The Tonle Sap is the most fertile and diverse freshwater ecosystem in Southeast Asia, receiving nurturing water flows from the Mekong and its immediate basin. In addition to rapid development in the Tonle Sap basin, climate change may threaten natural flow patterns that sustain its diversity. The impacts of climate change on river flows in 11 sub-basins contributing to the Tonle Sap Lake were assessed using the Soil and Water Assessment Tool (SWAT) model to quantify the potential magnitude of future hydrological alterations. Projected river flows from three General Circulation Models (GFDL-CM3, GISS-E2-R-CC and IPSL-CM5A-MR) for three time horizons (2030s, 2060s and 2090s) indicate a likely decrease in both the wet and dry season flows. The mean annual projected flow reductions range from 9 to 29%, 10 to 35% and 7 to 41% for the 2030s, 2060s and 2090s projections, respectively. Moreover, a decrease in extreme river flows (Q(5) and Q(95)) was also found, which implies there could be a decline in flood magnitudes and an increase in drought occurrences throughout the basin. The results of this study provide insight for water resources planning and adaptation strategies for the river ecosystems during the dry season, when water flows are projected to decrease.
1.Inst Technol Cambodia, Fac Hydrol & Water Resources Engn, Phnom Penh 12156, Cambodia 2.Univ Canterbury, Dept Civil & Nat Resources Engn, Christchurch 8140, New Zealand 3.Univ Calif Berkeley, Dept Landscape Architecture & Environm Planning, Berkeley, CA 94720 USA 4.Univ Lyon, Collegium Inst Adv Studies, F-69007 Lyon, France 5.Asia Ctr, Stockholm Environm Inst, Bangkok 10330, Thailand 6.Univ S Florida, Dept Civil & Environm Engn, Tampa, FL 33620 USA
Recommended Citation:
Oeurng, Chantha,Cochrane, Thomas A.,Chung, Sarit,et al. Assessing Climate Change Impacts on River Flows in the Tonle Sap Lake Basin, Cambodia[J]. WATER,2019-01-01,11(3)