研究生: |
蘇南州 |
---|---|
論文名稱: |
哈格比颱風(2008)雨帶結構與演變之模擬研究 A numerical study on rainband structure and evolution of Typhoon Hagupit (2008) |
指導教授: | 王重傑 |
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: | 2017 |
畢業學年度: | 105 |
語文別: | 中文 |
論文頁數: | 104 |
中文關鍵詞: | 哈格比颱風 、颱風雨帶 、雨帶生成 、主雨帶 |
DOI URL: | https://doi.org/10.6345/NTNU202203439 |
論文種類: | 學術論文 |
相關次數: | 點閱:162 下載:72 |
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過去的研究顯示,機載雷達所觀測的2008年哈格比颱風,其主雨帶具有較不一樣的結構特徵。為了對其有進一步的了解,本研究利用CReSS模式對本個案進行模擬,重現哈格比颱風雨帶的結構與演變,並探討其生成的機制。模擬的結果顯示,主雨帶的風場結構同時具有內、外雨帶的特徵;對流結構與外雨帶相似,向上向內傾斜,層狀降水區域則發生在雨帶內側。雨帶在徑向的移動上,於生成初期,並沒有明顯的移動;雨帶發展成熟後,則明顯向外移動,速度為4.72~6.1 m⋅s-1。
本研究個案的三個雨帶,具有類似的生成機制。舊有內雨帶外側的下沉氣流,使得空氣於近地表處堆積,造成近地表水平輻散。雨帶和其外側輻散區隨著時間相對於颱風中心向外(東)移動的過程中,氣流向外加速,並且輻散區的前緣亦使得氣流向外加速。向外加速的風場與環境氣流產生合流,進一步產生輻合,並激發出雨帶。由於雨帶走向主要為切向方向,本研究從圓柱座標的徑向運動方程,討論各作用力對於徑向風速加速的貢獻,結果顯示,不論擾動氣壓梯度力,離心力和科氏力,皆在雨帶生成之前,對於徑向風的加速產生正的貢獻。綜合以上顯示,雨帶之間的交互作用是影響雨帶發展的重要因素之一。
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