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首页> 外文期刊>Theoretical and applied climatology >Assessment of climate change impact on water diversion strategies of Melamchi Water Supply Project in Nepal
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Assessment of climate change impact on water diversion strategies of Melamchi Water Supply Project in Nepal

机译:评估气候变化对尼泊尔Melamchi供水项目的调水策略的影响

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摘要

This paper analyzes the climate change impact on water diversion plan of Melamchi Water Supply Project (MWSP) in Nepal. The MWSP is an interbasin water transfer project aimed at diverting water from the Melamchi River of the Indrawati River basin to Kathmandu Valley for drinking water purpose. Future temperature and precipitation of the basin were predicted using the outputs of two regional climate models (RCMs) and two general circulation models (GCMs) under two representative concentration pathway (RCP) scenarios which were then used as inputs to Soil and Water Assessment Tool (SWAT) to predict the water availability and evaluate the water diversion strategies in the future. The average temperature of the basin is projected to increase by 2.35 to 4.25 A degrees C under RCP 4.5 and RCP 8.5, respectively, by 2085s. The average precipitation in the basin is projected to increase by 6-18 % in the future. The annual water availability is projected to increase in the future; however, the variability is observed in monthly water availability in the basin. The water supply and demand scenarios of Kathmandu Valley was also examined by considering the population increase, unaccounted for water and water diversion from MWSP in the future. It is observed that even with the additional supply of water from MWSP and reduction of unaccounted for water, the Kathmandu Valley will be still under water scarcity in the future. The findings of this study can be helpful to formulate water supply and demand management strategies in Kathmandu Valley in the context of climate change in the future.
机译:本文分析了气候变化对尼泊尔Melamchi供水项目(MWSP)的调水计划的影响。 MWSP是一项跨流域调水项目,旨在将水从Indrawati流域的Melamchi河引到加德满都谷地,以用于饮用水。在两个代表性浓度路径(RCP)情景下,使用两个区域气候模型(RCM)和两个普通循环模型(GCM)的输出预测了盆地的未来温度和降水,然后将其用作土壤和水评估工具的输入( SWAT)以预测可用水量并评估未来的调水策略。在RCP 4.5和RCP 8.5下,盆地平均温度预计将在2085s之前分别升高2.35至4.25 A摄氏度。预计未来该盆地的平均降水量将增加6-18%。预计未来每年的可用水量会增加;但是,该流域的每月可用水量存在变化。加德满都谷地的供需情境也通过考虑人口增长进行了研究,这些人口是未来水和从MWSP引水的原因,但尚无定论。可以看出,即使通过MWSP提供额外的水,并且减少了无法解释的水量,加德满都谷地在未来仍将处于缺水状态。这项研究的结果将有助于在未来气候变化的背景下制定加德满都谷地的水供需管理策略。

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  • 来源
    《Theoretical and applied climatology》 |2017年第2期|311-323|共13页
  • 作者单位

    Asian Inst Technol, Sch Engn & Technol, Water Engn & Management, POB 4, Klongluang 12120, Pathum Thani, Thailand;

    Asian Inst Technol, Sch Engn & Technol, Water Engn & Management, POB 4, Klongluang 12120, Pathum Thani, Thailand;

    Asian Inst Technol, Sch Engn & Technol, Water Engn & Management, POB 4, Klongluang 12120, Pathum Thani, Thailand;

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