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Regional extreme‐dry‐spell frequency analysis using the L‐moments method in the middle reaches of the Yellow River Basin, China

机译:黄河中游地区采用L矩法的区域极端干拼频率分析

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摘要

In this research, the regional extreme-dry-spell frequency in the middle reaches of the Yellow River Basin (YRB) is studied by the L-moments method. The research area has been divided into three subregions (regions 1, 2 and 3), which have been identified as homogenous regions. The results of a goodness-of-fit test indicate that a generalized normal distribution is the optimal regional model for regions 1 and 2 whereas a generalized Pareto distribution is the optimal regional model for region 3. The return period analysis figures out that the maximum length-of-dry-spell (MxDS) values increase from south to north in the southern part and increase from northeast to southwest in the northern part of the middle reaches of the YRB under different return periods. The increments of quantiles of dry spell under different return levels indicate that drought risk in region 1 is higher than that in regions 2 and 3. The analysis of the occurrence day of MxDS shows that MxDS mostly occurred during winter of 1998 and spring of 1999 in most stations during the considered period. By comparing summer MxDS events, it can be found that mean MxDS values have slightly increased in regions 1 and 2 during the last five decades. The maximum mean MxDS values appeared in the 2000s for regions 1 and 2 and in the 1990s for region 3. The atmospheric circulation shows that the positive anomaly centre in the west of North China, negative anomaly centre in the east of North China and the strong western Pacific subtropical high led to the decrease of precipitation in North China during the summer of 1997. Copyright © 2013 John Wiley & Sons, Ltd.
机译:本文采用L-矩法研究了黄河流域中游地区的极端干散频率。研究区域被划分为三个子区域(区域1、2和3),这三个区域被确定为同质区域。拟合优度检验的结果表明,广义正态分布是区域1和2的最佳区域模型,而广义Pareto分布是区域3的最佳区域模型。回报期分析表明,最大长度在不同回报期,YRB中游地区的干法(MxDS)值从南到北增加,在东北部的北部从东北到西南增加。在不同回报水平下干法分位数的增加表明1区的干旱风险高于2区和3区。对MxDS发生日的分析表明,MxDS主要发生在1998年冬季和1999年春季。在考虑期间内的大多数电台。通过比较夏季的MxDS事件,可以发现在过去的50年中,区域1和2的平均MxDS值略有增加。最大平均MxDS值出现在2000年代的1区和2区,以及1990年代的3区。大气环流显示华北西部的正异常中心,华北东部的负异常中心和强华北地区。西太平洋副热带高压导致1997年夏季华北地区的降水减少。版权所有©2013 John Wiley&Sons,Ltd.。

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    Institute of Geographic Sciences and Natural Resources Research CAS Key Laboratory of Water Cycle and Related Land Surface Processes Beijing China. University of Chinese Academy of Sciences Beijing China. Wuhan University State Key Laboratory of Water Resources and Hydropower Engineering Science Wuhan China;

    Institute of Geographic Sciences and Natural Resources Research CAS Key Laboratory of Water Cycle and Related Land Surface Processes Beijing China. Wuhan University State Key Laboratory of Water Resources and Hydropower Engineering Science Wuhan China;

    Institute of Geographic Sciences and Natural Resources Research CAS Key Laboratory of Water Cycle and Related Land Surface Processes Beijing China. University of Chinese Academy of Sciences Beijing China;

    Beijing Normal University College of Global Change and Earth System Science Beijing China;

    International Water Management Institute Colombo Sri Lanka;

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  • 正文语种 eng
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  • 关键词

    regional frequency analysis; L‐moments method; extreme dry spell; Yellow River Basin;

    机译:区域频率分析;L矩法;极端干旱;黄河流域;

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