江淮流域持續性暴雨過程前期環流特征
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Preceding Atmospheric Circulation Characteristics of Persistent Heavy Rainfall in Yangtze and Huaihe River Basin
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    摘要:

    利用NCEP逐日再分析資料,通過合成分析以及滑動平均的低通濾波效果分析在江淮地區持續性暴雨過程發生前的環流場特征。研究認為持續性暴雨過程前期環流特征主要有以下幾點:澳大利亞高壓強度變化幅度小,馬斯克林高壓強度變化幅度大,兩者之間呈現此消彼長的關系;副熱帶高壓明顯比常年偏強,脊線平均位置偏南,西脊點平均位置偏西;南亞高壓屬于西部型,強度偏弱,東伸脊點偏東;南亞高壓的東伸脊點與副高的西伸脊點具有明顯的相向而行,相背而去的活動特征;副高脊線比南亞高壓脊線偏南4~6個緯距,并且兩者具有步調一致的南北移動,但是南亞高壓脊線移動時間比副高脊線提前1天左右。

    Abstract:

    The persistent heavy rainfall is a kind of extreme precipitation events that have a long duration, extensive coverage, and relatively stable heavy precipitation areas. Based on the daily averaged data derived from the NCEP/NCAR reanalysis dataset, the preceding signals in atmospheric circulation of persistent heavy rainfall events happened in the Yangtze and Huaihe River Basin in June are revealed by using the moving average analysis and composite methods. The results suggest that Australia high and the Mascarene high has a relation of “seesaw”; the subtropical high is obviously stronger than usual; the average position of the ridge line is farther south, and the average position of the west ridge point is farther west; the South Asia high,belonging to the west type high,is weaker, and the eastward stretch ridge point is farther east; the eastward stretch ridge point of the South Asia high and the westward stretch ridge point obviously come toward each other and goes away from each other; the ridge line of the subtropical high is 4 to 6 latitude distances farther south that that of the South Asia high, and they have concerted north south movement, but the movement of the ridge line of the South Asia high is about one day later than that of the ridge line of the subtropical high.

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朱科,張文娟.江淮流域持續性暴雨過程前期環流特征[J].氣象科技,2012,40(3):423~427

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  • 收稿日期:2010-10-22
  • 定稿日期:2011-04-15
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  • 在線發布日期: 2012-05-31
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