气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2012年
2期
54-59
,共6页
舟曲特大暴雨%WRF模式%数值模拟%诊断分析
舟麯特大暴雨%WRF模式%數值模擬%診斷分析
주곡특대폭우%WRF모식%수치모의%진단분석
Severe rainstorm in Zhouqu%WRF model%Numeric simulation%Diagnostic analysis
利用NCEP每6 h 1次的1°×1°格点资料和中尺度模式WRF(V3.2),对2010年舟曲"0808"特大泥石流暴雨天气进行了数值模拟,运用模式输出资料对此次天气过程发生发展的机制进行了诊断分析。结果表明:舟曲强暴雨发生在高原短波槽、低涡切变线和副热带高压等共同作用的有利天气形势下,三重嵌套的WRF模式对此次暴雨具有良好的模拟能力。低层强辐合、中层无辐散和高层强辐散的配置,以及强烈的上升运动是此次暴雨发生的主要动力条件。从低层向上延伸的等θse线高能舌和水平风垂直切变为暴雨的发生输送了大量的不稳定能量。中低层水汽辐合上升为暴雨的发生创造了有利的水汽条件。
利用NCEP每6 h 1次的1°×1°格點資料和中呎度模式WRF(V3.2),對2010年舟麯"0808"特大泥石流暴雨天氣進行瞭數值模擬,運用模式輸齣資料對此次天氣過程髮生髮展的機製進行瞭診斷分析。結果錶明:舟麯彊暴雨髮生在高原短波槽、低渦切變線和副熱帶高壓等共同作用的有利天氣形勢下,三重嵌套的WRF模式對此次暴雨具有良好的模擬能力。低層彊輻閤、中層無輻散和高層彊輻散的配置,以及彊烈的上升運動是此次暴雨髮生的主要動力條件。從低層嚮上延伸的等θse線高能舌和水平風垂直切變為暴雨的髮生輸送瞭大量的不穩定能量。中低層水汽輻閤上升為暴雨的髮生創造瞭有利的水汽條件。
이용NCEP매6 h 1차적1°×1°격점자료화중척도모식WRF(V3.2),대2010년주곡"0808"특대니석류폭우천기진행료수치모의,운용모식수출자료대차차천기과정발생발전적궤제진행료진단분석。결과표명:주곡강폭우발생재고원단파조、저와절변선화부열대고압등공동작용적유리천기형세하,삼중감투적WRF모식대차차폭우구유량호적모의능력。저층강복합、중층무복산화고층강복산적배치,이급강렬적상승운동시차차폭우발생적주요동력조건。종저층향상연신적등θse선고능설화수평풍수직절변위폭우적발생수송료대량적불은정능량。중저층수기복합상승위폭우적발생창조료유리적수기조건。
Based on the NCEP 1°×1° data with 6 h interval and the meso-scale WRF(V3.2) model,the physical mechanism of severe rainstorm caused by debris flow disaster on August 8,2010 was diagnosed.The results indicated that the severe rainstorm happened under the common action of short-wave trough at high altitudes,low vortex with shear line,the subtropical high and so on.The triple nested WRF model has simulated this rainstorm event quite well.The prime dynamic conditions of this process include strong convergence in the lower level,non-divergence in the middle level and strong divergence in the upper level as well as strong ascending motion.A lot of instability energy that rainstorm needs is transported by vertical wind shear and high energy tongue of pseudo equivalent potential temperature(θse) isoline which extends upward from the lower level.Convergence of water vapor in the middle and lower levels is favorable to rainstorm occurrence.