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Mapping floods in the middle Zambezi Basin using earth observation and hydrological modeling techniques

机译:使用地球观测和水文建模技术在中间的ZAMBEZI盆地中绘制洪水

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The Lower Middle Zambezi catchment, on the Zimbabwean side, is vulnerable to floods almost every year. In this work, the causes and impacts of floods in the Mbire District of the Middle Zambezi Basin are investigated. An algorithm based on the binary logistic regression is used together with MODIS NDVI images to determine the spatial and temporal variation of flood inundation. The HEC-HMS model is used to simulate rainfall time series at daily time step. The quantified peak flow is given as an input to a mono-dimensional hydraulic model, HEC-RAS. Results from the mapped inundated areas for the period 2005 to 2015 showed that 16 January 2006 had the highest flooded area of 1934 km(2). Factors explaining causes of flooding were distance from surface water bodies. The simulated flooded areas obtained are used to deepen our understanding of the contribution of geomorphic features towards flooding as well as the extent of flooding. Results obtained contribute towards defining new strategies for prompt flood risk management in the District.
机译:在津巴布韦侧的下层中间的Zambezi集水区几乎每年都容易受到洪水。在这项工作中,调查了ZAMBEZI盆地MBire区洪水的原因和影响。基于二进制逻辑回归的算法与MODIS NDVI图像一起使用,以确定洪水淹没的空间和时间变化。 HEC-HMS模型用于在日常时间步骤模拟降雨时间序列。量化的峰值流量作为单维液压模型的输入给出,HEC-RAS。 2005年至2015年期间的映射淹没区域的结果表明,2006年1月16日拥有1934公里的最高洪水(2)。解释洪水原因的因素是从地表水体的距离。获得的模拟洪水地区用于加深我们对地貌特征对洪水的贡献以及洪水程度的理解。结果有助于确定该区迅速洪水风险管理的新战略。

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