气象与环境科学
氣象與環境科學
기상여배경과학
METEOROLOGICAL AND ENVIRONMENTAL SCIENCES
2012年
1期
26-31
,共6页
持续性%强降雨%成因%高低空急流%垂直环流
持續性%彊降雨%成因%高低空急流%垂直環流
지속성%강강우%성인%고저공급류%수직배류
persistence%heavy rainfall%cause%upper-low level jet%vertical circulation
利用常规气象资料和NCEP再分析资料,从前期天气背景、大气环流演变及产生持续性强降雨的动力、热力和水汽等条件,分析了2008年6月广西出现的一次持续性强降雨过程。结果发现:这次持续性强降雨过程期间,500hPa环流形势稳定,高空西风小槽呈阶梯状持续下滑影响广西,不断诱发暴雨出现;200hPa广西处于南亚高压东部脊区和高空西风急流出口区右方,风速辐散明显,在高低空急流耦合作用下,华南出现了正反两支垂直环流,广西上空辐合上升运动明显,为强降雨的出现提供了极好的动力条件;南海季风暴发和副热带高压在华南沿海的稳定维持,使得华南低空形成了印度洋和南海两吏水汽通道,为暴雨区上空提供了源源不断的水汽;高温、高湿、高能的热力条件,有利于扰动的形成和对流不稳定能量产生,为广西持续性暴雨提供了必要的能量条件。
利用常規氣象資料和NCEP再分析資料,從前期天氣揹景、大氣環流縯變及產生持續性彊降雨的動力、熱力和水汽等條件,分析瞭2008年6月廣西齣現的一次持續性彊降雨過程。結果髮現:這次持續性彊降雨過程期間,500hPa環流形勢穩定,高空西風小槽呈階梯狀持續下滑影響廣西,不斷誘髮暴雨齣現;200hPa廣西處于南亞高壓東部脊區和高空西風急流齣口區右方,風速輻散明顯,在高低空急流耦閤作用下,華南齣現瞭正反兩支垂直環流,廣西上空輻閤上升運動明顯,為彊降雨的齣現提供瞭極好的動力條件;南海季風暴髮和副熱帶高壓在華南沿海的穩定維持,使得華南低空形成瞭印度洋和南海兩吏水汽通道,為暴雨區上空提供瞭源源不斷的水汽;高溫、高濕、高能的熱力條件,有利于擾動的形成和對流不穩定能量產生,為廣西持續性暴雨提供瞭必要的能量條件。
이용상규기상자료화NCEP재분석자료,종전기천기배경、대기배류연변급산생지속성강강우적동력、열력화수기등조건,분석료2008년6월엄서출현적일차지속성강강우과정。결과발현:저차지속성강강우과정기간,500hPa배류형세은정,고공서풍소조정계제상지속하활영향엄서,불단유발폭우출현;200hPa엄서처우남아고압동부척구화고공서풍급류출구구우방,풍속복산명현,재고저공급류우합작용하,화남출현료정반량지수직배류,엄서상공복합상승운동명현,위강강우적출현제공료겁호적동력조건;남해계풍폭발화부열대고압재화남연해적은정유지,사득화남저공형성료인도양화남해량리수기통도,위폭우구상공제공료원원불단적수기;고온、고습、고능적열력조건,유리우우동적형성화대류불은정능양산생,위엄서지속성폭우제공료필요적능량조건。
Based on the weather background, atmospheric circulation evolution and the meteorologi- cal conditions, including dynamic, thermodynamic, water vapor and so on conditions, the persistent torrential rain weather in Guangxi in June of 2008 is examined by using the observation data and NCEP reanalysis data. The results showed that during the course of the continuous heavy rainfall, 500 hPa circu-lation situation stable, high-altitude westerly trough continued deeline as a ladder and influence Guangxi, which constantly evoked heavy rainfall. The high-level wind speed dispersed in Guangxi at 200 hPa be- cause of Guangxi lied to the eastern ridge of high pressure zone in South Asia and exports of upper-level westerly jet right areas. Because of the reciprocity of the upper-low level jet, Southern China generatedpositive and negative of two vertical circulation and Guangxi converged ascending motion, which provided excellent dynamic force of heavy rainfall. The eruption of the South China Sea monsoon and the stably maintaining in low-altitude southern China of the subtropical high-pressure system offered water vapor continuously, which formed the Indian Ocean and the South China Sea two water vapor channels. In ad- dition, the high temperature and high humidity and high energy are the necessary thermal energy condi- tions for the generation of continuous heavy rain in Guangxi, which is propitious to the development and the generation of convective instability energy.