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首页> 外文期刊>Journal of Hydrology: Regional Studies >Modelling impact of climate change on catchment water balance, Kabompo River in Zambezi River Basin
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Modelling impact of climate change on catchment water balance, Kabompo River in Zambezi River Basin

机译:赞比西河流域卡博姆波河气候变化对流域水平衡的影响模拟

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Study RegionThe Kabompo River Basin (KRB) in Zambia is one of the 13 basins found in the Zambezi River Basin in Southern African region.Study FocusGlobal Climate Model (GCMs) projections have spatial resolution of up to several hundred kilometres, which may not be adequate for capturing local details mostly needed for impact assessment at local and regional scale. Downscaling techniques developed to improve the detail include; regional climate modelling and statistical techniques linking climate information at GCM resolution with that at local scale. This paper deals with evaluation and assessment of the impact of climate change on water balance for the KRB. In order to evaluate climate change impact, six bias–corrected and downscaled GCM outputs were acquired and used as inputs for hydrological modelling with the SWAT model to determine the impact under two future climate scenarios.New Hydrological Insights for the RegionThe results indicate that the future catchment water balance for KRB under RCP4.5 will have insignificant variation from the current catchment water balance as annual statistics show that rainfall will reduce by 1 % while water yield and runoff will increase by 5 % and 6 % respectively. Meanwhile under RCP8.5, annual statistics show that rainfall will increase by 19 % while water yield and runoff will increase by 40 % and 65 % respectively and resulting in a significant increase in catchment water balance.
机译:研究区域赞比亚的卡波姆波河流域(KRB)是南部非洲地区的赞比西河盆地中发现的13个流域之一。研究重点全球气候模型(GCM)预测的空间分辨率高达数百公里,可能不够充分用于捕获本地和区域规模的影响评估最需要的本地详细信息。为改善细节而开发的缩小尺寸技术包括;区域气候建模和统计技术将GCM分辨率的气候信息与地方尺度的气候信息联系起来。本文针对KRB评估和评估气候变化对水平衡的影响。为了评估气候变化的影响,获得了6个经偏差校正和按比例缩小的GCM输出,并用作SWAT模型进行水文建模的输入,以确定在两种未来气候情景下的影响。该地区的新水文见解结果表明,未来RCP4.5下的KRB的集水量与当前集水量的平衡变化不大,因为年度统计数据显示降雨将减少1%,而水的产量和径流量将分别增加5%和6%。同时,根据RCP8.5,年度统计数据显示降雨将增加19%,而水的产量和径流量将分别增加40%和65%,从而导致流域水量平衡显着增加。

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