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马哈拉卡里流域查梅利流域对气候变化的水文响应。

Hydrological response of Chamelia watershed in Mahakali Basin to climate change.

机构信息

International Water Management Institute (IWMI), Nepal Office, Lalitpur, Nepal.

International Water Management Institute (IWMI), Nepal Office, Lalitpur, Nepal.

出版信息

Sci Total Environ. 2019 Feb 10;650(Pt 1):365-383. doi: 10.1016/j.scitotenv.2018.09.053. Epub 2018 Sep 5.

Abstract

Chamelia (catchment area = 1603 km), 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 °C (1.1 °C), 1.4 °C (2.1 °C), and 1.6 °C (3.4 °C), respectively. Minimum temperature for the same scenarios and future periods are projected to increase by 0.9 °C (1.2 °C), 1.6 °C (2.5 °C), and 2.0 °C (3.9 °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.

摘要

查梅利娅(集水区面积为 1603 平方公里)是尼泊尔西部一条发源于雪山的河流,属于玛哈卡里亚河的支流。该集水区有 14 个处于不同开发阶段的水电项目。本研究使用土壤和水评估工具(SWAT)模拟了查梅利娅当前和未来的水文系统。该模型经过 2001-2007 年的校准、2008-2013 年的验证,随后被用于评估未来气候情景对河川流量的响应。多站点校准确保模型能够再现流域内的水文异质性。目前,Q120 水文站以上的水量平衡以降水、实际蒸散(AET)和净产水量的形式分别为 2469mm、381mm 和 1946mm。未来三个时期的两种代表性浓度途径(RCP)下,考虑了五个区域气候模型(RCM)的输出,以评估气候变化的影响。一组经偏差校正的 RCM 预测结果显示,RCP4.5(RCP8.5)情景下,近、中、远期的最高温度预计将分别比基准值增加 0.9°C(1.1°C)、1.4°C(2.1°C)和 1.6°C(3.4°C)。同一情景和未来时期的最低温度预计将分别增加 0.9°C(1.2°C)、1.6°C(2.5°C)和 2.0°C(3.9°C)。RCP4.5(RCP8.5)情景下,近、中、远期的年平均降水量预计将分别增加 10%(11%)、10%(15%)和 13%(15%)。根据所考虑的五个 RCM,在温度升高方面有很高的一致性,但降水方面的不确定性更高。在这些预测的变化下,RCP 下的近、中、远未来的年平均径流量都逐渐增加;例如,RCP4.5 情景下,近未来增加 8.2%,中未来增加 12.2%,远未来增加 15.0%。这些结果有助于规划查梅利娅和整个玛哈卡里亚流域的水基础设施项目,以确保在气候变化下的长期可持续性。

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