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Adapting to Climate Change: Assessing the World Bank Group ...

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CHAPTER 3CLIMATE VARIABILITYBox 3-1. Managing Water Resources in <strong>the</strong> Mekong River BasinThe Mekong River Basin illustrates <strong>the</strong> challenges of transboundary integrated water resourcesmanagement and <strong>the</strong> inextricability of climate change and development planning.The lower basin riparians—Cambodia, Lao Peoples Democratic Republic, Thailand, and Vietnam—began discussing basin management in 1957 and formed <strong>the</strong> Mekong River Commission (MRC) in 1995.The MRC’s mission is “To promote and coordinate sustainable management and development of waterand related resources for <strong>the</strong> countries’ mutual benefit and <strong>the</strong> people’s well-being.” This is a technicallyand politically challenging task. The lower basin alone has 60 million inhabitants and <strong>the</strong>re are complexinterconnections among <strong>the</strong> many water uses. The river’s annual cycle of ebb and flood sustain <strong>the</strong> richfisheries and distinctive ecology of <strong>the</strong> Tonle Sap Great Lake and regulate water and nutrient flows <strong>to</strong><strong>the</strong> fertile irrigated fields of <strong>the</strong> Mekong Delta. Development of <strong>the</strong> basin’s immense hydropowerpotential can bring income and carbon-free energy, but it also affects water and sediment flows, as wellas <strong>the</strong> river’s unique aquatic biodiversity. Sorting out development plans would be difficult enoughwithin a single country, let alone among four nations with a his<strong>to</strong>ry of conflict.The GEF-funded, <strong>Bank</strong>-executed Water Utilization Project (WUP) addressed both <strong>the</strong> technical andpolitical challenges. The core idea was <strong>to</strong> build confidence, trust, and data sharing through <strong>the</strong>construction of a hydrological model of <strong>the</strong> basin—<strong>the</strong> Decision Support Framework (DSF). The DSFwould <strong>the</strong>n be used <strong>to</strong> determine minimum allowable values for water flow and water quality.Agreement on <strong>the</strong>se “rules” would define a “Development Opportunity Space” that could be used <strong>to</strong>determine <strong>the</strong> acceptability of proposed plans for development. A similar approach was successfullyused, over a long period in <strong>the</strong> negotiation of European treaties on transboundary air pollution. Riverbasin modeling activities were also included in <strong>the</strong> <strong>Bank</strong>-executed portion of <strong>the</strong> Nile Basin Initiative.Results <strong>to</strong> date have been mixed. Progress was made on adopting procedural guidelines, including thoserelated <strong>to</strong> prior consultation on projects that affect <strong>the</strong> Mekong mainstream. The DSF was constructedand <strong>the</strong> process has contributed <strong>to</strong> capacity building and data-sharing. However, <strong>the</strong> MRC countrieshave so far been unable <strong>to</strong> agree on <strong>the</strong> critical parameters defining water quality and quantity. Soinstead of starting with criteria for water quality and quantity and using <strong>the</strong>m <strong>to</strong> assess developmentscenarios, <strong>the</strong> MRC has proceeded in <strong>the</strong> opposite direction. It has defined some development scenariosand used <strong>the</strong> DSF <strong>to</strong> assess <strong>the</strong>ir impact on water quality and quantity, <strong>to</strong>ge<strong>the</strong>r with o<strong>the</strong>renvironmental and economic impacts.The DSF has been used <strong>to</strong> explore <strong>the</strong> implications of development and climate change for <strong>the</strong> Basin. In<strong>the</strong> absence of fur<strong>the</strong>r development, climate change would tend <strong>to</strong> increase both high and low flows.However, a development scenario (including ongoing construction of s<strong>to</strong>rage reservoirs in China), tends<strong>to</strong> even out <strong>the</strong> annual flow cycle, especially upstream in <strong>the</strong> Lower Basin, counteracting climate impactsduring <strong>the</strong> rainy season and reinforcing <strong>the</strong>m during <strong>the</strong> dry season. The DSF can assess some of <strong>the</strong>costs and benefits of <strong>the</strong>se changes, including impacts on <strong>the</strong> Tonle Sap and on <strong>the</strong> Mekong Delta,though it does not well represent sediment flows or fish migration.The <strong>Bank</strong> is increasingly engaged in analytic and project work on integrated water resourcemanagement in large river basins (both national and transboundary), including <strong>the</strong> Amu Daurya, Niger,Shire (Malawi), Tana and Beles (Ethiopia) and Zambezi,. As in <strong>the</strong> case of <strong>the</strong> Mekong, much of thiswork relies heavily on hydrological modeling <strong>to</strong> explore <strong>the</strong> economic and environmental impacts ofalternative development and climate scenarios. A lesson from <strong>the</strong> WUP is <strong>the</strong> desirability of using opensourcemodeling. The WUP uses, in part, a proprietary model. This inhibits wider distribution andindependent review of model structure and performance, undermining capacity building andcredibility.Source: IEG mission; (Mekong River Commission 2010)35

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