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Analysis of Spatio-temporal Characteristics and Regional Frequency of Droughts in the Southern Peninsula of India

机译:印度南部半岛干旱的时空特征和区域频率分析

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A detailed regional drought study is carried out in the southern peninsula of India to characterize the spatio-temporal nature of droughts and to predict the drought magnitudes for various probabilities in the homogeneous drought regions. The method of several random initializations of the cluster centres of the K-means algorithm is suggested for the identification of the initial regions in the context of drought regionalization, which is shown to perform better than the initialization from the Ward's algorithm and the Ward's algorithm itself. The peninsula is classified into seven spatially well-separated homogeneous drought regions. The robust L-moment framework is used for the regional frequency analysis of drought magnitudes computed using the standardized precipitation index. The Pearson type III is found to be appropriate for regional drought frequency analysis in six of the regions, while the robust Wakeby distribution is suggested for one region. Low magnitude droughts are frequent and dominant in the northern part of west coast, the north-eastern coast and its adjoining inland region, while high magnitude droughts are less in number and are experienced in semi-arid central part, southern part of western coast, south-eastern part and north-western inland region. The spatial maps of drought magnitudes indicate that at higher return periods (100 and 200 years) the south-eastern part of the peninsula is likely to encounter high magnitude droughts, while the central region is likely to experience the same at lower return periods (10 and 50 years). Hence these regions need to be given special importance in the drought mitigation planning activities.
机译:在印度南部半岛进行了详细的区域干旱研究,以表征干旱的时空特征,并预测均匀干旱地区各种概率的干旱幅度。建议在干旱区域化的背景下,对K-means算法的聚类中心进行几次随机初始化的方法来识别初始区域,该方法表现出比Ward算法和Ward算法本身更好的初始化效果。半岛被分为七个空间上分开的均匀干旱地区。鲁棒的L矩框架可用于使用标准化降水指数计算的干旱强度区域频率分析。发现Pearson III型适用于六个区域中的区域干旱频率分析,而建议在一个区域中使用鲁棒的Wakeby分布。在西海岸的北部,东北海岸及其毗邻的内陆地区,低强度干旱是常见且占主导地位的;而高强度干旱的数量较少,且在西海岸南部的半干旱中部地区较为常见,东南部和西北内陆地区。干旱幅度的空间图表明,在较高的回归期(100年和200年),半岛的东南部可能会遇到高强度干旱,而中部地区在较低的回归期可能会经历相同的干旱(10)。和50年)。因此,这些地区在减灾计划活动中需要特别重视。

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