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颱風引發焚風之初步研究

A Preliminary Study on Typhoon-Induced Foehn Winds

摘要


焚風是山脈背風面下沉的乾暖風。迎風面的強風是誘發山背焚風的主要原因。本研究用數值模式討論焚風發生的機制及水汽在焚風現象中扮演的角色。同時,以民國60年9月22日貝絲颱風為例探討颱風誘發台灣東南地區焚風的現象。

關鍵字

焚風 颱風 地形效應

並列摘要


The foehn is a warm, dry wind descending in the lee of a mountain range. The strong wind in the upslope is mainly responsible for the induced foehn wind. The mechanism of foehn and the role of water vapour in the foehn are studied in this thesis by means of numerical modeling. Meanwhile, a numerical integration is conducted to simulate the typhoon case occurred on 22 September, 1971, which caused foehn wind in the south-east area of Taiwan.

並列關鍵字

foehn typhoon errain effect

被引用紀錄


陳雨青(2010)。颱風侵台期間路徑發生打轉之研究〔碩士論文,國立臺灣大學〕。華藝線上圖書館。https://doi.org/10.6342/NTU.2010.01986

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