanduse(Nakicenovic/Swart2000),factorswhichsigni-
cantlyaffectthescaleofemissionsandofclimatechange.
TheCarbonBudget2007reportpublishedinSeptember2008
(TheGlobalCarbonProject2008)showshowCO2emissions
haveincreasedinrecentyears,risingfourtimesfastersince
2000 than before. Th e following diagram from the Human
Development Report 20 07/20 08 (HDR 2008: 20) shows the
7.000
6.000
5.000
4.000
3.000
2.000
1.456
1.000
2000 2032 2042 2100
0
Fig.3
1IPCCscenarioA1FI
2IPCCscenarioA2
3IPCCscenarionA1B
4IPCCscenarioB2
5IPCCscenarioA1T
6IPCCscenarioB1
7Sustainableemissionscurve
CO2budgetwhichwould
preventdangerousclimate
change
Explanation: the describe plausible future global developments in population,
economicgrowth,technologicalchangeandrelatedCO2emissions. The assumestrong
populationandeconomicgrowth,linkedtodependencyonfossilfuels(A1FI),non-fossilfuels(A1T)or
acombinationof both (A1B). The assumes weaker economic growth,a lesserdegreeof
globalizationandmuchhigherpopulationgrowth.Theandincludeacertainreduction
in emissions due to increasingly efc ient useof resources and technological improvements(B1)or
increasinglydecentralizedsolutions(B2)
Source:Meinshausen20 07
1
2
3
4
5
6
7
Inthe long term,very differentrisingtemperaturepatterns
arepossible, depending onwhich emissions scenario actu-
allyoccurs. Ifgreenhouse gasconcentrations are stabilised
atbelow 450 ppm (partsper million,the usual measureof
greenhouse gas concentrations in the atmosphere), global
warmingcouldbeheldatatotalof2°Cabovepre-industrial
levels.Increasesbeyondthisraisetoover50%theprobabil-
ity of climate change reaching dangerous levels. If the cli-
mateisnotprotected,risesofupto7°Carepossible.These
areglobalaverages;theguresonthecontinents,especially
inthemostvulnerableareas,aremuchhigher.IntheIPCC’s
twomostextremescenarios,thetemperatureispredictedto
rise2.4–6.4%(worstcase)or1.1to2.9°(bestcase)by2100
(IPCC2007a:749).
Alterationstoprecipitationpatternsaremuchmoredifcult
topredict.Sometendenciesarerelativelyclear,forexample
Afurthertemperatureincreaseofbetween0.4to0.6°Cisex-
pectedtooccurbetween2005and2030.Thiswillbecaused
byexisting emissionsofgreenhouse gases, independentof
howemissionsdevelopin the nearfuture.Accordingtothe
WBGU (2007: 60), only adrasticevent suchas ameteorite
impact could alter this prognosis. The cont inents will heat
up more than the oceans; higher latitudes will also warm
upmoreasmeltingsnowandicecoverresultsinmoresolar
radiationbeingabsorbedinsteadofreected.
Inhabitantsofpolarareaswillbeparticularlyaffectedastem-
peraturestherewillriserapidly.Itismuchharderfornature
andhumanstocope witha rapid risethan a gradual,slow
increase.Theeffectswillalsobesevereonthepopulationin
areaswheretheclimateisalreadyhot.Heatwaveslikethat
in2003inEuropewillbethenormin2050.
that arid subtropical zones, the Medi terranean region and
southernAfricawillbecomedrier,whereasareasofhighrain-
fallinthe tropics andinhigher latitudes willbecome even
wetter(WBGU2007:62).However,itisnotclearhowrainfall
patterns will develop in the Sahel zone. The long-term de-
velopmentsinhurricaneoccurrencearealsoveryuncertain.
Thetotalriseinsealevelsisalso difculttopredict,mainly
becauseitdependslargelyonhowmuchinlandicemelts.If
noactionistaken,thesealevelisprojectedtorisebyupto
halfametrecomparedto1990levels,possiblyevenupto140
centimetres(Rahmstorf2007).Ifglobalwarmingisstabilised
at3°Ccomparedtothepre-industrialaverage,thesealevel
mayriseby3to5metresby2300(WBGU2007:38).
Looking at specicregional projections (e.g.inIPCC2007a:
ch.11,2007b:ch.9-16;WBGU2007:ch.7),itmustbenoted
that,atbest, changesin the weathercan be projected. Re-
gional or even national project ions of how vulnerable the
populationwillbeinthefaceofthesechangesarestillvery
uncertain atpresent and are sometimeseven dismissedas
“purespeculation”(FeinsteinIC2008:7).
III.1 GLOBAL PROJECTIONS: IMPACTS
Thefollowingdiagram(Fig.4)fromtheGermanAdvisoryCoun-
cilonGlobalChange(WBGU2007:176)showspossibleeffects
ofrisingglobaltemperatures.
An update of the IPCC’s Reasons for Concern from 2001
was published in March 2009 (Smith et al. 2009). These
climateconcerns includethreatened systems (island states,
tropicalglaciersetc),extremeweatherevents, theunequal
distributionofclimatechangeimpactsandmassivealterations
to the earth system (tipping elements). The update shows
thatecosystemsarereactingmorequickly,extremeweather
eventsarehappeningmorefrequentlyandaremoresevere
than anticipated. Greater risks and severe consequences
followingevenslighttemperaturerisesaretobeexpectedin
allaspects.TheinternationalScienticCongressonClimate
Change conrms that the IPCC’s worst case scenarios are
occurringandthatsocietiesareextremelyvulnerabletoeven
moderatechangesinclimate.
IV.1 CLIMATE CHANGE, POVERTY AND POVERTY
REDUCTION: HOW ARE THEY RELATED?
Wehavealreadyshown themostimportantlinkbetween cli-
matechangeandpovertyreduction:climatechangecausesand
exacerbates poverty, while also impeding development and
povertyreductionbymakingthefutureavailabilityofnatural
resourcesdoubtful.However,povertyandlackofdevelopment
alsoreducepeople’sabilitytoreacttoclimatechange;inother
works,povertyitself aggravates the consequencesofclimate
changeforthoseaffected.
Therearehoweverotherlinksbetweenclimatechange,pov-
erty reduc tion and development. Does povert y also play a
part in causing climate change? That would be the case
wherepovertycontributestonon-sustainablelanduseprac-
tices,producinghighgreenhousegasemissions.IntheAma-
zonregionof Brazil,for example, poor smallholderfarmers
areinvolvedinthedestructionoftherainforest,butonlyas
theweakestlinkinachainmainlyconsistingofmorepower-
fulactors–thetimber,beefandsojaindustries.Soeachcase
IV. Climate change and poverty
reduction
Food
Water
Ecosystems
Extreme weather conditions
Risk of rapid climate
change and large-scale
irreversible effects
Final temperature levels (compared to preindustrial levels
0° C 1° C 2° C 3° C 4° C 5° C
Disappearance of small
glaciers worldwide – potential
threat to water supply in
many areas
Considerable changes in water availability
Over 30% increase on flowing
away of surface water in the
Mediterranean region and in
southern Africa
Rising sea levels threaten large
cities such as London, Shanghai,
New York, Tokyo or Hong Kong
Coral reef ecosystems
extensively damaged;
damage finally irreversible
Possible start of breakdown
of parts of or all the Amazon
rain forest
Large proportion of ecosystems which cannot preserve their present form
Many species threatened
with extinction
Increasing intensity of storms, forest fires, flooding and heatwaves
Slight increase in hurricane
intensity causes twice as much
damage in dollars in the USA
Danger of weakening of natural carbon dioxide sinks and the Atlantic
thermohaline circulation; possible increase in release of natural methane
Start of irreversible melting
of Greenland icecap
Increased risk of abrupt, large-scale climate shifts
(e.g. collapse of Atlantic thermohaline circulation or
western Antarctic icesheet)
Severe effects
in the Sahel
zone
Increasing harvests in many
developed regions due to
CO2 fertilizer effect
Decline of harvests in many developed
regions despite CO2 fertilizer effect
Decreasing harvests in many developing regions
Rising number of people threatened
by hunger. Biggest increase in Africa
and West Asia
Severe decline of harvests in
whole regions
(e.g. up to one third of Africa)
mustbeconsideredcarefullyindeterminingwhetherpoverty
causesemissions.
Doespovertyreductionalsoreduceemissions?Ifso,itwould
betrueto saynotonlythat“climateprotection equalspov-
erty reduction”, in that reducing climate change would at
leastbenetthepoorofthefuture,butalsothat“povertyre-
ductionequalsclimateprotection”.However,reducinglarge-
scaleemissionsonanationallevel,whetherinindustrialised,
emerging or developing economies, is themore important
task.
Ispoverty reduction ratherthanclimateprotection thepri-
mary goal? By boosting and industrialising the economy,
development and poverty re duction themselves could con-
tribute to climate change. On the other hand, some argue
thatclimateprotectionwillimpedepovertyreductioninthat
avoidingemissionswillslowdown thegrowth necessaryto
overcomepoverty.
Sometimes a w in-win option bene ting all sides makes it
possible to implement sustainable development, reducing
bothpovertyandemissionsatthesametime.Oneexample
would be strategies to enable the poor to benet d irectly
fromeconomicprotsfromclimateprotection.Inthiscase,
climateprotectionandpoverty reductiongohandinhand,
preventingpovertyarisingfromclimatechangeandreduc-
ingexistingpoverty.Thepoor canoften reduce CO2emis-
sionsorbindtheminbiomass(e.g.byplantingtrees)inrela-
tivelysimpleways.Iftheyarethengivenaccesstomarkets
where they can sell these savings, they can actually earn
more,especiallyiftheyalreadygainanincomefromthese
activities(seebox2).
BOX 2: MI BOSQUE. CLIMATE PROTECTION =
POVERTY REDUCTIONG
The CAREproject Mi Bosque(myforest)in westernGua-
temalacombinescommunity-based adaptationtoclimate
changeimpactswithavoidanceoffurtherclimatechange.
Treeplantinghelps preventerosion,producesfruittobe
eatenand marketedand improvessoilquality.Reforesta-
tionalsocounteractsdeforestation,itselfthecauseofCO2
emissions,aswellasbindingadditionalCO2whichwould
otherwisereinforcethegreenhouseeffect.
Currently,treeplantingbindsover200tper hectare.Ad-
ditionalbenetsofthissustainablelanduseareimprove-
mentsinagriculturalproductivity,acorrespondingreduc-
tioninmigrationtoseekpaidworkandincomefromselling
thewood. Efforts are beingmade to measureandcertify
theCO2savingsmoreeffectivelyandtomarketthem.
TheprojectexempliestheconceptofReducingEmissions
fromDeforestationandDegradation(REDD).Deforestation
anddamagetoforestscauseupto25%oftotalanthropo-
genicgreenhousegases.Protectingforeststoavoidthese
emissionsisacost-effectiveclimatechangestrategy(Stern
2006).Atpresentitisstillunclearhowforestpreservation
canbe rewardednancially.Possible alternatives are rec-
ognition of CO2 avoidance on the emissions certicates
marketsorvoluntarynancingthroughfunds.
IV.2 ADAPTING TO THE IMPACTS OF CLIMATE
CHANGE
As the CARE projec t Mi Bosque (Box 2) shows, it is possible
tocombineefforts to avoid climate changewith adaptingto
itsimpacts.Foryears,thefocushasbeenonavoidance;more
recently,adaptationhasbeguntotakecentrestage.Thereare
severalreasonsforthis(Füssel/Klein2002):
The effec ts of greenhouse gases already in the atmos-
phere willbe feltin the future;in otherwords, climate
changeisunavoidable.Theglobalpopulationmustadapt
toitinanycase.Equally,thepositiveeffectsofsuccessful
emissions avoidance strategies will not be felt for dec-
ades.
Adaptationmeasuresat local,regionalornationallevel
can protec t the population directly from the ef fects of
climatechange.Avoidancemeasuresaremore depend-
entoninternationalcooperation.
Adaptation measures also protec t the population from
theeffects ofclimatic variations- short-term variations
which currently have damaging effects par ticularly on
thelivesofthepoor.
Avoidingemissionsisindisputablynecessary,butthiswillnot
besufcienttopreventnegativeimpactsofclimatechange.
The suggestions for combining poverty reduction and cli-
mateprotectiondescribedbelowfocusonadaptationatlo-
callevel,sustainedbythelocalcommunityandsupportedby
projectsandorganisationswhichtacklepoverty.
Adaptationtoclimatechangeisalreadyhappening,notjust
inorganisedform.Thismakesitessentialfororganizations
to take into account the ways in which people are already
adaptingtoenvironmentalchangesandlocalclimatechange
effects.The population may beforcedby their situation to
takeunsustainablemeasures.InToineke,somefamilieshave
increasedtheirsaltproductionby“saltboiling”.Thisusesup
alargeamountofwood,leadingtoover-useofthesurround-
ingforestwhich otherwiseprovideserosionprotectionand
asourceoffood.Thistypeofmaladaptationcanbeavoided
bysuitablesupport.Ontheotherhand,thelocalpopulation
usuallyknowtheirlocalenvironmentwell.Measurestosup-
port them in theiradaptation strategiesshouldbe compat-
iblewiththisknowledgeandcangainfromit.
IV.3 SUPPORTING RESILIENCE
People must be viewed as ac tive agents in connection with
climatechange, for the reasonsshownabove.Thisviewpoint
isthebasisofthelivelihoodconcept,whichiswidespreadin
developmentresearchandinorganizationswhichworktore-
ducepoverty.
It covers the strategies people use to ensure their surv ival
and full their needsbased on their capabilities and avail-
ableresources.Someofthesestrategiesinvolvemaintaining
accesstocertainresources,includingsocialcapital(e.g.inte-
gration in thecommunity),human capital(e.g.knowledge,
health),physicalcapital (housing)andnancial capital(sav-
ings).Themost importantfactor isnaturalcapital – fruitful
land,regularrainfallandotherecosystemservices.
Thelivelihoodsperspectiveincludesthewaypeople’sability
toactivelyensuretheirsurvivalisaffectedbychangestothe
availableresources.Italsocoversthreeotheraspectsofpov-
erty.Therstoftheseispeople’svulnerabilitytotheimpacts
ofclimatechangeasmentionedabove.Vulnerabilitymeans
theextent to which people’sopportunities tosustain their
livelihoodaredamagedbythese impacts.In this case, pov-
ertyreductionmeansovercomingthisvulnerability.
Thesecondaspectisresilience.Apopulation’svulnerability
dependson how itcan react whenclimatechange impacts
affectitsmeansoflivelihoodintheformofsporadicshocks
(e.g.astorm)orlong-termpressuressuchasdwindlingwater
resources.Resilienceincludesrst,solvingtheproblemand
second, adapting to the new conditions (Handmer/Dovers
1996).If people can onlyreact byabsorbing thechanges –
e.g.eatingevenlessifharvests fail – thiswill notdecrease
theirvulnerability.Inthelongterm,therefore,absorbingor
copingstrategiesarenotsustainable(Davies1993).Adapta-
tiontothechangedconditions,however,canreducevulner-
ability.Onthe other hand, reducing vulnerabilitycan open
upnewopportunitiesforapopulationtoadaptintheirown
waystothenewconditions(Kelly/Adger2000).Forexample,
ifwateraccessisensuredandstoragefacilitiesimprovedby
external suppor t, it mayb ecome possible to increase food
production, which ac ts as a buffer. So resilience draws on
availablelocalresources, but alsoonaccesstoexternal aid
(IISD2003:6).
Strengtheningresilienceiscentraltoanapproachtopoverty
reduction. Measures may be specically tailored to a par-
ticular threat: if climate change reduces rainfall, drought-
resistanttypesofgraincanbeprovidedforsmallholders. A
prerequisiteforthisisdeniteknowledgeofboththethreat
itselfandtheefcacyofthemeasuresagainstit. Thisisnot
thecaseifthenewlyintroducedgrainsaredroughtresistant,
but growing them is incompatible w ith the farmers’ other
activities.
However,strengtheningthepopulationgenerallywillcontin-
uetobeveryimportant.Becauseitissohardtopredictthe
consequencesofclimatechangeandhoweffectivestrength-
eningresilienceina particular aspectwillbe,itisessential
tomaintain people’sgeneral capacity toact and react.This
includestheir health as a prerequisiteaswell as incometo
enableaccesstoadditionalresourcesandsocialnetworksto
compensateforunforeseenvulnerability(IISD2003:7).
Finally, security must be mentioned. Poverty reduction as
practised by CARE and other organizations involves more
thansimplyensuring thatpeoplehaveadequate and effec-
tive access to resources which provide theirlivelihood and
fulltheirneeds.Itisalsonecessarytoensurethatthisaccess
isguaranteedforthelongterm.However,climatechangeim-
pactsunderminetheseefforts.Sothestrategiesandactivities
ofthepeoplethemselves,aswellasthoseaimedatpoverty
reduction, must beclimate secure:they muststillfunction
eveniftheeffectsofclimatechangearemoresevereordif-
ferentfromthoseanticipated.Theyshouldalsobenoregret
measures,usefulevenwithoutclimatechange.
IV.4 CRITERIA FOR SUCCESSFUL
ADAPTATION MEASURES
A2007paperanalysed130casestudiesofadaptationandde-
velopmentpolicyinreactiontoclimatechange.Themeasures
wereplacedonaspectrum(McGrayetal.2007:18,cf.Fig.5).
At one end are activities which concentrate on structural
causes of poverty and v ulnerability in general (left). At the
other end are those related toclimate change itself (right).
Inbetweenaremeasureswhichstrengthenpeople’scapacity
toreacttoclimatechangeimpactsandthosewhichintegrate
foreseeable climate risks into economic, polit ical and other
decision-makingprocesses.
Theaimof this arrangementisnotso much totmeasures
correctlyinto one category or another;the spectrumshows
variousaspectsandapproaches which ideally shouldbeim-
plementedtogether.Ifalltheseaspectsaretakenintoaccount
inasingle project,it may belessfocussed on particularas-
pects.However,thiscanbeanadvantageoverconcentrating
tooexclusivelyonasingleaspect.Aholisticapproachismore
effectivethan precision, since local climate change impacts
thepopulationindifferentwaysatthesametime.
Effectivenessisoneofseveralcriteriawhichadaptationmeas-
ures, in the sense of livelihood- oriented poverty reduc tion,
aimtofull.Asurveyevaluatingpreviousformsofadaptation
(IDS2008:27f.)proposesvecriteria,asfollows:
Thesecriteriaarenotonlyimportantattheplanning stage.
The local population’s own ways of adapting to climate
change impac ts, and the effe ct these have at a soc ial level
(e.g.increased energy requirementsduetoincreaseduseof
airconditioning),canbetestedagainstthem.Nationaladap-
tationpoliciesshouldalsotakethemintoaccount.
1 2 34
Providingwomen
withcrossbredgoatsand
instructioningraze-freefeed-
ing(KaramojaAgropastoral
DevelopmentProgramme)
Diversication
oflivelihoodstrategiesin
areasvulnerabletoooding
(SouthSouthNorth)
Vaccinationprogram
toeradicatediseasesinlow-
incomeareas(CubanMinistry
ofHealth)
Participatoryrefor-
estationinRiodeJaneiro’s
hillsidefavelastocombat
ood-inducedlandslides(City
ofRiodeJaneiro)
Reinstating
pastoralnetworkstofoster
appropriaterangelandman-
agementpracticesinarid
regions(NationalUniversityof
Mongolia)
Revivingtradi-
tionalenclosurestoencour-
agevegetationregeneration
andreducelanddegradation
(MinistryofNaturalResources
andTourism,Tanzania)
Monitoringsalini-
zationofdrinkingwaterand
drillingnewwellstoreplace
thosethatarenolongerus-
able(SouthSouthNorth)
Teachingfarmerstocol-
lectclimatedataandintegrate
itintotheirplantingdecisions
(GovernmentofMali/Swiss
Agenc yforDevelopmentand
Cooperation)
Usingnation-
allystandardizedriskassess-
mentprocedurestodevelopa
communityadaptionplanof
action(localgovernment)
Managingcoral
reefsinresponsetowide-
spreadcoralbleaching(WWF)
Reducingther iskof
glaciallakeoutburstoods
fromTshoRolpaLake(Govern-
mentofNepal)
IV.5 MEASURES
CARE differentiates between measures for (1) support, (2)
protectionand(3)livelihoodprovision,accordingtourgency.
The third type compr ises emergency aid designed to keep
peoplealiveinanacutesituation.
Longer-termadaptation to climate change involvesthe rst
twocategories.Thefollowingtableshowsthesedistinctions;
measurestoensurefood security havebeen supplemented
toincludegeneraladaptationtoclimatechange(CARE1998,
Cordetal.2008,IDS2008).
CRITERION DESCRIPTION
EFFECTIVE-
NESS
FLEXIBILITY
FAIRNESS
EFFICIENCY
SUSTAINA-
BILITY
Thepopulation’svulnerabilityisreallyreduced,theirresiliencestrengthened,theiraccesstoresources
secured.Effectivenessalsodependsonmeasuresbeingcompatiblewiththepopulation’scircumstances,
strategies and culture. Therefore it is essential that people participate in the development and
implementationofmeasures.Themeasuresshouldnotconictwitheachother.
Because thefuture isso unpredictable, measures shouldbe exible enough to havepositiveeffects
whateverclimatechangebrings(noregretmeasures).Theyshouldalsoinvolvelowlevelsofsunkcosts
(i.e.costswhichcannotberecovered).
Povertyreductionmeasuresaiddifferentgroupstovaryingextents;theyshouldnotreinforceexisting
inequalities–eventhoughitissometimeseasiertostrengthenlessvulnerablegroups.Povertyreduction
effortsshould be distributed fairlyanyway, for ethicalreasons – butalso forstrategic reasons,since
otherwisethemeasureswilllacksupportandlong-termeffectswillnotbeachieved.
Maladaptati on also occurs when the most cost-e ffective measures are not used and/or the costs of
adaptation are higherthan itsusefulness. However,itisdifcult to quantifyusefulness: how muchis
itworthtoenablepeopletomaintaintheirlivelihoods?Thisperspectiveisknownastheeconomicsof
adaptation.
Beforemeasuresareadopted,theirlong-termeffectsshouldbeconsidered:whethertheywillbestable
andare efcientinthelongterm.Sustainability also requiresthat measureshavenonegativeeffects
onlocalecosystems,socialcohesionetc.Themainfactoristhatmeasuresshouldbesormlyrootedin
people’severydaylivesthattheyaresustainedoncetheaidorganizationhaswithdrawnitssupport.
PROTECTION AND MAINTENANCE OF LIVELIHOODS SUPPORTING LIVELIHOODS
• General:protection/restorationofsecureaccessto
resourcesormeansofproduction.
• Basicraisingofawareness:whatishappeningdueto
climatechangeandhowdoesitaffectthepopulation?
Enablelocalstoparticipateandcombinetheir
knowledgeabouteffectswithexternalknowledge.
• Ensurethatdealingwithclimatechangebecomesthe
newnorm,sopeopleareawareofitandadapttheir
livelihoodstrategiesontheirowninitiative.
• Applyaidpaymentstoensurepeopledonotselltheir
meansofproductioninacrisis.
• Setupearlywarningsystemsandtrackclimate
change;makeriskprognosisandinformationabout
possibleimpactsavailable(radioetc.).
• Emergencyplanstoenablequick,effectivereactionto
unexpectedevents.
• Managementofremainingrisks,e.g.intheformof
microinsurancesagainstweatherevents.
• Materialinfrastructuretodefendagainstimmediate
effectsofclimatechange(e.g.dykes,building
regulations/technologies,irrigationsystems,water
reservoirsinaridareas).
• Improvementofsoil,forestandwatermanagement
e.g.tomaintainagriculture(e.g.treeplantingto
protectagainsterosion).
• Healthandothermeasurestoensurethatpeopleare
notsoweakenedbydiseaseorundernourishmentthat
theylosethecapacitytoactandreact.
• Institutionalizingand„automating“localprotective
measures:whoisresponsibleforwhat,ensuring
communicationbetweenthesepeopleandinstitutions
etc.
• Relatedtothis:traininglocalindividualsresponsible
fortheseparticularroles.
• Stabilizingharvestsbydiversifyingcropsandadapting
themtotheprojectedclimateconditions.
• Developingalternativeincome- generatingactivities,
esp.thoselessdependentonthenaturalenvironment
(e.g.notagricultural)orlesslikelytobeaffectedby
climatechange.
• Providingconditionsandincentivestoadoptthese
alternativestrategies.
• Ensuringaccesstonewtechnologies,graintypesand
otherinnovationsasprerequisitefornewpractices.
• Strengtheningstrategieswhichhaveprovedsustainable,
notmaladaptationse.g.seasonaljobmigration.
• Improvingstoragecapacitiesforreservesincaseof
failedharvests.
• Improvedmanagementofcommunityassetswhich
areaffectedbyclimatechangebutcannoteasilybe
protectedbyindividualowners.
• Educationtoimprovepeople’scapacitytoactandreact.
• Improvingaccesstopoliticaldecision-making,so
communityadaptationisdesignedtomeetactualneeds.
• Empowermente.g.ofwomentoenablethemtotake
morepartindecisionmaking.
V. Poverty reduction and strate-
gies to secure livelihoods: case
studies and lessons learned
AsTable2shows,theinstrumentsofthelivelihoodapproach
topovertyreductioncanbeappliedtopromoteadaptation
toclimatechangeimpacts.Itisnotnecessarytoinventnew
formsofpovertyreduction;however,existingstrategiesmust
bemadeclimatesecure.Ifthiscanbeachieved,theseinstru-
mentsareparticularlysuitable,becausetheystrengthenthe
self-preservationcapacityofpoorpopulations.Thiscapacity
isendangered by climate change, but is also an important
partofthesolution.Decentralized,community-basedadap-
tationcannotonlycoveractualneeds,butalsomakeuseof
localadaptationcapacities.
Wenow describesome cases of reactiontoclimatechange
impacts. People oftenreactontheir own initiative.Climate
variationsarenotanewphenomenontomostofthem,but
theunusualextentandspeedofcurrentclimatechangechal-
lengetheiradaptationcapacity.However,adaptationistak-
ingplace,sopovertyreductioneffortsmustsupportthisor,
ifnecessary,offeralternatives.Hereweshowinmoredetail
how these reactions and adaptations combat poverty and
whatcan be learnedfrom this. We relatethis tothe crite-
riamentionedabove–effectiveness, exibility,fairness, ef-
ciency andsustainability.The casestudy on thevillage of
ToinekeinWestTimor,Indonesia,wascarriedoutespecially
forthispaperbyZEFincooperationwithCARE.
V.1 SMALLHOLDER FARMERS IN TANZANIA: SPECIAL-
ISING AND REDUCING DEPENDENCE ON AGRICULTURE
The livelihood approach to poverty reduction emphasises
diversicationofeconomicactivities(Ellis1998).Thisreduc-
esthepopulation’svulnerability,inthattheycanfallbackon
otherincomesources.
Thedisadvantageisthattheymustmaintainbothactivities
simultaneouslyandso can investlesseffortineach.Some-
times it seems more advantageous to specialise. This was
observedamongsmallholderfarmersinKenyaandTanzania
(Eriksen/Brown/Kelly2005).
CARE carried out a country-wide study of climate change
impacts and adaptat ion in Tanzania (Ehrhar t/Twena 200 6).
Tanzaniais the l argest, most densely populated country in
EastAfrica,but also the poorest. Theprimary threat is the
anticipated increase in frequency and severity of extreme
weatherevents.About80%ofthepopulationisdependent
onrain-fedsubsistenceagriculturewhichissusceptibletocli-
matevariations.Undernourishmentiswidespreadand food
aidisoftennecessary.
The study investigated smallholder farmers in the Saweni
district in northeast Tanzania,to see howthey coped with
droughtand maintainedfoodsecurity(Eriksen/Brown/Kelly
2005).Harvestsinthisareaoftenfailduetodrought.Water,
grazingland andrewood are inshort supply.Smallholder
farmerscultivateafairlywiderangeofcrops,themostpopu-
larbeingmaize.Animalhusbandryhasdiminisheddrastically
in recent decades. Impor ts of additional produce from the
surroundingareahavebeenincreasingsincethelate1970s.
Non-agricultural income is becoming more important, al-
though most households continue to practise agriculture.
Youngpeopleseekpaidwork;youngmenoftenmigrate.
Inthepast,fruitandtubersweregatheredandanimalsand
poultrysoldduringperiodsofdrought.Othercopingmecha-
nisms included occasional work, family support and emer-
gencyaid.Thelocalpeopledifferentiatebetweenmainand
secondary strategies.The formerare regular activities pro-
ducingareliableincome overlongerperiods;these replace
agriculture. Small businesses (e.g. shops) or crafts such as
carpetweavingarecommonstrategies.Secondarystrategies
entail using individual opportunities, e.g.making and sell-
ingrope,whenthemainstrategy isnot possible.Themain
strategiesareintensive,specialisedandbringacashincome.
Moneyhasbecomeimportant,aboveallforpurchasingad-
ditionalfoodandhealthservices.
Theauthorsidentiedincreasingmonetarizationanddwin-
dlingsignicanceoflocalproduceasreasonswhylocalpeo-
plespecialiseinafewactivitiestocopewithdroughts.This
includesthepossibilitythatseveralpeopleinonehousehold
– not the whole household – concentrate on one activity.
Although agriculture is still the preferred activity, people
continue to practise the specialised, cash- oriented activit y
sotheydonotlosetouchwithitandcancontinueitduring
phasesofdrought(Eriksen/Brown/Kelly2005).
Thisresponsetoclimatechange impactshasbeen initiated
bythelocalpopulation.Accesstopreferredmethodsofgain-
ingaspecialised,cash-bringinglivelihoodisunequal;e.g.it
iseasierforthebetterqualied.Thisformofcopingiseffec-
tive because the popul ation is more dependent on money
anywaythanin thepast.Money mayalsomakethemmore
exible,becauseitcanbeusedforavarietyofpurposes,un-
likeagriculturalproduce.
However,coping isnot thesame asadaptation.Constantly
copingwithenvironmentalstressandpressureonlivelihood
activitiesisnotsustainableanddoesnotreducethepopula-
tion’sstructuralvulnerability.Itmaybethatthecopingstrat-
egiesfordroughtobservedinTanzaniaarenot“maladapta-
tions”.Howeverbecauseoflowgrowth,localjobmarketscan
onlyabsorbalimitedamount of non-agricultural activities.
Thegreaterthenumberofpeopleconcentratingonthiscop-
ing strategy, the less effective it is, because the potential
income declines. People who spec ialise in non-agr icultural
activ ity also lose the food secur ity which subsistence agri-
culturecanprovide despiteclimatechangeimpacts. Acash
income may fail or lose its purchasing power, for example
whenglobal food prices rise.The strategyofgaining inde-
pendencefromagricultureandnaturalresourcesinresponse
toclimatechangeisrisky;othereconomicsectorswillalsobe
affectedbyclimatechange,sothepopulation’svulnerability
mayonlybepostponed,notreduced.
V.2 MICROINSURANCE IN INDIA:
THE POOR PROTECT THEMSELVES AGAINST RISKS
Micronancialserviceshavebeenusedformanyyears now
tosupportpeopleinbreakingoutofthepovertytrap.Micro-
loans,forexample,enablethebeneciariestosetupsmall
businesses.
Recently, microinsurance has also been initiated, to insure
peoplewhohavefewpossessionsandcanonlyaffordsmall
premiums. This provides a form of livelihood protection:
if sudden or long-term events - storms, drought – destroy
meansofproduction,thethreatenedincomecanbesecured
byinsurancepayments.
Insurances,especiallyindex-basedinsurances,alsohavethe
advantagethat they rewardrisk provision.Payment is trig-
geredbyaphysicalfactor,e.g.acertainlevelofrainfall,not
bytheactualdamageafarmersuffers.Hecanreducetherisk
bycultivatingmorerobustcrops(Arnold2008).Inthisway,
theinsurance isalso an incentiveto make one’slivelihood
climatesecure.
Riskreductiongivesthepoorscopetoadapttoclimatechange
impacts (Lemos/Tompkins 2008). Because microinsurance
secures existing livelihoods and encourage improvements,
theyare a good instrumenttoprotect peoplefromslipping
(back)intoorenablethemtoriseoutofpoverty.Thepoor,
however,often cannot affordthisinsurance(Reiner 2008).
Onlyasmallnumbers of insurances reach the poor(Arnold
2008,Pierro/Desai2008).Thiscouldbecounteredbyassist-
ance in paying premiums – this could be taken on by the
BOX 3: MICROINSURANCES AND
WEATHER-RELATED DISASTERS:
CARE INDIA AND BAJAJ ALLIANCE
CAREIndiaandtheIndianinsurancecompanyBajajAlliance
together provide microinsurance for about 92,000 peo-
pleinthe coastalregionsofthe Indianstate TamilNadu.
AccordingtoRNMohanty,headofCAREIndiaMicroinsur-
ance,themainchallengetheconceptentailsisconvincing
peopletoincluderiskprovision in their livelihoodstrate-
giesandtodevelopacultureofmakingprovisionforthe
future:“Almost90%ofourcustomersarerst-timeinsur-
ancetakers.[…]The hardesttaskistoteachandtrain the
people.”
Tosucceed,thesystemmustgainpeople’strust,soitisof
primeimportancetoregulateclaimssatisfactorily.Thesys-
temwasputtothetestinNovember2008,whentropical
storm Nishahit theTamilNadu coast, making thousands
homeless. Project workers went at once to the affected
areastoassessthedamageandmakepaymentsasquickly
aspossible.Thatshowedpeoplehowusefulitwastoinvest
ininsurance,leadingtogrowinginterest.
countries primarily responsible for anthropogenic climate
change. To suit these users, insurance must be straightfor-
wardand easy to understand; it shouldalso bepossible to
payexiblepremiums,sinceotherwisepeoplewithirregular
incomeswouldsoondropoutofthesystem.
Insurancesare not theonlywayinwhichthepoorcandeal
withclimate change risks, such aslossescaused by natural
disasters. Financial and social capital (savings, knowledge
andtraining,familysupport)arealsoimportantcomponents
oflivelihoodresources.However,thesecanbeoverstretched
whenonedisasterfollowsanothertooquickly.Inthatcase,
peoplecanbeforcedtosellpossessions,takeoutloansand
sofallbackintopoverty(Arnold2008).Naturaldisastersalso
tend to affect all member s of a community,s o in order to
function,insurancesmustspreadtherisk;otherwise,thepre-
miumswillbecometooexpensiveortheinsurerwillnotbe
abletoaffordtomakepayment.
Climate change is also making it more difcult to sustain
thissystem.Potentialdamagefromextremeweatherevents
isbecoming morefrequentandextensive,sosomeinsurers
arewithdrawingfromthemarket.Thishasalreadybeenob-
servedincoastalareas.Thesystemwillonlybe worthwhile
inthelongterm,onascalelargeenoughtospreadtherisk.
Reinsurance must also be built up and investments in im-
provedinfrastructure are necessary, to reduce the demand
forinsurance.
Finally,newtypesofinsurancetailoredtolocalneedsarebe-
ingtested,tolimitinsurers’costs.BajajAllianceIndia’shealth
insuranceisoneexample.WorkingwithCARE,acooperative
system has been developed in which the local community
itself administers the insurance, retaining 67 % of the pre-
miums.Thisissufcienttocovermostclaims.BajajAlliance
onlytakesoverwhenacaseexceedsthecommunity’scapac-
ity.Afterayear,it appearsthat80 to90 %ofcasescanbe
coveredinthecommunity(Alliance2009).
VI. Case study West Timor,
Indonesia
The following example of the village of Toineke in West
Timor,Indonesia,showsclearlyhowclimatechangeimpacts
people’ssurvivalstrategiesandhowtheydealwiththesitu-
ation–moreorlesssuccessfully.
VI.1 IMPACTS OF CLIMATE CHANGE IN
(EAST) INDONESIA
Inpart1,wereferredtotheuncertaintyofmakingconcretepre-
dictionsabouttheeffectsofclimatechangeonlocalweather
conditions.However,regionalprojectionsdoexist(IPCC2007a:
ch.11,2007b:ch.9-16;WBGU2007:ch.7).
Warmingin SoutheastAsia will beat 2.5°C, similar to the
globalaverage.Rainfallwillincreasebyabout7%,butwith
concentrationsinparticularregions(Boer,Faqih2004).Indo-
nesiawill probably be badlyaffected by risingsealevels:a
riseofonemetrewouldleadtothelossof2,000islandsand
400,000 hectares ofland (IPCC2007b:485).Local develop-
mentscouldbeverydifferentfromtheseregionaltrends,due
tothe complex geographyof theregion;temperaturesmay
risemuchmoreininlandareas.EastIndonesiainparticular
isaffected by the El Nino southern oscillation (ENSO)phe-
nomenon,wherereducedrainfallleadstolongerdryseasons
and droughts. This happened, for example, in 1982/1983,
1991, 1994 and 1997/1998 (Hulme/Sheard 1999). Where
rainfallincreases, thetrendtosudden,heavyrainfallisalso
strengthened,resultinginerosionandooding(IPCC2007a:
886).Littleisknownabout the development of the tropical
stormswhichoccurespeciallyinEastIndonesia,buttheyare
expectedtoincreaseinintensity(byabout10–20%ifthe
seasurfacetemperaturerisesbetween2to4°C,IPCC2007b:
479),whiletheirfrequencymayactuallydecrease.Indonesia,
thethirdlargestglobalemitterofgreenhousegases,isusu-
allyperceivedasdamagingtheclimate(Weck2007,J.Müller
2008).ThiscasestudyshowsthatinIndonesia,asintherest
oftheworld,itisthepoorwhousuallyprotleastfromthe
overexploitationofthenatural environmentbutwhosuffer
mostfromitseffects.
VI.2 TOINEKE, WEST TIMOR: ECONOMY AND SOCIETY
ToinekeisavillagelocatedatthemouthofRiverNoemukein
theIndianOcean.Itcomprises680households(approx.3,000
inhabitants),twoprimaryschools,vechurchesandfourlocal
healthcentres.
GENERAL DATA ON WEST TIMOR, INDONESIA
NusaTenggaraTimur
Kupang
Timor
14,394.90km²
1.7m.
AtoinMeto,Tetum,Bunak,Kemak
Indonesian,UabMeto,Helong,Rotinese,
Tetum
55%Catholic,34%Protestant,8%Muslim;
ancestorworshipandbeliefinspiritsarewidespread
Agriculture(40%GNP;68,5%of
workingpop.),trade(15,9%;6,5%),construction(7%;
2,4%),transportandcommunications(6,2%;4%),
manufacturingindustry(1,7%,8,2%),mining(1,3%;
0,8%),electricity,gas(0,4%;0,1%)
Westmonsoon/rainyseason(Nov.oApril),
eastmonsoon/Dryseason(MaytoOct).
The population has lived from subsistence farming for
generations, making them very dependent on the natural
environment. They also have vegetables gardens and
orchards,keepanimals,trade on a smallscaleandpractise
home industries. Very few families sh in the nearby sea.
Apart from agricultural and animal produce, goods are
manufactured for sale, including woven goods, palm leaf
containers,artsandcrafts,coconutoilandsweets.Carpentry
products and construction material from the putak palm,
rewood, coconut seedlings, betel nuts and cigarettes are
alsotraded.Afewfamiliesusetheelectricitysupplyavailable
atnight toproduceicecream.Otherssellsalt,producedby
boiling sea water for hours. This method of “boiling salt”
entailschoppingdownlargenumbersoftreesforrewood.
Originally thesoil wasvery fertile,attracting acontinually
increasingpopulation sincethe 1960s. In 1960, there were
78householdsinthevillage;within10years,thegurehad
risen to 180. As a result,Toineke’spopulation is amixture
ofethnicgroupsfromdifferentplaces.Thegreatmajorityof
thevillagers live in smallone tothreeroom houses,made
ofwood (frame and roof timbers),dried putakpalm twigs
(walls) and palm stalks (roong). The oor is usually of
tampedearth.Cookingtakesplaceonthreestonesinthere
ontheoor.Moremodernwooden,stoneorconcretehouses
aretheexception.
VI.3 PERCEPTIBLE LOCAL IMPACTS OF
CLIMATE CHANGE
Untilthe1980s,the WestTimorese climate was typiedbya
relativelyreliable divisionintoa dryseason from May toOc-
toberandarainyseasonfromNovembertoApril.Thestartof
therainyseasonwasmarkedbyseveraldaysofconstantrain.
Farmersstartedplanting aftertwoorthreedays of continual
rain.
However,sincetheearly1990s,Toineke’spopulationhasob-
served massive local alteratio nsin th e climate. Since then,
thedryseasonhasbeengetting longer and the villagesuf-
feredseveralprolongeddroughts,lastingthewholeyear(in
1992,1994,1995,1997,1998,2006,2007and2008).Fourof
thesevenvillagewellsdriedoutbetween1992and1995,so
fetchingwater involved farmore effort. The extratime re-
quiredhadnegativeeffectsonhomeindustries,watershort-
ages reduced harvests in vegetable and fruit gardens and
damaged the health of people and animals. Field har vests
werealsobadlyaffected.Peoplesoldtheirsmalleranimals,
oodingthemarketandresultinginfallingprices.Thesitu-
ationforagriculturerecoveredsomewhatbetween1997and
2006, w ith a pattern of two years of extended dry season
followedbyayearwithagoodrainyseason.
Onthe eveningof16May2000,a rapidlyrisingoodinun-
datedthevillage.Thehousesatgroundlevelwerestanding
inwatercontainingloamandsomesaltysedimentsforupto
two months. The ooddestroyed elds,vegetable gardens
and home industries, damaged houses and washed away
possessions; many animals drowned. The standing water
broughtmosquitoesanddiseases,inparticular malariaand
diarrhoealdiseases,butalsodenguefever.Inpartsofthevil-
lage,wellsandsoilwerecontaminatedwithsalt.
Thevillagehadpreviouslyonlyexperiencedoodingin1972
and1990;villagersstatedthattheearlieroodswerenothing
incomparisonwiththatof2000.Sincethen,thevillagehas
beeninundatedseveraltimeseveryyearbetweenDecember
andMay,thoughnotonthescaleofthe2000ood.Thewa-
terandsedimentremainforuptothreeweeksinsomeparts
ofthevillage.Thevillagersdifferentiatebetweenwaterand
sedimentfromthemountain and from the riverintheiref-
fectsfor agriculture.Mountainwaterisconsideredpositive
andfruitful,whereasriverwaterismixedwithseawaterand
damagesagriculture.
Comparedtothe dryperiodsinthe1990s,therainyseason
hasbeenmorereliablesince2000.However,theprecisetim-
ing and duration are not reliable. In some years, the rain
CASE STUDY: IBU YANSE TON
Since2000,thefamilyhasgotusedtotheoodsbutdoes
notat temptanypreventivemeasuresorp ursueanylonger-
termadaptivestrategy.Instead,IbuYanseleavesherhouse
whenthewaterrisesandstayswithrelativeswholiveon
higherground.Whenthewaterlevelfallsandherhouseis
nolongerooded,shereturnsandgetsridofthesediment
andanywaterleft.IbuYanseexplainsthiswiththelackof
nancial andhumancapital.“It’salreadyhardenoughto
get food eachday. How could we plan tobuilda secure
houseaswell?”Sheusedtokeepsmallanimals(particu-
larly chickens).“Now the oods makeit moredifcult to
earnalittlemoremoney.”Whenthewaterandsediment
destroytheharvestyetagain,shegatherswildcassavaand
tamarindseedsintheforestasfoodsubstitutes.However,
thatisalsobecomingmoredifcult.Thereislessandless
wildcassavaintheforest,shereports.
Ibu Yanse Ton (age unknown, 2 years primary school,
widowed,4adultchildren)liveswithherson,hiswifeand
twochildreninabadlydamagedhousebuildoflocalma-
terialsatgroundlevel,intheregularlyoodedpartofthe
village. In2000, the ood washedaway all their posses-
sions,theiranimalsweredrownedandpartsofthehouse
collapsed . Her family fell ill wi th malaria and diarr hoea,
necessitatingaweekinhospital.
startsinOctoberbutthenstops.PakMartinusTaneosays,“In
thepast,whenthe rainy season started,it didn’t stop rain-
ing.Nowitrains,weplantoureldsandthentherainstops,
sometimesuntilJanuary orFebruary”.Thesubsequentheat
kills the newly sown plant s, so that when the rains return
inDecember or January,newseedshaveto be boughtand
planted.TheBircheffect,theincreasedrelease of nutrients
toplantsaftertherstrain,whichisresponsiblefor30%of
theharvest,islost(Wood1995:76).Inotheryears,therain
doesnotstartuntilthesecondweekinDecemberorinJanu-
ary and thencontinues untilMay.Since2005, thevillagers
haveobservedthattherainyseasonisgettinglongeragain,
sometimeslastingfromOctobertoMay.However,duringthis
periodtherainfallsinshort,abruptphases,followedbydays
withoutrain.Thisisoftencombinedwithooding.Inthelast
threeyears,incontrast,thedryseasonswereextremelylong
andhot, like the droughtsin the 1990s.However,it rained
occasionally,whichisunusualforthedryseason.
VI.4 COPING AND ADAPTATION STRATEGIES
The increasing irregularity of the weather endangers agri-
cultureand solivelihoodsecurity.However,thelocalsdonot
seethesealterationsinthe context ofglobalclimatechange.
Theyperceivethemasconcrete changes inthelocalenviron-
mentandweatheranddiscussthem in these terms.Twofre-
quently heard sentences are, “alam sudah berubah” (nature
haschanged)and“musimsudahberubah”(theseasonshave
changed).Some villagers also see the changes as God’sway
ofchallengingthem to ndwaystolivein future withthese
changes.
Sofarthevillagershaveundertakenavarietyofcollectiveef-
fortstostemtheooding,butwithverylittlesuccess.There
is no long-term adaptation strategy for the whole vill age,
thoughpossibilitiesarebeingdiscussedwiththesupportof
thirdparties.
At an individual level, a number of successful short-term
copingstrategieshavebeendeveloped,measurestopredict
changes in the weather and some longer-term adaptation
strategies.Amongtheshort-termmeasures,thepopulation
falls back on tradit ional ways of securing food in times of
hunger. However, because this has been more frequently
necessaryinrecentyears,theresourcesusedforthisstrategy
arebeingoverstretched.
Preventive measures to avert the
impacts of climate change
The villagers haveattempted toundertakesome measures
to inuence their surroundings and the vill age location so
thattheyarelessaffectedbycurrentclimatechangeimpacts
–suchastoprotectthe villagefromooding.Forexample,
inJuly2000thevillageelders attempted toarrangeforthe
villagetoberelocated.However,thisfailedbecauseitwould
havebeennecessarytonegotiatewiththeministryforagri-
CASE STUDY: PAK AUGUSTINUS LEBISA UND
IBU NAEMA BANOET
Pak Augustinus Lebisa and
Ibu Naema Banoet (age
unknown,married,no chil-
dren) live in a small, one-
roomedhousemadeoflocal
materials, furnished with
a wooden bench, wooden
bed andopen cooking re.
Theystoremaizeunderthe
roof in the traditional way.
They originally come from
Kollbana and Nununamat, but set up home in Toineke.
Unfortunatelytheyhadnochildren.Today,IbuNaema(no
schooling)has been blind for two years andPakAugusti-
nus(threeyearsprimaryschool)ishardofhearing.Distant
relativescultivate theirone hectare of landon the hillin
exchangefor 20 kilogrammesofmaizeayear.Thisisnot
enoughtoliveon,butPakAugustinusandIbuNaemacan
nolongercultivatethelandthemselves.Instead,theykeep
animals.Theirvecowsdrownedin2000.Nowadaysthey
keepapigandtwohens.
Ibu Naemasays: “When we wereyoung, we grew maize
anditourished.Nowadaysit’stoohotanddry,followed
by oods.” When Pak Augustinus senses that the rains
arecoming, he buildsa stable onstilts. Heand his wife,
however,waituntilthewatercomesandthenclimbonto
their roof. The sediment the water brings is often over
theirknees,soIbuNaemacooksontherooffordays.They
wouldliketobuildahouseonstilts,buttheyhaveneither
thematerialsnorthestrength.
PakAugustinusandIbuNaemahavenoaccesstostatesys-
temsofsocialsecurity,nordotheyhavefamilytoprovide
forthem.Theiropportunitiesofadjustingtothechanged
conditionsareminimal.PakAugustinusexplains,“Weare
old.Wehavenomoney.Wearewaitingtodie.“
cultureandforestry in Jakarta, which is responsibleforthe
land they hoped touse. Thecurrent village head explains:
“Forone thing, wehaven’tenoughmoney toytoJakarta
andfor another,we are littlepeople without much educa-
tion. We can’t meet with rich, intelligent people.“ In the
sameyear,thedistrictgovernmentbegantodredgetheriver
annually.Howeverthesedimentllsuptheriverbedagain,
sothisdoesnotpreventooding.
In2004,thevillagebuilta5,600metrelongcanalabovethe
village,topreventthesediments and waterbroughtbythe
oodsfromreachingthevillage.Theyreceivedfundingfrom
anIndonesianNGOforthisproject.Theone-meterdeepbar-
rierwasbuiltbyhand–butoneoodwassufcienttollit
in.Thepresentvillageheadconsidersthatitwasbuiltinthe
wrongdirection,sothewatercollectedinitinsteadofow-
ingawaytowardstheriver.
In2006/2007,thevillagersplantedabout20,000treesatthe
foot of the mountain behind the vill age, where the forest
hadbeengraduallyclearedinthepreviousdecades.Thenext
dryperiodkilledhalfthetrees.Sincethen,thevillageelders
havenotplannedtoplantanymoretreesaboveToineke.
Short-term reactive coping strategies
Other measures were reactive, consisting of immediate,
short-term responses to acute dangers. M ost of the strate-
gies mentioned here are traditional coping measures for
periodsofshortages.Theyarerootedintraditionalpractices
andlocalknowledge.Tosomeextent,theyarethesameas
theeverydaylivelihoodstrategiesbut are used moreinten-
sivelywhenfoodisscarce:
If ooding occurs, climbing onto the roof or staying
withrelativeswhoarenotaffected;
lookingforfoodintheforest(e.g.Putakpalmpith,tam-
arindseeds,wildcassava);
sellinganimalstobuyfood–sacricinglong-termcapi-
talforshort-termsurvival;
productionandsaleofcoconutoil,saltandpalmwine
(IrisTuak),kapok(plant-derivedmattresslling)andpe-
lepah(constructionmaterialfromtheputakpalm);
shinginthesea
searchingfortemporaryworkinsurroundingtowns(as
householdworkers,motorcycletaxidrivers,tofusellers
etc.);
takingchildrenoutofschool;spendingtheschoolbook
moneyonfood;
duringoods:notsendingchildrentoschoolforfearof
furtheroodwavesanddrowning.
Future oriented coping strategies
Future oriented coping strategies are implemented before
oodingordrought,tobepreparedforthesetimesofscarci-
ty.However,theyarealsochosenbecausetheyarerelatively
easyandcheaptocarryout.Thelocalsdonotknowwhether
orwhentheoodsordroughtsmayreturnandwhetherthe
newclimatewill stabilizeorchangefurther,sotheychoose
thecheaper provisionalmeasuresrather than themore ex-
pensiveadaptation.Relativelyshort-termreactivestrategies
arementionedaboveallinconnectionwithdrought,whereas
thelonger-termcopingstrategiesaremoreimportantwhen
facingtheoods:
“WhenIseeblackclouds,Iputallourpossessionsupin
theroof: tax return,marriagecerticate,baptism and
conrmationcerticates,schoolreportsandclothes.”
Elevatingthecookingandsleepingaccommodationand
theanimals’quarters;
Keepingcleantominimizethedangerofcontagion;
Laying in stocksofKayuular(snakewood,Lat.:Strych-
noslucida)for malariaoutbreaks (boiled inwater; the
liquidisdrunk);
Stockinguponrewood,drinkingwaterinclosedcon-
tainers,waterforwashing,lamppetroleum;
Plantingvegetablesinpartsofthegardenwhichdonot
becomeooded;
Takinganimals(torelatives)tohigherground.
Long-term adaptation strategies
Long-termadaptationstrategies(asopposedtocopingstrat-
egies) for climate change impacts are more expensive, so
people’s ability to adopt these strategies depend on many
factors: income, social networks, access to other land, re-
quiredknowledge,aswellaspersonalreadinesstomakede-
cisionsandadoptinnovations.Tousethevocabularyofthe
vulnerabilityperspective(seeSectionIV.3),itdependsonthe
availablenancial,social,physicalandnaturalcapital.
ThemostcommonadaptationstrategyinToinekeistoadopt
differentcropsandplantingtimes.Insteadofthetraditional
maize,riceisincreasinglyoftensown.Maizeplantsgrowwell
intheoods, buttheharvest ispoor.Riceseed(paddy go-
rah),ontheotherhand,ourishedlastyear;asaresult,some
villagersareconsideringterracingandirrigationsystems.
Maizeisstill cultivatedon higherground. Green beansare
alsocentralto food security.Inthe last fewyear,thebeans
plantedintherainyseason either drowned in theoods or
weredestroyed by sediments orsalt water.Toprevent this
happening again, the vill agers are planting a fast-growing
beanvariety at thestartof and during therainy season in
areaslessaffectedbyooding.Theycanharvesttheseplants
beforetherstoods,soprotectingthemfromsediments.
Thewomendescribediversication of varieties in fruitand
vegetable production. Fruit varieties which grow on tall
plants or trees, such asbananas, coconutsand sugarcane,
arebecomingmoreimportant.Vegetablesdonotsurvivethe
oods, so they are only grown during the r ainyseason by
farmerswhoselandislocatedhigherup,andinthedrysea-
sonby those whohaveaccessto good water.Tospreadthe
riskinthedryseason,awiderrangeofdifferentvegetables
iscultivated.
Thevillagershavealsoextendedtherangeofitemsproduced
inhomeindustries,particularlyintheuseofproductsgained
fromresources not affected by theoods (e.g.coconut oil,
coconutseedlings,coconutlampshadesetc.).
Finally,some villagers have beguntoestablishasecondary
source of income as carpenters, motorcycle tax i drivers or
openingakiosk,inadditiontosubsistenceagriculture.This
showsthatsomeofthelocalpopulationalreadyperceivethe
impacts of climate changesoclearly that their dependence
on agriculture seems too r isky. Pract ising small scale trad-
ingandhome industriestogenerate income inaddition to
CASE STUDY: IBU YANSE LAK ABU
havehergardenterracedandtousethewaterowingpast
herhouseforricegrowing.
Inherview,thealterationsinthenaturalenvironmentare
go d - givenandit isthev il l agers’tasktor eactappro pr iatel y.
Terracing the village could make use of the god-given
oodwatertocultivaterice,whichisalsothegoaldened
byBupati.
IbuYanseseesitasessentialtoretainherabilitytoactin
thefaceofdroughtsandooding.Thepriorityistosecure
foodforpeopleandanimals.Knowledgeiscentral,inher
view.“Ihaveplentyofthingstosell,butifIdon’tknowthe
prices,I will be cheated by theJavanese or people from
Flores.”In her opinion, knowledge enables people to act
andndsolutions;sheseesthisasmuchmoreimportant
intheattempttoadaptsuccessfullyandtosurviveunder
the changed conditions than nancial resources (e.g. to
raisehousesonstilts)orpersonalnetworks(e.g.toaccess
landinhigherlocations).
IbuYanseLakabu(62),daugh-
ter of a Protestant pastor,
widowoftheformervillage
policeman, retired teacher
and mother of the current
villageschoolteacher,isone
of the better-educated and
better-offvillagers.Shelives
with her daughter and two
grandchildreninahouseon
“jalanair”,oneofthewater-
ways created by the an nual
oods. She plans to pay to
subsistence farming is not a new strategy, but the increas-
ingimportanceoftheseincomesourcesindicatestheoften
predictedexodusfromagriculturalproduction.Thistypically
beginswiththedevelopment ofalternative income sources
inruralareas(initiallyastrategytoavoidimmediatemigra-
tion)andendswiththelarge-scalemigrationofyoungpeo-
plefromruralareasintothelargecitiesoftheircountry.
In contrast to the situation described in Tanzania, the vil-
lagersinToinekeseemtoconcentratemoreon diversifying
crops,varyingplantingtimesandseekingalternativeincome
sourcesratherthanspecialisinginafew protablebutalso
risky income sources. Three other long-term adaptation
strategieswere observed:rst, moving house, animalsand
cultivatedland;second,raisingthehouseandthird,protect-
ingcultivated land byfencing. The prerequisiteformoving
house,animalsandcultivatedlandisaccesstohigherground
inthevillage.However,mostvillagersdonothaveaccessto
higherground forconstruction, so they concentrate onse-
curing higher land for cult ivation or ask owners to permit
themtocultivatetheirlandforthemandsharetheharvest.
Successinthesecasesdependsonsocialcapitalsuchasfam-
ilyrelationshipsandpersonalnetworks.Toraisethehouses,
localconstructionmaterials(woodenpillars)orhome-made
cementblocks are useddepending onincome.Fencing the
vegetable gardens is intended to protect the cultivated ar-
easfromoodwater,sedimentsandbranchescarriedbythe
oods.
As well as these positive adaptation measures, there are
some negative adapt ations or maladaptations (see Sec tion
IV.2). One example is salt boiling, as already mentioned,
whichrequireslargeamountsofrewood.PakNohHun(45)
describes howhisfamilycarriesout traditionalsubsistence
agricultureaswellassaltproduction.However,oodinghas
made agriculture so dif cult that they are increasingly de-
pending on salt production fortheir livelihood. The use of
the forest around the village for rewood not only causes
additionalCO2emissions;thelocalecosystemisalsofurther
stressedandthevillagehaslesserosionprotection.Another
maladaptionwithseriousconsequencesistakingthechildren
out of school, in order to buy food w ith the money saved
fromthefees.Thisreduces the children’sabilitytofacethe
challengesofthefuture;knowledgeandinnovativethinking
areofcentralimportancewhendealingwiththeimpactsand
uncertaintiescausedbyclimatechange.
CASE STUDY: PAK YANDRI A. NENO
UND IBU ANTONIA MISA
ometerstohigherground.HecalledhisnewdaughterAiti
Mena,whichinUabMetomeans,“whowillcarryher?”The
ooddestroyedtheirhouse andtheircow,calf,hensand
goats were drownedor died later from the after-effects.
Pak Yandri turn ed to the village chi ef to ask permission
tobuildanewhouseabovethevillageonlandwhichhad
oncebe-longed tohisfather.Todayhehasaquarterhec-
tareofvegetablegardenaroundhisnewhouse,ahectare
on thehill for maize and a quarterhectare near the old
house.Heplanstoplantriceonthelower-lyinglandnext
rainyseason.Hissocialcapitalintheformofconnections
andfamilypossessionshasenabledhimtosecurealong-
termincomeforhisfamily.
It is a recurr ing problem for Pak Yandr i to nd the cash
forschoolfees.Forsomereason,hereceivesnothingfrom
thestatefund (KeluargaHarapanprogramme)set upfor
such situations (114 of the 680 households receive Rp.
200,000.00 per childper quarter). SoPak Yandri andIbu
Miasellcassavarootsandleavesattheweeklymarketand
PakYandrialsoworksintheeldsandasacarpenter.The
move away from the village centre makes the job hunt
moredifcult.Hehastovisitpossibleemployersregularly,
whereaspreviouslyhesawthemeverydayanyway.
P a k Ya n d r i A . N e n o (4 7, c o m -
pleted grammar school),
Ibu Antonia Misa (43) and
their four children were
caught by surprise in their
house by the ood on the
evening of 16 May 2000,
threedaysafterthebirthof
theirfourthchild.Withina
fewminutes,thewaterrose
chest high. Pak Yandri lift-
edhiswifeandthebabyto
safetyonatwo-meterhigh
roof beam. Next morning
he carried them three kil-
VI.5 TOINEKE: AN EXAMPLE OF LIFE IN POVERTY IN
CONDITIONS OF CLIMATE CHANGE
The people of Toineke are currently living under constantly
changing climatic conditions which have direct, immediate
conseqencesforagriculture,thebasisoftheirexistence.Their
methodsofdealing withthesituationexemplifymanyofthe
linksmentionedbetweenpovertyandclimatechange.
Likesubsistencefarmersinmanyothercountries,thefarmers
of Toineke aree xtremely dependent on their natural envi-
ronment.Climatechange signiesdirectdamagecausedby
droughtandoodingaswellasincreasingclimaticuncertain-
ty.Theyarebecomingevermorevulnerable,bothbecauseit
isnotclearhowtheyshouldbestreactandalsobecausethey
simplylackthemoney.Theyonlyachievepartialsuccesses:
smallinnovations(suchastheprotectivefencesaroundtheir
elds),lesseningtherisksbyplantingmoreordifferentcrops
etc.
Variousformsofknowledge arecrucialtoenablepeopleto
maintaintheircapacitytoactandcope withtheuncertain-
tiescausedbyclimatechange.Localknowledgeoftraditional
strategiestobeusedintimesofscarcityareimportant(e.g.
using the putak palm for food). Local innovati ons (such as
protective fencing around the gardens, raising houses on
stilts) and external knowledge (e.g. new varie ties of seed)
arealsosignicant.Inaddition,thepopulationrequiresthe
basicunderstandingorawarenessthatchangesintheirliving
conditionsaremore extensiveandlonger-lastingthanthey
have ever experienced. Lack of knowledge about climate
changeasa global process delaysthe developmentof local
adaptation strategies and makes it more dif cult, because
thelocalsconcentratetheirfewresourcesonshort-termpro-
visionalcopingstrategies.
These various forms of knowledge are combined in daily
dealingswithimpacts of climate change withmoreorless
success,workingtogethertoenablepeopletodevelopcop-
ingandadaptationstrategies.In this way,local knowledge
adjuststothedemandsofclimatechangeimpacts.Thekey
factorishowexibleandinnovativepeopleareinthinking
abouttheirsituation.Thecasestudiespresentedshowclearly
thatsuccessiscloselyrelatedtothedegreeofformaleduca-
tionreceived;themajorityofthosewhohavedevelopednew
strategiesandtechniqueshadbeentosecondaryschool.This
meansthatpovertyreductioneffortsshouldmakeeducation
availabletoenablepeopletoimplementtheknowledgethey
alreadyhave,newideasandtheircapacitytochange.
People’s ability to react to climate change also depend on
howprosperoustheyalreadyare.Inthisway,climatechange
deepens the gulfbetweenthe poor and thebetter-off and
leadsto new inequalities, both withinvillage communities
andbetweenvillages,regionsandcountries.Thebetter-off
familieswereoftenabletoutilizetheircapital–social,nan-
cial (see section IV.3)–to counter thechanging conditions
successfullyandinsomecases,eventousethempositively.
Others, such asIbu Yanse Ton and PakAugustinus andIbu
Naema,loseeventhelittlelivelihoodbasetheyhad.Insuch
cases, climate changeimpactsresult in a huge overload of
people’slivelihoodstrategiesandcopingcapacity.
Thefollowingrecommendationsareprimarilyrelatedtothe
workoforganizationssuchasCAREinternational.Although
theyweremainlyimplementedaslocalmeasuresandprojects
carriedoutdirectlyincooperationwithpoorerpopulations,
variousconclusionscanbedrawnfromthemforthenational
orinternationallevel.
Community-basedadaptation.Povertyreductionshould
encourageadaptationtonewlivingandeconomiccondi-
tions.Thisshouldtakeplaceatlocallevelandwithlocal
participation, and, aboveall,shouldbe basedonexist-
inglocalcopingandadaptationstrategies.Thesemay(or
maynot)begoodstartingpointsforlocalmeasuresand
“homegrown”bestpracticesforotherorganizationsand
projects.
Supportinglocalknowledge.Detailedlocalknowledge
ofecosystems andalternative options shouldbe gath-
eredandupdated.Itisimportanttogainnewknowledge
aboutadaptation optionsonthe spot. It isalsoimpor-
tanttocreateawarenessthatcurrentweathervariations
arepartofaglobalprocesswhichissettocontinue.Vil-
lage communitieslike Toineke must be encouraged to
test the ir knowledge to see how far it w ill help the m
to deal with climate change impacts. The experience
of other regions with ooding or drought should be
shared. “Global”knowledge, e.g.ndingsfromclimate
research,must be madeavailable, soit can berelated
tolocal knowledge. Theremust be a continuous proc-
ess of updating local climate managementknowledge,
becausetheclimate isnotlikelytostabilizeinthenear
future.
Criticalanalysisofexistingpractices.Existingcopingand
adaptation mechanisms may have become widespread
and may be assumed to be in the interests of at least
somegroups.However,theyshouldbeexaminedinthe
contextofthevecriteriamentionedabove–effective-
ness, exibility, fairness, ef ciency and sustainability –
particularly in relation tothe poorest.For example, an
adaptationmechanismmaybesuccessfulandalso“home
grown”.However,itmayatthesametimeexacerbatein-
equalityandsoincreaseabsolutepoverty.Itmaybewell
established,butpossiblybymorepowerfulgroupsandto
thedisadvantageofwomenormarginalsocialgroups.
Raisingawarenessforclimatechangeimpactswhichare
notyetacute.Finally,adaptationprocessesshouldbeena-
bled,evenwheretheydonotappearurgent.Itisessential
toraiseawarenessofthefactthatclimatechangeisnot
alwaysdramatic;itcanalsotakeplacegradually.People
arealreadyawareofsomeclimatechangeimpacts.Oth-
ersarenotyetknownordealingwiththemispostponed
infavourofothertaskswhichseemmoreurgent.
Recognizinguncertainties.Projectionsofclimatechange
processesand impactsgive theimpressionthat poverty
reduction can be based on concrete weather develop-
ments. However this cannot be taken for granted, be-
causethemodelsareuncertainandtheclimatechange
VII. Recommendations:
poverty reduction in times of climate change
process depe nds on humanity’s futur e actions. Mak ing
poverty reduction measures climate secure does not
meanbasingthemononeprojection.First,itisnotclear
howpeoplewillreacttothemeasuresandwhetherthey
willbeeffective,eveniftheclimatepredictionsareful-
lled. Second,the climatemight developinunforeseen
ways. Poverty reduction strategies are climate secure
onlyiftheyhavepositiveeffectsinvariousscenarios(no
regretcriterion).
Carefulhandlinginthefaceoftheurgencyofadaptation
to climate change imp acts. The pressur e to implement
adaptationmeasuresis enormous:however,thisshould
notleadtoimposingstrategiesonthelocalpopulation,
ignoring their local knowledge and existing adaptation
practices.Nor shoulditleadto hastyxingonparticular
scenariosasabasisforquickandapparentlysuitablemeas-
ures.Thisdoesnotmeanunderestimatingtheurgencyof
climate change; on the contrary, it means guaranteeing
thatmeasuresarereallyeffectiveandsustainable.
Poverty reductionmeansmaintainingbasiccapacityfor
action.Inordertoberealisticandtoconcentrateefforts,
povertyreductionshouldconcentrateonthepoorestand
onmaintainingtheirbasiccapabilityofaction.Thepopu-
lation’sresilienceshouldbestrengthenedgenerally,not
just in relat ion to specic r isks. It is likely that climate
change will cause even morerapidreactions in future,
soitisimportanttofocusontheshort-sightedmaladap-
tations. Governments must al so maintain room to ma-
noeuvre,tocopewithclimatechangeandpoverty.The
economiceffectsofclimatechangemustnotbeallowed
tocausefurtherreductionsinstatefundingforpoverty
reduction.Development aid canbe a temporarysource
ofassistanceduringtheglobaleconomicdownturnand
nancialcrisis.
Broad-based, in-depth analysis of climate change im-
pacts and measures. As the c ase studies show,climate
changeimpactsandadaptationmechanisms oftenhave
unexpectedconsequences.Someapparentlyappropriate
suggestions such as diversifying income sources have
turnedouttobecounter-productive.Organizationstack-
lingpovertyshouldinvestsufcientlyinresearchtoesti-
matethecomplexconsequences.Theyshouldtakeeven
more careful accountof particular local conditions and
thewaysin which ecosystemsandsocialsystems inter-
act.Holisticanalysisis essential to cover alltheinterac-
tionsasfully,evenifnotasprecisely,aspossible.
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IMPRINT
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CenterforDevelopmentResearch(ZEF)
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Dr.Anna-KatharinaHornidge(Case-StudyIndonesia)
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SandraBulling
www.kava-design.de,Bonn
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