ClimateThe different parts of Hispaniola see major variationsin annual rainfall as a result of topography,prevailing winds, <strong>and</strong> the sporadic nature oftropical storms <strong>and</strong> hurricanes. The wettest areasare the peaks of the highl<strong>and</strong>s along the southerncoast, where rainfall can exceed 4000 mm,whilst the driest areas are in the northwest, whererainfall can drop to 350 mm per annum. All partsof Hispaniola experience a drier season fromDecember to April.At the national level, year round average temperaturesare 25° C for <strong>Haiti</strong> <strong>and</strong> 26.2° C for the<strong>Dominican</strong> <strong>Republic</strong>. Temperature variations arelinked to the seasons but also to the extent of cloud<strong>and</strong> altitude: the hottest regions are the dry plainsnear sea level where temperatures commonlyexceed 35° C <strong>and</strong> the coldest regions are thewet mountain peaks where temperatures rarelyexceed 20° C <strong>and</strong> can drop to 10° C degrees orlower.Climate Change<strong>Haiti</strong> has recently ranked 6 th at the 2012 ClimateRisk Index developed by the research institute Germanwatch.83 This indicator analyzes the impactsof extreme weather events of the last 20 years<strong>and</strong> identified <strong>Haiti</strong> as one of the most affectedcountries in the world. The <strong>Dominican</strong> <strong>Republic</strong>also ranks high on the same risk index, being oneof six Caribbean countries in the world’s top 40climate “hot spots”. 84 With a possible increase inthe frequency <strong>and</strong> severity of storms <strong>and</strong> adecrease in average rainfall 85 , the impacts ofchanging global <strong>and</strong> regional weather patternsis likely to further increase the vulnerability of theisl<strong>and</strong> to extreme weather events.Climate change projections for <strong>Haiti</strong> <strong>and</strong> the<strong>Dominican</strong> <strong>Republic</strong> are very similar. Both countriesanticipate increased average temperatures ofapproximately 0.7-1.0° C by 2030 <strong>and</strong> continuedincreases thereafter. 86, 87 Both countries also anticipatesignificant reductions in rainfall: up to 11% by2030 <strong>and</strong> 23% by 2050. 88, 89 Projections, however,vary greatly, highlighting the high level of uncertaintyin respect to the effects of climate changeon the isl<strong>and</strong>. The combination of increasedtemperature <strong>and</strong> decreased rainfall may well leadto water deficits <strong>and</strong> greatly reduced runoff/streamflows in both countries. 90More interesting, however, are changes that havealready taken place. In <strong>Haiti</strong>, <strong>UNEP</strong> field enquirieshave recorded significant anecdotal evidencefrom farmers of increased rainfall variability <strong>and</strong>later starting dates for the wet season. This issupported by studies showing that <strong>Haiti</strong>’s averagemonthly rainfall volumes have considerablydecreased <strong>and</strong> its patterns changed betweenthe beginning of the 20 th century <strong>and</strong> that of the21 st century. 91, 92 Data from 1900-1930, 1930-1960,1960-1990, had similar rainfall patterns. The threeperiods were characterized by two peaks, onebetween March-May <strong>and</strong> another betweenAugust-October. 93 These numbers contrast withthose of the 1990-2009 period. During this period,rainfall patterns have significantly changed,showing only one yearly peak in the month ofSeptember. Average monthly rainfall is the lowestcompared to the three previous 30-year periodsat 106 mm, <strong>and</strong> yearly average rainfall during thisperiod is the lowest at 1269 mm. The 1990-2009period has experienced a decrease in averageyearly rainfall of 368 mm compared to the precedingperiod. The 1990-2009 period has also seenthe most extreme rainfall variability, presentingboth the lowest (8.9 mm) <strong>and</strong> the highest (478 mm)monthly rainfall averages amongst all four 30-yearperiods analyzed.The <strong>Dominican</strong> <strong>Republic</strong> has experienced similarrainfall patterns as <strong>Haiti</strong>. Its yearly peaks havechanged from two a year, around March-May<strong>and</strong> August-October, to only one in the monthof September. 94 Even when the 1930-1960 periodexperienced lower average monthly <strong>and</strong> yearlyrainfall, the 1990-2009 period experienced themost extreme monthly rainfall volumes amongstthe four 30-year periods compared, with a low of13 mm <strong>and</strong> a high of 471 mm. 95 The 1990-2009period experienced a decrease in average yearlyrainfall of 275 mm compared to the 1960-1990period.Temperature patterns in <strong>Haiti</strong> also seem to havechanged throughout the course of the 20 thcentury <strong>and</strong> into the 21 st century. <strong>Haiti</strong>’s averagemonthly temperatures have gradually increasedthroughout the four periods mentioned. The 1900-1930 <strong>and</strong> 1930-1960 time periods had an averagetemperature of 24.3° C. For the 1960-1990 period,average temperatures increased by 1° C to anaverage temperature of 25.3° C, <strong>and</strong> increased24 <strong>Haiti</strong> <strong>–</strong> <strong>Dominican</strong> <strong>Republic</strong>: Environmental challenges in the border zone
once again for the 1990-2009 period to an annualaverage temperature of 25.4°C. 96The <strong>Dominican</strong> <strong>Republic</strong> has experiencedsimilar temperature patterns as <strong>Haiti</strong>. Averagetemperatures in the <strong>Dominican</strong> <strong>Republic</strong> haveincreased by around 1.2° C from the 1930-1960to the 1960-1990 time period. Between the1960-1990 <strong>and</strong> 1990-2009 time periods, however,temperatures decreased by 0.3° C to a yearlyaverage of 24.7° C. 97In summary, climate change for Hispaniola isexpected to result in an overall drier <strong>and</strong> hotterclimate, with more severe dry seasons with lowerstream flows, <strong>and</strong> exacerbating existing health,social <strong>and</strong> economic challenges.HydrologyThe majority of the rivers in the mountainous regionsof Hispaniola are short <strong>and</strong> steep. This means thatwater flow rates at any particular time are governedmainly by recent rainfall (days to hours) rather thanannual rainfall. Flash floods can occur in a matterof hours <strong>and</strong> the same rivers can run almost dryfor two months in the dry season. Flow variations of100 times or more are not uncommon. The levelof responsiveness reduces with increasing size, thelarger rivers with large catchments are much morestable than the smaller rivers.At the national level <strong>Haiti</strong> has substantial fresh waterresources, divided between 30 main watersheds. 98However it also has national scale, chronic waterproblems including degraded catchments, waterscarcity, flooding <strong>and</strong> bacterial contamination ofwater sources.The different Departments of <strong>Haiti</strong> see major variationsin annual rainfall as a result of topography,prevailing winds <strong>and</strong> the sporadic nature of tropicalstorms <strong>and</strong> hurricanes. The wettest areas are thepeaks of the highl<strong>and</strong>s along the southern coast,where rainfall can exceed 4000 mm, while thedriest areas are in the northwest Departments,where rainfall can drop to 350 mm per annum.All parts of the country experience a drier seasonfrom December to April.The Pedernales river, that forms the border in the southern part of the isl<strong>and</strong>, has a low water flow duringlarge parts of the year <strong>and</strong> is easy cross on foot. The water flow can, however, increase dramatically withinhours as a result of heavy rains falling in the mountains a couple of kilometers from the low lying coastalareas.© <strong>UNEP</strong><strong>Haiti</strong> <strong>–</strong> <strong>Dominican</strong> <strong>Republic</strong>: Environmental challenges in the border zone25
- Page 1: Haiti - Dominican RepublicEnvironme
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interventions if well designed do w
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contaminated rivers are disease vec
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crust substantial enough to be the
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tuna, sea bream, yellowtail, hake,
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Mangroves are being cut to be sold
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Case study 6. Cooperation between f
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private sector better informed. Cus
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carrying money, and missing their d
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etween these two cordilleras), but
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Mineral exploration is starting in
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assessment team are all small scale
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Extreme poverty is a key driving fo
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it is present. The Haitian populati
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Atlantic storms will double in the
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A charcoal kiln burning inside the
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Table 5. Summary of the key recomme
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Ten recommendations are provided un
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oth environmentally damaging and li
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Improving cooperation and governanc
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f. Create and formalize fishing agr
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g. In the long term, aim for variou
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Haiti - Dominican Republic: Environ
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Annex I - Report terminologyArgumen
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Annex II - List of Acronyms and Abb
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Annex IV - Table connecting thereco
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23. United States Census Bureau. (2
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73. UN Development Programme - Haï
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117. Urban Design Lab, Columbia Uni
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161. Miniel, L. (2012, 20 April). I
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204. Peralta, C. (2012, 18 April).
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246. González Sánchez, F.F. (2012
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290. Laboratoire des Relations Hait
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Annex VI - AcknowledgementsContribu
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Claude PhanorMartin RapillyAdelita
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José Cristino CastilloRobert Crowl
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www.unep.org/disastersandconflicts