气象与减灾研究
氣象與減災研究
기상여감재연구
METEOROLOGY AND DISASTER REDUCTION RESEARCH
2014年
4期
24-32
,共9页
郭达烽%包慧濛%周芳%郑婧
郭達烽%包慧濛%週芳%鄭婧
곽체봉%포혜몽%주방%정청
台风%空心结构%暴雨%冷空气
檯風%空心結構%暴雨%冷空氣
태풍%공심결구%폭우%랭공기
typhoon%hollow structure%torrential rainfall%cold air
利用常规气象观测资料、NCEP再分析资料、雷达资料,从环流特征、水汽条件、动力条件以及冷空气侵入作用等方面,对2014年台风“麦德姆”登陆后的空心结构及其引发的7月24日德安县局部特大暴雨过程进行分析。结果发现,高层南亚高压东风急流形成的高空辐散流场的变化,以及下垫面和地形的影响导致了台风减弱为热带风暴,并出现空心结构;冷空气与热带风暴的东北象限发生作用,使热带风暴外围德安县附近大气垂直层结处于非常不稳定状态,地面中尺度辐合线的形成与维持,使低层辐合加强和对流加强,在东风急流带来充足的水汽辐合条件下引发了特大暴雨。
利用常規氣象觀測資料、NCEP再分析資料、雷達資料,從環流特徵、水汽條件、動力條件以及冷空氣侵入作用等方麵,對2014年檯風“麥德姆”登陸後的空心結構及其引髮的7月24日德安縣跼部特大暴雨過程進行分析。結果髮現,高層南亞高壓東風急流形成的高空輻散流場的變化,以及下墊麵和地形的影響導緻瞭檯風減弱為熱帶風暴,併齣現空心結構;冷空氣與熱帶風暴的東北象限髮生作用,使熱帶風暴外圍德安縣附近大氣垂直層結處于非常不穩定狀態,地麵中呎度輻閤線的形成與維持,使低層輻閤加彊和對流加彊,在東風急流帶來充足的水汽輻閤條件下引髮瞭特大暴雨。
이용상규기상관측자료、NCEP재분석자료、뢰체자료,종배류특정、수기조건、동력조건이급랭공기침입작용등방면,대2014년태풍“맥덕모”등륙후적공심결구급기인발적7월24일덕안현국부특대폭우과정진행분석。결과발현,고층남아고압동풍급류형성적고공복산류장적변화,이급하점면화지형적영향도치료태풍감약위열대풍폭,병출현공심결구;랭공기여열대풍폭적동북상한발생작용,사열대풍폭외위덕안현부근대기수직층결처우비상불은정상태,지면중척도복합선적형성여유지,사저층복합가강화대류가강,재동풍급류대래충족적수기복합조건하인발료특대폭우。
Using conventional weather data , NCEP reanalysis data and Nanchang Doppler radar data , the hollow structure of typhoon “Matmo” after its landing and local torrential rainfall occurred on July 24 2014 over De′an county in Jiangxi Province are analyzed in terms of circulation characteristics, vapor condition and the intrusion of cold air. The results showed that the hollow structure of typhoon “Matmo” was caused by the change of high-level divergence flow field from south Asia easterly jet , the underlying surface and the topography. The interactions between the cold air and the northeast circulation of typhoon greatly strengthened the atmosphere instability over De′an. The formation and maintenance of meso-scale convergence line led to intensify low-level convergence and strong convection. In addition , enough vapor convergence from easterly jet caused this heavy torrential rainfall.