“環(huán)高”熱帶風(fēng)暴登陸后路徑分析及其對(duì)遼寧暴雨影響

doi:10.3969/2012jms.00**

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“環(huán)高”熱帶風(fēng)暴登陸后路徑分析及其對(duì)遼寧暴雨影響
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                        10.3969/2012jms.00**
                    
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中圖分類號(hào):P457.8
基金項(xiàng)目:中國(guó)氣象局新技術(shù)推廣項(xiàng)目(CMATG2006Y02)

Analysis of the path of “Huangao” tropical storm and its contribution to the regional rainstrom in Liaoning

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2003年第11號(hào)熱帶風(fēng)暴“環(huán)高”在浙江省南部登陸后強(qiáng)度迅速減弱，但其殘余云系及水汽仍然繼續(xù)北上，為遼寧8月22—23日區(qū)域性暴雨提供了動(dòng)力、熱力、水汽及充分的能量。本文在分析熱帶氣旋維持、北上條件的基礎(chǔ)上，對(duì)此次暴雨的成因和物理量進(jìn)行分析，指出北上熱帶氣旋攜帶的暖濕空氣為暴雨提供了熱力條件；熱帶氣旋北上使低空偏南急流加強(qiáng)并維持，為暴雨提供了必要的動(dòng)力條件；熱帶氣旋為這次暴雨過(guò)程提供了充足的能量；熱帶氣旋是這次暴雨過(guò)程重要水汽來(lái)源。

Abstract:

The intensity of tropical storm weakened quickly after its landing in 2002. But the remaining cloud system and water vapor kept going northward. In this way, momentum, heat, water vapor and abundant energy were supplied for the regional rainstorm happened during 22—23 August in Liaoning. The weather condition under which the tropical cyclone was sustained and moved northward is analysed. Through studying the cause of the rainstorm and doing diagnosis for the corresponding variables, this paper points out the following conclusions. The northward moving tropical cyclone brought the warm and moist air, which is in favor of the thermal conditions for the rainstorm. Low level southern jet was built up earlier and lasted for a longer time because of the northward moving of the tropical cyclone. This change in low level jet provided the dynamic conditions. The energy and water vapor of this rainstorm are supplied by the tropical cyclone.

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孫欣,陳傳雷.“環(huán)高”熱帶風(fēng)暴登陸后路徑分析及其對(duì)遼寧暴雨影響.氣象科學(xué),2009,(4):536-540 Sun Xin, Chen Chuanlei. Analysis of the path of “Huangao” tropical storm and its contribution to the regional rainstrom in Liaoning. Journal of the Meteorological Sciences,2009,(4):536-540

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