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                  โครงการหนังสออเล็กทรอนกสด้านการเกษตร เฉลมพระเกียรตพระบาทสมเด็จพระเจ้าอยู่หัว
                               International Seminar on Biodiversity and Sustainable Development in the Mekong River Basin   41

               corresponding to scenario B2). Next is the rice crop. Irrigation water demand of crop rice increases
               at least (0.6% in 2050 and 1.9% in 2100, B2 scenario).

               Study area
                       According  to  the  National  Center  for  Planning  and  Investigation  of  Water  Resources
               (NAWAPI), the Central Highlands in general and the SRB in particular are one of the regions most
               affected by CC. With the trend of high rainfall in the rainy season and a sharp decrease in the dry
               season, it has led to a serious water shortage for the study basin in the dry season. Especially in
               recent  years,  erratic  rain  has  caused  a  prolonged  dry  season,  high  temperature  and  frequent
               droughts in the Srepok River Basin (SRB). Since the SRB is a closed basin, rainwater resources
               will play an important role and be the only water source to replenish and supply water for the entire
               basin.




































                                Fig 1. DEM and drainage networks of the Srepok River Basin

                       Under  the  impact  of  CC,  the  tendency  of  rainfall  to  increase  in  the  rainy  season  and
               decrease sharply in the dry season has led to a serious water shortage for the basin in the dry
               season. Especially in recent years, erratic rain has caused a prolonged dry season, high temperature
               and frequent droughts in the SRB. The scenario of rainfall variation in the SRB is located in 4
               provinces: Gia Lai, Dak Lak, Dak Nong and Lam Dong. Based on the 2017 version of CC scenario
               - Ministry of Natural Resources and Environment built for the above 4 provinces to interpolate the
               rainfall change of the SRB according to the above scenarios (NAWAPI). In general, the average
               annual rainfall in the 4 Provinces of the SRB increased significantly (NAWAPI). The period 2016
               - 2050 compared with the baseline period 1986 - 2005 has the following changes in rainfall: In Gia
               Lai, the rainfall increased by 8.3% for the RCP 4.5 average scenario and 10% for the RCP 4.5
               scenario. High RCP 8.5. In Dak Lak, the rainfall increases by 6.5 % for the RCP 4.5 scenario and
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