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首页> 外文期刊>The Science of the Total Environment >Hydrological response of Chamelia watershed in Mahakali Basin to climate change
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Hydrological response of Chamelia watershed in Mahakali Basin to climate change

机译:Mahakali盆地Chamelia流域对气候变化的水文响应

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Chamelia (catchment area = 1603 km(2)), a tributary of Mahakali, is a snow-fed watershed in Western Nepal. The watershed has 14 hydropower projects at various stages of development. This study simulated the current and future hydrological system of Chamelia using the Soil and Water Assessment Tool (SWAT). The model was calibrated for 2001-2007; validated for 2008-2013; and then applied to assess streamflow response to projected future climate scenarios. Multi-site calibration ensures that the model is capable of reproducing hydrological heterogeneity within the watershed. Current water balance above the Q120 hydrological station in the forms of precipitation, actual evapotranspiration (AET), and net water yield are 2469 mm, 381 mm and 1946 mm, respectively. Outputs of five Regional Climate Models (RCMs) under two representative concentration pathways (RCPs) for three future periods were considered for assessing climate change impacts. An ensemble of bias-corrected RCM projections showed that maximum temperature under RCP4.5 (RCP8.5) scenario for near-, mid-, and far-futures is projected to increase from the baseline by 0.9 degrees C (1.1 degrees C), 1.4 degrees C (2.1 degrees C), and 1.6 degrees C (3.4 degrees C), respectively. Minimum temperature for the same scenarios and future periods are projected to increase by 0.9 degrees C (1.2 degrees C), 1.6 degrees C (2.5 degrees C), and 2.0 degrees C (3.9 degrees C), respectively. Average annual precipitation under RCP4.5 (RCP8.5) scenario for near-, mid-, and far-futures are projected to increase by 10% (11%), 10% (15%), and 13% (15%), respectively. Based on the five RCMs considered, there is a high consensus for increase in temperature but higher uncertainty with respect to precipitations. Under these projected changes, average annual streamflow was simulated to increase gradually from the near to far future under both RCPs; for instance, by 8.2% in near-, 12.2% in mid-, and 15.0% in far-future under RCP4.5 scenarios. The results are useful for planning water infrastructure projects, in Chamelia and throughout the Mahakali basin, to ensure long-term sustainability under climate change. (c) 2018 Elsevier B.V. All rights reserved.
机译:Chamelia(集水区= 1603 km(2))是Mahakali的支流,是尼泊尔西部的雪域。该流域有14个处于不同开发阶段的水电项目。这项研究使用土壤和水评估工具(SWAT)模拟了Chamelia的当前和未来的水文系统。该模型已针对2001-2007年进行了校准;经过验证的2008-2013年;然后用于评估对预计的未来气候情景的水流响应。多站点校准可确保模型能够再现流域内的水文非均质性。 Q120水文站上方当前的水平衡分别为降水量,实际蒸散量(AET)和净水量,分别为2469毫米,381毫米和1946毫米。为了评估气候变化的影响,考虑了两个代表性浓度路径(RCP)下三个未来时期的五个区域气候模式(RCM)的输出。一组经过偏差校正的RCM预测表明,在RCP4.5(RCP8.5)情况下,近,中和远期的最高温度预计将从基线升高0.9摄氏度(1.1摄氏度),分别为1.4摄氏度(2.1摄氏度)和1.6摄氏度(3.4摄氏度)。预计在相同情况下和未来一段时间内的最低温度将分别增加0.9摄氏度(1.2摄氏度),1.6摄氏度(2.5摄氏度)和2.0摄氏度(3.9摄氏度)。在RCP4.5(RCP8.5)情景下,近,中和远期的年平均降水量预计分别增加10%(11%),10%(15%)和13%(15%) , 分别。基于所考虑的五个RCM,对于温度升高存在高度共识,但降水方面的不确定性更高。在这些预计的变化下,模拟了两个RCP的年均流量从近期到远期逐渐增加。例如,在RCP4.5情景下,近端上升8.2%,中段上升12.2%,远期上升15.0%。该结果对于在Chamelia和整个Mahakali流域规划水基础设施项目很有用,以确保在气候变化下的长期可持续性。 (c)2018 Elsevier B.V.保留所有权利。

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