气象科学
氣象科學
기상과학
SCIENTIA METEOROLOGICA SINICA
2009年
6期
727-733
,共7页
傅灵艳%寿绍文%黄亿%岳彩军
傅靈豔%壽紹文%黃億%嶽綵軍
부령염%수소문%황억%악채군
台风暴雨%非地转湿Q矢量%诊断分析%次级环流
檯風暴雨%非地轉濕Q矢量%診斷分析%次級環流
태풍폭우%비지전습Q시량%진단분석%차급배류
Typhoon rainstorm%Ageostrophic wet Q vector%Diagnostic analysis%Secondary circulation
利用WRF中尺度模式模拟了台风"圣帕"登陆后减弱成热带低压造成湖南省大暴雨的过程,使用模拟输出的高分辨率资料,借助非地转湿Q矢量对这次暴雨过程做了详细的诊断分析.结果表明:非地转湿Q矢量能比较清楚地揭示此次暴雨演变过程,尤其700 hPa的非地转湿Q矢量散度场对降水预报具有较好的指示意义,其散度辐合区域对应着降水的落区,散度辐合强度变化指示着降水强度的变化趋势,并且非地转湿Q矢量散度辐合强度的大小可预示着未来3~6 h降水的强弱,是具有预报价值的;非地转湿Q矢量散度是非地转ω方程的强迫项,并与地形条件共同作用激发了地面中尺度系统的发展与次级环流的形成,是此次暴雨得以发展与维持的机制.
利用WRF中呎度模式模擬瞭檯風"聖帕"登陸後減弱成熱帶低壓造成湖南省大暴雨的過程,使用模擬輸齣的高分辨率資料,藉助非地轉濕Q矢量對這次暴雨過程做瞭詳細的診斷分析.結果錶明:非地轉濕Q矢量能比較清楚地揭示此次暴雨縯變過程,尤其700 hPa的非地轉濕Q矢量散度場對降水預報具有較好的指示意義,其散度輻閤區域對應著降水的落區,散度輻閤彊度變化指示著降水彊度的變化趨勢,併且非地轉濕Q矢量散度輻閤彊度的大小可預示著未來3~6 h降水的彊弱,是具有預報價值的;非地轉濕Q矢量散度是非地轉ω方程的彊迫項,併與地形條件共同作用激髮瞭地麵中呎度繫統的髮展與次級環流的形成,是此次暴雨得以髮展與維持的機製.
이용WRF중척도모식모의료태풍"골파"등륙후감약성열대저압조성호남성대폭우적과정,사용모의수출적고분변솔자료,차조비지전습Q시량대저차폭우과정주료상세적진단분석.결과표명:비지전습Q시량능비교청초지게시차차폭우연변과정,우기700 hPa적비지전습Q시량산도장대강수예보구유교호적지시의의,기산도복합구역대응착강수적락구,산도복합강도변화지시착강수강도적변화추세,병차비지전습Q시량산도복합강도적대소가예시착미래3~6 h강수적강약,시구유예보개치적;비지전습Q시량산도시비지전ω방정적강박항,병여지형조건공동작용격발료지면중척도계통적발전여차급배류적형성,시차차폭우득이발전여유지적궤제.
Mesoscale model WRF has been used to simulate the course of heavy rainstorm caused by typhoon "Sepat" being weakened to tropic cyclone after landing in Hunan province, which provides the high resolution output data, detailed diagnostic analysis on the rainstorm is done with method of ageostrophic wet Q vector. It shows that, the ageostrophic wet Q vector can reveal the evolvement of rainstorm clearly, especially at the 700hPa layer it has good direction for precipitation forecast, its convergence area corresponds to precipitation area and its convergence intensity gives guidance for the variation of precipitation intensity, besides its convergence intensity can foreeast precipitation in the coming 3~6 hours; the divergence of ageostrophic wet Q vector was taken as an only forcing term in the whole ω-equation, which motivates development of surface mesoscale system and formation of secondary circulation accompanied with terrain. Both factors are the mechanism to maintain rainstorm.