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Assessment of the Impacts of Climate Change on Hydrological Characteristics of the Mbarali River Sub Catchment Using High Resolution Climate Simulations from CORDEX Regional Climate Models

机译:使用CORDEX区域气候模型的高分辨率气候模拟评估气候变化对姆巴拉里河流域水文特征的影响

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This study assesses the impacts of climate change on water resources over Mbarali River sub-catchment using high resolution climate simulations from the Coordinated Regional Climate Downscaling Experiment Regional Climate Models (CORDEX_RCMs). Daily rainfall, minimum and maximum temperatures for historical climate (1971-2000) and for the future climate projection (2011-2100) under two Representative Concentration Pathways RCP 8.5 and RCP 4.5 were used as input into the Soil and Water Assessment Tool (SWAT) hydrological model to simulate stream flows and water balance components for the Mbarali River sub-catchment. The impacts of climate change on hydrological conditions over Mbarali river catchment were assessed by comparing the mean values of stream flows and water balance components during the present (2011-2040), mid (2041-2070) and end (2071-2100) centuries with their respective mean values in the baseline (1971-2000) climate condition. The results of the study indicate that, in the future, under both RCP 4.5 and RCP 8.5 emission scenarios, the four main components that determine change in catchment water balance (rainfall, ground water recharge, evaporation and surface runoff) over Mbarali river catchment are projected to increase. While the stream flows are projected to decline in the future by 13.33% under RCP 4.5 and 13.67% under RCP 8.5 emission scenarios, it is important to note that simulated surface runoff under RCP8.5 emission scenario is higher than that which is obtained under the RCP4.5 emission scenario.
机译:这项研究使用协调的区域气候缩减实验区域气候模型(CORDEX_RCMs)的高分辨率气候模拟评估了气候变化对姆巴拉里河小流域水资源的影响。在两个代表性浓度路径RCP 8.5和RCP 4.5下,历史气候(1971-2000)和未来气候预测(2011-2100)的每日降雨量,最低和最高温度被用作土壤和水评估工具(SWAT)的输入水文模型来模拟姆巴拉里河子汇水流和水平衡组成部分。通过比较当前(2011-2040),中期(2041-2070)和末期(2071-2100)两个世纪之间河流流量和水平衡成分的平均值,评估了气候变化对姆巴拉里河流域水文条件的影响。在基线(1971-2000年)气候条件下它们各自的平均值。研究结果表明,将来,在RCP 4.5和RCP 8.5排放情景下,决定姆巴拉里河流域集水区水平衡变化(降雨,地下水补给,蒸发和地表径流量)的四个主要因素是预计会增加。虽然预计未来河水流量在RCP 4.5下会下降13.33%,在RCP 8.5排放下会下降13.67%,但需要注意的是,RCP8.5排放下的模拟地表径流量要高于RCP8.5排放下的模拟地表径流量。 RCP4.5排放情景。

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