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大尺度環流剖面結構之年際變化與台灣梅雨之活躍度

Interannual Variabilites of the Large-scale Cross-sectional Structure and the Related Activities Taiwan Mei-Yu

摘要


本文利用NCAR網格點資料,分析1975-1984年台灣梅雨期(5月15日-6月15日)大尺度環流之剖面結構,並探討其年際變化與梅雨活躍度之相關。結果顯示,副熱帶太平洋高壓之強度與位置,為決定台灣梅雨活躍度之先決條件。而中緯度冷空氣南侵以維持梅雨鋒面,為決定梅雨活躍度之必要條件。東亞梅雨區哈德里胞在梅雨顯著時較強,顯示有較強之中低緯度交互作用。此外,並發現梅雨區大氣屬正壓穩定狀態,擾動若有發展,正壓不穩定過程顯然並不重要。

關鍵字

梅雨 年際變化 大尺度環流

並列摘要


NCAR grid point data were used to analyze the cross sectional structure of the large-scale circulations for the Taiwan Mei-Yu season (May 15-June 15) of 1975-1984. The interannual variations of the large-scale circulations and the Mei-Yu rainfalls were also investigated. Results showed that the prerequisite condition for the Mei-Yu activities was the intensity of subtropical Pacific high over the Mei-Yu area. It was also found that the intrusion of the midlatitude cold air was a necessary condition for having an active Mei-Yu season.The local Hadley circulation was stronger over the East Asia for the more active Mei-Yu season. Thus, the more active interactions between the lower- and middle-latitude circulations will be expected. Finally, the atmosphere over Mei-Yu area was found to be barotropically stable. Should the disturbance develop, the barotropic process would not be important.

被引用紀錄


姜禮鴻(2005)。花蓮地區梅雨季降水特性與豪(大)雨個案診斷分析〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU.2005.02696

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