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首页> 外文期刊>Journal of Water Resources Planning and Management >Impact of Climate Change on Hydrology and Hydrologic Extremes of Upper Blue Nile River Basin
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Impact of Climate Change on Hydrology and Hydrologic Extremes of Upper Blue Nile River Basin

机译:气候变化对上蓝尼罗河流域水文和水文极端的影响

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The potential global warming impact on the extreme and mean streamflow of the Upper Blue Nile (UBN) River Basin was projected for the 2050s and 2080s by three hydrological models [Nedbor-Afstromnings Model (NAM), Variable Infiltration Capacity (VIC) model, and Watflood model] driven by Representative Concentration Pathway (RCP) 4.5 and 8.5 climate change scenarios of four general circulation models (GCMs) dynamically downscaled by a regional climate model, Weather Research and Forecasting (WRF). The three hydrological models were able to capture the flow dynamics accurately in both calibration and validation periods. The mean daily maximum (minimum) temperature of UBN are projected to increase by about 1.35 degrees C-2.38 degrees C (1.72 degrees C-2.74 degrees C) under the RCP4.5 climate scenario and 2.22 degrees C-4.47 degrees C (2.5 degrees C-5.1 degrees C) under RCP8.5 climate scenario in future periods with reference to 1976-2005 as the base period. However, changes projected for the mean annual precipitation vary widely, ranging from -10.3% to 19.4%. The projected increase in evapotranspiration and increase or decrease in precipitation will result in a projected increase or decrease in streamflow of UBN. Overall, the median of mean annual streamflow of UBN is projected to decrease by 7.6% within a range of -19.7% to +17.7% in the 2050s and by 12.7% within a range of -26.8% to +31.6% in the 2080s. The ensemble mean of annual maxima (minima) of high return periods are projected by the three hydrologic models to be larger (smaller) in the 2050s and 2080s, respectively. On the whole, uncertainties due to the structure of hydrologic models, especially for low flow projections, are likely larger than uncertainties from GCMs and climate change scenarios. The results suggest that UBN is likely to experience more frequent and severe hydrologic extremes (flooding and droughts) in the future. Preliminary adaptive measures have been presented to mitigate the possible impact of droughts on UBN. (c) 2020 American Society of Civil Engineers.
机译:对2050年代和2080年代的三种水文模型(NEDBOR-AFSTOMNINGS(NAM),可变渗透能力(VIC)模型,将对2050年代和2080年来预测对大蓝尼罗河(UBN)河流域的极端和平均流出的潜在全球变暖的影响Watflood模型]由代表性浓度途径(RCP)4.5和8.5气候变化方案的四个一般循环模型(GCMS)由区域气候模型,天气研究和预测(WRF)动态缩小。三种水文模型能够在校准和验证期间精确地捕获流动动力学。 UBN的平均每日最大(最小)温度被投影为在RCP4.5气候情景下增加约1.35摄氏度C-2.38摄氏度(1.72摄氏度C-2.74摄氏度)和2.22摄氏度C-4.47摄氏度(2.5度C-5.1摄氏度C-5.1摄氏度在RCP8.5下降期间,参考1976-2005作为基本期间。但是,为平均年降水量投入的变化很大,范围从-10.3%到19.4%。预计的蒸散量增加和降水量的增加或降低将导致UBN的流流量的预计增加或减少。总体而言,UBN的平均年度流流量的中位数预计将在2050年代的范围内减少7.6%至+ 17.7%,2080年代的范围为-26.8%至+ 31.6%。在2050年代和2080年代的三种水文模型中投射了高回流期的年度最大值(最小值)的集合均值,分别更大(更小)。总的来说,由于水文模型结构,特别是对于低流量投影,可能比来自GCMS和气候变化情景的不确定性,不确定性。结果表明,未来UBN可能会经历更频繁和更严重的水文极端(洪水和干旱)。提出了初步自适应措施以减轻干旱在UBN上的可能影响。 (c)2020年美国土木工程师协会。

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