Uncertainty assessment in river flow projections for Ethiopia's Upper Awash Basin using multiple GCMs and hydrological models

被引:18
|
作者
Chan, Wilson C. H. [1 ,5 ]
Thompson, Julian R. [1 ]
Taylor, Richard G. [1 ]
Nay, Alistair E. [1 ]
Ayenew, Tenalem [2 ]
MacDonald, Alan M. [3 ]
Todd, Martin C. [4 ]
机构
[1] UCL, Dept Geog, Pearson Bldg,Gower St, London WC1E 6BT, England
[2] Univ Addis Ababa, Sch Earth Sci, Addis Ababa, Ethiopia
[3] British Geol Survey, Lyell Ctr, Res Ave South, Edinburgh, Midlothian, Scotland
[4] Univ Sussex, Dept Geog, Brighton, E Sussex, England
[5] Univ Reading, Dept Meteorol, Reading, Berks, England
基金
英国自然环境研究理事会; 英国经济与社会研究理事会;
关键词
Upper Awash Basin; hydrological modelling; climate change; uncertainty; CLIMATE-CHANGE; WATER-RESOURCES; IMPACT; RAINFALL; RUNOFF; CALIBRATION; RESPONSES; DROUGHT;
D O I
10.1080/02626667.2020.1767782
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Uncertainty in climate change impacts on river discharge in the Upper Awash Basin, Ethiopia, is assessed using five MIKE SHE hydrological models, six CMIP5 general circulation models (GCMs) and two representative concentration pathways (RCP) scenarios for the period 2071-2100. Hydrological models vary in their spatial distribution and process representations of unsaturated and saturated zones. Very good performance is achieved for 1975-1999 (NSE: 0.65-0.8;r: 0.79-0.93). GCM-related uncertainty dominates variability in projections of high and mean discharges (mean: -34% to +55% for RCP4.5, - 2% to +195% for RCP8.5). Although GCMs dominate uncertainty in projected low flows, inter-hydrological model uncertainty is considerable (RCP4.5: -60% to +228%, RCP8.5: -86% to +337%). Analysis of variance uncertainty attribution reveals that GCM-related uncertainty occupies, on average, 68% of total uncertainty for median and high flows and hydrological models no more than 1%. For low flows, hydrological model uncertainty occupies, on average, 18% of total uncertainty; GCM-related uncertainty remains substantial (average: 28%).
引用
收藏
页码:1720 / 1737
页数:18
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