研究生: |
曾世任 |
---|---|
論文名稱: |
中尺度對流系統個案之數值研究 |
指導教授: | 簡芳菁 |
學位類別: |
碩士 Master |
系所名稱: |
地球科學系 Department of Earth Sciences |
論文出版年: | 2002 |
畢業學年度: | 90 |
語文別: | 中文 |
論文頁數: | 121 |
中文關鍵詞: | MCS 、背風波 、離岸風 、潛在不穩定 |
論文種類: | 學術論文 |
相關次數: | 點閱:140 下載:3 |
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本文針對1998年6月4-5日,發生在華南/南海北部的組織性中尺度對流系統,利用NCAR/PSU MM5模式,探討此一地區MCSs的演變及結構。此個案最顯著的外部特徵為伴隨梅雨鋒面的南側,沿著20∘N呈東—西方向排列了三個組織完整的MCS,每個MCS之間相距約400公里。經由模擬的結果顯示,模式大體上能夠掌握諸如鋒面、風切線、槽線及低層噴流(LLJ)等綜觀尺度的系統特徵。對於三個MCS(分別以MCS A、B及C來標示)的模擬上,其中除MCS B的模擬結果生命期較觀測為短,且降水強度稍弱外,其他與觀測結果相近。
模式15公里網格之模擬的結果顯示,MCS A在具有暖濕、氣旋式風切、合流及風速輻合的環境下初始。夜間中南半島陸風的增強,更加強了離岸風在MCS A處之風速輻合的效果。初始前,盛行西南風越過狹長的安南山脈形成背風波。由背風擾動所造成一連串垂直運動中的上升氣流,將850 hPa高相當位溫區的潛在不穩定氣層舉升,是激發MCS A初始前對流活動的重要機制。位於MCS A南方及西南方的底層暖平流,在成長期階段是重要的對流活動強迫項。另外,850 hPa風切線南方的綜觀尺度LLJ在成長期到成熟期階段顯著增強,透過LLJ所帶來的豐沛暖濕空氣,使得位於LLJ左前方的MCS A獲得較強的水汽及質量輻合,產生更強的上升運動。
MCS B形成於華南低層相當位溫脊線附近及風切線南側,伴隨大尺度鋒區之輻合帶並具潛在不穩定的大氣環境內。激發MCS B的強迫機制,包括了:1.此區內的合流及局部風速輻合之效應;2.由熱力因素激發之前一降水系統外流邊界和MCS B初始前降水蒸發冷卻所造成之冷池對氣流的強迫抬升;3.地形對氣流的強迫抬升作用等因素。發展過程中由水汽凝結潛熱釋放所誘發出來的中尺度低壓(低層)及中尺度高壓(高層)也是維持MCS繼續發展的有利條件。而次綜觀環境中底層冷平流的出現,則為模式中MCS B迅速消散的重要因素。
MCS C初始於呂宋島西北方海面上,同樣位於具有850 hPa高相當位溫區,屬於潛在不穩定的環境。低層強西南氣流下風處的風速輻合、合流效應及暖平流,是MCS C初始的可能舉升機制。且在MCS C發展過程中,其中的風速輻合及合流效應幾乎均有伴隨。消散期階段,位於巴士海峽附近的850 hPa相當位溫脊線明顯減弱,MCS C的降水強度亦隨之迅速減弱。
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