埃塞俄比亚Muger次盆地地表水资源评价

Dereje Adeba, Shimelis Tafese
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摘要

水资源评价是为了更好地开发和管理水资源而测量、收集和分析水资源数量和质量的有关参数的过程。本研究的目的是对埃塞俄比亚Muger次盆地地表水资源进行评价。从Abbay流域RCM中提取未来可能出现的局地气候变量,与观测到的气象变量进行偏差校正后作为气候数据输入到水土评估工具(SWAT)模型中,并利用气候数据、土壤数据、土地利用、土地覆盖、子流域坡度和weather Generator共同模拟Muger子流域未来的水量。采用水土评估工具(SWAT)进行径流模拟。结果表明,SWAT模型具有良好的性能,在月径流校正过程中,Nash-Sutcliffe效率(NSE)和决定系数(R2)分别为0.76和0.99,在月径流验证过程中,Nash-Sutcliffe效率(NSE)和决定系数(R2)分别为0.63和0.99。与基期(1996-2009)相比,马格尔盆地降水变化(2010-2023)、(2024-2037)和(2038-2050)分别减少了0.36%、1.076%和1.74%,最高气温(1996-2009)分别增加了0.55%、2.32%和4.6%,最低气温(2010-2023)、(2024-2037)和(2038-2050)分别增加了0.83%、2.80%和8.54%。结果表明:受气候变化影响,1996-2009年、2010-2023年、2024-2037年、2038-2050年的平均年产水量分别为4634.07 Mm3、4525.92 Mm3、4456.20 Mm3和4411.89 Mm3。一般来说,随着研究区气温的升高,降雨量会减少,这直接影响到出水量。
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Assessment of Surface Water Resources in Case of Muger Sub Basin, Ethiopia
Water resources assessment (WRA) is the process of measuring, collecting and analysing relevant parameters on the quantity and quality of water resources for the purposes of a better development and management of water resources. The aim of this research is Assessment of Surface Water Resource in Case of Muger Sub Basin in Ethiopia. The future possible local climate variables are extracted from Abbay basin RCM and then the bias-corrected with observed meteorological variables which are then used as input to the soil and water assessment tool (SWAT) model as climate data, in addition to climate data soil data, land use land cover, slope of the sub basin and weather Generator together are used to simulate future water yield of Muger sub-basin. Soil and Water Assessment Tool (SWAT) was adopted to perform runoff simulation. The good performance of the SWAT model was confirmed, with a Nash-Sutcliffe efficiency (NSE) and determination coefficients (R2) of 0.76 and 0.99 respectively during calibration for monthly runoff, Nash-Sutcliffe efficiency (NSE) 0.63 and determination coefficients (R2) 0.99 respectively during validation for monthly runoff. The variation of precipitation in Muger sub basin decreased by (2010-2023), (2024-2037) and (2038-2050) from base period (1996-2009) will be 0.36%, 1.076% and 1.74% respectively, Maximum Temperature in sub basin increase from base period (1996-2009) by 0.55%, 2.32% and 4.6% and also minimum temperature in Muger sub basin increase by (2010-2023), (2024-2037) and (2038-2050) from base period (1996-2009) was 0.83%, 2.80 and 8.54% respectively. From this study, it was observed that due to climate change Average annual water yieldin Mugersub basinin (1996-2009), (2010-2023), (2024-2037), (2038-2050) is 4634.07 Mm3, 4525.92 Mm3, 4456.20 Mm3 and 4411.89 Mm3 respectively. Generally as Temperature increase in the study area the amount of rainfall decreases which directly affect the amount of water yield.
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