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首页> 外文期刊>Aceh International Journal of Science and Technology >Modeling Hydrologic Response to Land Use and Climate Change in the Krueng Jreu Sub Watershed of Aceh Besar
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Modeling Hydrologic Response to Land Use and Climate Change in the Krueng Jreu Sub Watershed of Aceh Besar

机译:亚齐贝萨尔省Krueng Jreu小流域对土地利用和气候变化的水文响应建模

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摘要

Soil and Water Assessment Tool (SWAT) model was used to simulate impact of landuse and climate change on water resources in Krueng Jreu subwatershed located in Aceh Province – Indonesia. The subwatershed is a primary source of water to irrigated 233.52 km2 paddy field area through a surface irrigation system. The model performance was considerably good in predicting streamflow. The coefficients of determination varied between 0.58 and 0.72, while the Nash-Sutcliffe coefficients (ENS) ranged between 0.65-0.72 and the percentage bias were in the range of -0.36 to 2.30. Scenarios were applied to the best fit model to evaluate watershed responses to land use and climate changes. The model predicted increases in both runoff and water yield by 1% and 0.1% respectively as the result of increasing 15% settlement area. When all agricultural land within subwatershed converted to forest, water yield would increase by 1% during dry period and runoff contribution would decrease by 5%. Increases in surface flow by 23.6% and water yield by 15.1% were found under scenario of increasing 10% of daily precipitation. Increasing in evapotranspiration caused by an increase of 1.5?C in daily air temperature would decrease surface flow and water yield by 0.8% and 1.3%, respectively. Combination scenarios of changes in daily temperature and precipitation would increase evapotranspiration rate, annual water yield and runoff contribution.
机译:土壤和水评估工具(SWAT)模型用于模拟印度尼西亚亚齐省Krueng Jreu小流域的土地利用和气候变化对水资源的影响。该小流域是通过地面灌溉系统灌溉233.52 km2稻田面积的主要水源。在预测流量方面,模型性能相当好。测定系数在0.58至0.72之间变化,而纳什-萨克利夫系数(ENS)在0.65-0.72之间变化,偏差百分比在-0.36至2.30之间。将方案应用于最佳拟合模型,以评估流域对土地利用和气候变化的响应。该模型预测,由于增加15%的沉降面积,径流量和水产量分别增加1%和0.1%。如果该小流域内的所有农业用地都转化为森林,则干旱时期的水产量将增加1%,径流贡献将减少5%。在每日降水增加10%的情况下,发现地表流量增加了23.6%,水产率增加了15.1%。每天气温升高1.5?C引起的蒸散量的增加将分别使地表流量和水产率降低0.8%和1.3%。日温度和降水量变化的综合情景将增加蒸散量,年产量和径流贡献。

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