海河流域严重干旱500hPa信号场异常信号分析
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NULL

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严小林 (1987-),女,湖南娄底人,博士,主要从事水文气象方面研究。 E-mail:yanxl5566@126.com

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P333

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国家973重点基础研究发展计划项目(2010CB951103);国家十二五科技支撑计划项目(2012BAC21B01,2012BAC19B03);水利部公益性行业专项经费资助项目(200801001,201101015);


Anomalies of 500hPa Signal Field during Meteorological Droughts in Haihe River Basin
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    摘要:

    基于严重少雨旬的定义,分析海河流域19612009年严重少雨旬的分布特征,进而对汛期40个典型严重少雨旬的500hPa信号场进行经验正交分解(EOF分析)。结果表明:EOF第一模态的方差贡献率达到35.3%,远高于其他模态;第一模态呈现出2个负异常区和1个正异常区,在对应的环流背景下,海河流域受暖性高压控制,高纬冷空气及低纬暖湿气流难以到达流域上空交绥,持续高温少雨造成流域严重干旱。

    Abstract:

    Based on the definition and analysis of 10-day precipitation drought events, the anomalies of the 500hPa signal field duringmeteorological droughts in the Haihe River Basin were investigated with 40 10-day precipitation drought events from 1961 to 2009, usingempirical orthogonal function analysis. The results showed that the relative variance contribution of the first mode is 35.3%, much higherthan those of other modes; and there are three abnormal areas in the 500hPa signal field: two negative ones and a wide stretches of positiveone. The abnormal spatial pattern of soohPa signal field meant that the Haihe River Basin is under the control of warm high, and the coldair and warm air can not meet over it, which would cause severe drought in the Haihe River Basin eventually.

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  • 收稿日期:2011-12-30
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  • 在线发布日期: 2022-06-17
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