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A new precipitation index for the spatiotemporal distribution of drought and flooding in the reaches of the Yangtze and Huaihe Rivers and related characteristics of atmospheric circulation

机译:江淮流域旱涝时空分布的新降水指数及大气环流特征。

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摘要

Characteristics of the spatiotemporal distributions of precipitation anomalies in the reaches of the Yangtze River and Huaihe River (YHR) were studied using EOF method. Four main precipitation patterns for the YHR in summer identified by the first two modes: a region-wide flood over the entire YHR (RWF); a region-wide drought over the entire YHR (RWD); a flood in the south with a drought in the northern region of the Yangtze River (FS-DN); and a drought in the south with a flood in the northern region of the Yangtze River (DS-FN). Based on the first two modes and the actual precipitation departure percentage, a new precipitation index is defined in this paper. The typical flood/drought years associated with the various rainfall patterns defined by this precipitation index are more representative and closer to reality compared to some existing precipitation indexes which just use the area-mean precipitation or the EOF time components individually.
机译:利用EOF方法研究了长江和淮河地区降水异常的时空分布特征。前两个模式确定了YHR夏季的四种主要降水模式:整个YHR的区域性洪水;整个YHR(RWD)发生了区域性干旱;南部洪水,长江北部地区干旱(FS-DN);南部干旱,长江北部地区洪水泛滥(DS-FN)。基于前两种模式和实际降水偏离率,确定了一种新的降水指数。与一些仅使用面积平均降水量或EOF时间分量的现有降水量指标相比,与该降水量指标定义的各种降雨模式相关的典型洪水/干旱年份更具代表性,并且更加接近实际。

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