Water Balance Evaluation for Flood Risk Reduction in the Yala River Basin, Western Kenya

Mary Kiluva, Wanyonyi E.S, Wakhungu J.W
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Abstract

The Yala River Basin (YRB) in Western region of Kenya has in the past experienced climate and weather extreme events that include floods. Floods have triggered loss of lives, destruction of property, outbreak of water borne diseases and siltation of arable land. This study utilized the Nedbør-Afstrømnings-Model (NAM) hydrologic model (available in the NAM Module of the MIKE 11 hydrodynamic model) on the Yala River Basin (YRB) to generate flood flows for water balance evaluation. The study utilized satellite imagery data for the period 1984-2010 sourced from the Regional Centre for Mapping of Resources for Development, rainfall (1980-2012) and river discharge (1947-2012) data sets from the Kenya Meteorological Department (KMD) and the Water Resources Management Authority (WARMA), respectively. Data quality control was statistically checked before sensitivity analysis, calibration, validation, and simulation of the flood flows. Daily water balance estimates for the Yala River Basin (YRB) over the period 1980-2010 were developed using the NAM hydrologic model. The results indicate that the mapped flood area extent varied by a value of 34.23 km2 over the period 1980-2010. The Yala River Basin (YRB) indicated an estimated inflow value of 4,814.72 MCM and outflow value of 4,578.23 MCM, with a coefficient of determination of 0.867. The difference between the inflow and outflow values was 236.49 MCM, that formed the flood flow or the water balance. This study concluded that the water balance value of 236.49 MCM was responsible for the floods recorded in the Yala River Basin (YRB) for the period 1980-2010, and it should be taken care of through flood risk reduction initiatives.
肯尼亚西部雅拉河流域减少洪水风险的水平衡评价
肯尼亚西部地区的亚拉河流域(YRB)过去曾经历过包括洪水在内的气候和天气极端事件。洪水造成了生命损失、财产破坏、水传播疾病的爆发和可耕地的淤积。本研究利用Nedbør-Afstrømnings-Model (NAM)水文模型(可在MIKE 11水动力模型的NAM模块中使用)对雅拉河流域(YRB)进行洪水生成,用于水平衡评价。该研究利用了1984-2010年期间的卫星图像数据,这些数据分别来自肯尼亚气象部门(KMD)和水资源管理局(WARMA)的降水(1980-2012)和河流流量(1947-2012)数据集。在敏感性分析、校准、验证和洪水流量模拟之前,对数据质量控制进行统计检查。利用NAM水文模型对雅拉河流域1980-2010年的日水量平衡进行了估算。结果表明:1980—2010年,洪涝区面积变化34.23 km2。雅拉河流域预计入水量为4814.72 MCM,出水量为4578.23 MCM,决定系数为0.867。流入与流出值之差为236.49 MCM,形成洪水流量或水量平衡。研究认为,雅拉河流域1980—2010年汛期洪水发生的主要原因是236.49 MCM的水平衡值,应通过防洪减灾措施加以控制。
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