高原渦與西南渦相互作用暴雨天氣過程的診斷分析
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國家自然科學基金項目(40775032)資助


Diagnostic Analysis of Vorticity in a Heavy Rain Event under Interaction of Plateau Vortex and Southwest Vortex
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    摘要:

    利用動力診斷方法,對2008年7月20~22日高原低渦與低層西南低渦相互作用引發西南低渦強烈發展和四川大面積特大暴雨天氣發生機理進行了診斷分析。分析表明:高原渦與西南渦渦心之間的緯向距離在5個緯度的時候,兩者上升氣流都在500 hPa以下,當兩者繼續東移,在經向上耦合的時候,二者同時得到發展,西南渦中心的上升氣流達到300 hPa,而高原渦中心的上升氣流突破200 hPa;西南渦在低層出現初期,在一定程度上制約了高原渦的發展,隨著兩者在經向方向發生耦合,上下渦度平流不同造成垂直差動,將激發500 hPa以下的上升運動與氣旋性渦度加強,使得500 hPa與700 hPa渦心正渦度值的增大近 1倍 。并且渦前的正渦度變率使得高原渦發展并東移,待垂直耦合后,高原渦與盆地渦相互強迫作用促使氣流上升運動加強也是導致高原低渦與西南低渦共同發展的一種機制。

    Abstract:

    With the momentum diagnosis method, an analysis is made of the interaction between plateau vortex and southwest vortex during a heavy rain event in Sichuan on 20 to 22 July 2008. The results show that when the latitudinal distance between plateau vortex center and southwest vortex center was 5°, the updrafts in both vortexes were confined within 500 hPa; when moved eastward and coupled longitudinally, they both developed, with the updraft of the southwest vortex center reached 300 hPa and that of the plateau vortex center reached 200 hPa. The southwest vortex restricted the development of the plateau vortex in some way at the early stage when it appeared in the lower atmosphere. When they were coupled longitudinally, the vertical difference caused by the different vorticity advections between the upper and lower levels excitated the updrafts under 500 hPa and strengthened cyclone vorticity, and then the positive vorticity at 500 hPa and 700 hPa increased by two times The change rate of positive vorticity facilitated the plateau vortex to move eastward. After coupled longitudinally, the interaction of the plateau vortex and basin vortex strengthened the updrafts. As a result, the plateau vortex and southwest vortex influenced each other and developed together.

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周春花,顧清源,何光碧.高原渦與西南渦相互作用暴雨天氣過程的診斷分析[J].氣象科技,2009,37(5):538~544

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  • 收稿日期:2008-10-30
  • 定稿日期:2009-03-26
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