气象科学
氣象科學
기상과학
SCIENTIA METEOROLOGICA SINICA
2010年
2期
250-255
,共6页
暴雨%西南急流%不稳定能量%数值模拟
暴雨%西南急流%不穩定能量%數值模擬
폭우%서남급류%불은정능량%수치모의
Rainfall Southwestern jet Unstable energy Numerical simulation
用NCEP/NCAR全球逐日再分析格点资料和广西区域日降水资料,对2008年6月12-13日发生在广西的持续性暴雨过程进行了诊断分析,并利用中尺度数值模式WRF进行了数值模拟研究.结果表明:暴雨过程的水汽来源主要为孟加拉湾南部和南海北部;在强降水期间,暴雨区上空低层为较强的大气层结不稳定区,中高层为大气层结相对稳定区,不稳定能量与降水强度有着很好的对应关系;西南急流作为对流系统上升的触发机制,为广西持续性暴雨过程的发生和发展提供了水汽条件和动力条件.WRF模式成功模拟出本次暴雨过程的大尺度环流形势的演变及中尺度降雨分布,本次暴雨与850 hPa上一个β中尺度低涡的生成和强烈发展直接关联.
用NCEP/NCAR全毬逐日再分析格點資料和廣西區域日降水資料,對2008年6月12-13日髮生在廣西的持續性暴雨過程進行瞭診斷分析,併利用中呎度數值模式WRF進行瞭數值模擬研究.結果錶明:暴雨過程的水汽來源主要為孟加拉灣南部和南海北部;在彊降水期間,暴雨區上空低層為較彊的大氣層結不穩定區,中高層為大氣層結相對穩定區,不穩定能量與降水彊度有著很好的對應關繫;西南急流作為對流繫統上升的觸髮機製,為廣西持續性暴雨過程的髮生和髮展提供瞭水汽條件和動力條件.WRF模式成功模擬齣本次暴雨過程的大呎度環流形勢的縯變及中呎度降雨分佈,本次暴雨與850 hPa上一箇β中呎度低渦的生成和彊烈髮展直接關聯.
용NCEP/NCAR전구축일재분석격점자료화엄서구역일강수자료,대2008년6월12-13일발생재엄서적지속성폭우과정진행료진단분석,병이용중척도수치모식WRF진행료수치모의연구.결과표명:폭우과정적수기래원주요위맹가랍만남부화남해북부;재강강수기간,폭우구상공저층위교강적대기층결불은정구,중고층위대기층결상대은정구,불은정능량여강수강도유착흔호적대응관계;서남급류작위대류계통상승적촉발궤제,위엄서지속성폭우과정적발생화발전제공료수기조건화동력조건.WRF모식성공모의출본차폭우과정적대척도배류형세적연변급중척도강우분포,본차폭우여850 hPa상일개β중척도저와적생성화강렬발전직접관련.
A diagnostic analysis and numerical simulation of persistent heavy rainfall in Guangxi is performed by using the daily precipitation data of Guangxi area and the NCEP/NCAR reanalysis daily data and the mesoscale model WRF.The results show that moisture came mainly from the south of Bengal and north of south China sea. There is the unstable stratification at low level while the relative stable stratification at middle and high levels over the rainfall area and there is a good relationship between the unstable energy and rain rate.As a trigger mechanism of the increase of convective system,the southwestern jet provided the occurrence and progression of the persistent heavy rainfall water vapor and dynamic condition. WRF model could successfully simulate the changing of large scale circulation and the distribution of meso-β scale rainband. This persistent heavy rainfall is in direct relationship with the genesis and intensive development of a mesoscale low vortex at 850 hPa.