廣東罕見特大致洪暴雨形成機理個例分析
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廣東省氣象課題(200526)資助


Formation Mechanism Analysis of a FloodInducing Heavy Rain in Guangdong Province
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    摘要:

    利用常規觀測、雷達衛星和NCEP 1°×1°格點資料,從形勢場配置、水汽供應、動力機制等方面對廣東罕見特大暴雨的形成機理進行診斷分析。結果表明:西太平洋副高位置偏南,強度偏弱,副高北側的西南暖濕氣流與西風槽前的冷空氣共同作用是此次特大致洪暴雨形成的重要原因;強盛低空急流為暴雨過程提供了充沛的水汽;高層輻散低層輻合激發強烈上升運動;特大暴雨過程中垂直螺旋度量級(10-6hPa·s-2)比常規(10-8h Pa·s-2)大2個量級,其正值區長軸與700 hPa的切變輻合線走向和移動方向一致;廣東暴雨范圍和量級增大期間,其上空垂直螺旋度具有中低層正、高層負螺旋度閉合中心向低層明顯傳送的特征。

    Abstract:

    The mechanism analysis of a floodinducing heavy rainfall occurred in June 2005 Guangdong Province is diagnosed by analyzing the circulation situation, moisture, dynamical mechanism, vertical helicity, and so on based on the conventional observation data, radar echo, satellite image and NCEP grid data. The results show that the causes of the heavy rainfall include the farther south and weakerthannormal ridge position of the West Pacific subtropical high and the interaction between the southwest warm and wet airflow to the north of the subtropical high and the cold air in front of the westerly trough; the lowlevel jet stream provides enough moisture; the divergence in high level and the convergence in low level resulted in strong updraft; the vertical helicity is two orders of magnitude greater than normal with the long axis of the positive vertical helicity area having the same direction with the movement of the shear convergence line on 700 hPa. During the heavy flooding rainfall, there was an enclosed negative center of vertical helicity at the middle level and an enclosed positive center at the upper level, spreading obviously down to the lower level.

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姜麗萍,尤紅,夏冠聰,黃靜,陳楨華.廣東罕見特大致洪暴雨形成機理個例分析[J].氣象科技,2007,35(3):374~378

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  • 收稿日期:2006-08-15
  • 定稿日期:2006-11-23
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