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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 李清勝(Cheng-Shang Lee) | |
dc.contributor.advisor | 李清勝(Cheng-Shang Lee | cslee@ntu.edu.tw | ), | |
dc.contributor.author | Ching-Wei Wang | en |
dc.contributor.author | 王鏡惟 | zh_TW |
dc.date.accessioned | 2023-03-19T23:29:24Z | - |
dc.date.copyright | 2022-10-20 | |
dc.date.issued | 2022 | |
dc.date.submitted | 2022-09-28 | |
dc.identifier.citation | 王時鼎,1970:臺灣區域冬半年連續三至六天惡劣天氣型研究。氣象學報,16,18-31。 曲克恭與陳正改,1988:琳恩颱風豪雨研究。大氣科學,16,253-262。 李清勝、羅英哲、張龍耀,2007:琳恩颱風(1987)與東北季風交互作用產生強降水之研究。大氣科學,35(1),13-33。 李清勝,2018:臺灣颱風預報技術提升整合研究-子計畫:伴隨特殊特徵之侵臺颱風的研究(II)。科技部補助專題研究計畫報告,MOST 106-2625-M-002-019,共102頁。 林士然,2014:奈格颱風引起遠距降雨之個案研究。國立臺灣師範大學地球科學所碩士論文,147頁。 陳郁涵,2018:西南季風氣流與颱風路徑對颱風離陸後台灣降雨之影響。國立臺灣大學理學院大氣科學研究所博士論文,106頁。 郭渝靖,2018:艾利颱風(2016)期間臺灣東部強降雨之研究。國立臺灣大學理學院大氣科學研究所碩士論文,87頁。 廖思瑩,2013:颱風對臺灣地區遠距降雨之影響-梅姬與馬鞍颱風個案分析。國立臺灣師範大學地球科學所碩士論文,173頁。 劉宇其,2017:哈隆颱風(2014)通過琉球海域期間臺灣西南部沿海豪雨事件之研究。國立臺灣大學理學院大氣科學研究所碩士論文,116頁。 Bosart, L.F., and F. H. Carr, 1978: A case study of excessive rainfall centered around Wellsville, New York, 20-21 June 1972. Mon. Wea. Rev., 106, 348-362. Bi, M., T. Li, M. Peng, and X. Shen, 2015: Interactions between Typhoon Megi (2010) and a low-frequency monsoon gyre. J. Atmos. Sci., 72, 2682-2702. Byun, K.-Y., and T.-Y. Lee, 2012: Remote effects of tropical cyclones on heavy rainfall over the Korean peninsula-Statistical and composite analysis. Tellus, 64, 14983 Cote, M. R., 2007: Predecessor rain events in advance of tropical cyclones. M.S. thesis, Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York, 200 pp. Chen, T.-C., and C.-C. Wu, 2016: The remote effect of Typhoon Megi (2010) on the heavy rainfall over northeastern Taiwan. Mon. Wea. Rev., 144, 3109–3131. Galarneau, T. J., Jr., L. F. Bosart, and R. S. Schumacher, 2010: Predecessor rain events ahead of tropical cyclones. Mon. Wea. Rev., 138, 3272–3297. Iacano, M. J., J. S. Delamere, E. J. Mlawer, M. W. Shephard, S. A. Clough, and W. D. Collins, 2008: Radiative forcing by long-lived greenhouse gases: calculations with the AER radiative transfer models. J. Geophys. Res., 113, D13103. Kodama S., and M. Satoh, 2022: Statistical analysis of remote precipitation in Japan caused by typhoons in September. J. Meteor. Soc. Japan., Ser II. Lee, C. S., L. R. Huang, H. S. Shen, and S. T. Wang, 2006: A climatology model for forecasting typhoon rainfall in Taiwan. Natural Hazards, 37, 87-105 Lim, K.-S., and S.-Y. Hong, 2010: Development of an effective double-moment cloud microphysics scheme with prognostic cloud condensation nuclei (CCN) for weather and climate models. Mon. Wea. Rev., 138, 1587–1612. Schumacher, R. S., T. J. Galarneau Jr., and L. F. Bosart, 2011: Distant effects of a recurving tropical cyclone on rainfall in a midlatitude convective system: A high-impact predecessor rain event. Mon. Wea. Rev., 139, 650-667. Schumacher, R. S., and T. J. Galarneau Jr., 2012: Moisture transport into midlatitudes ahead of recurving tropical cyclones and its relevance in two predecessor rain events. Mon. Wea. Rev., 140, 1810-1827. Tiedtke, M., 1989: A comprehensive mass flux scheme for cumulus parameterization in large-scale models. Mon. Wea. Rev., 117, 1779-1800. Wang, Y., Y. Wang, and H. Fudeyasu, 2009: The role of typhoon Songda (2004) in producing distantly located heavy rainfall in Japan. Mon. Wea. Rev., 137, 3699-3716. Wu, C. C., K. K. Cheung, & Y. Y. Lo, 2009: Numerical study of the rainfall event due to the interaction of Typhoon Babs (1998) and the northeasterly monsoon. Mon. Wea. Rev., 137(7), 2049-2064. Zhang, C., Y. Wang, and K. Hamilton, 2011: Improved representation of boundary layer clouds over the southeast pacific in ARW-WRF using a modified tiedtke cumulus parameterization scheme. Mon. Wea. Rev., 139, 3489-3513. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/85931 | - |
dc.description.abstract | 部分颱風在距離一地數百至上千公里遠時,雖未直接侵襲該地,該地卻伴隨有強降雨事件發生,稱之「遠距颱風降雨」。過去針對臺灣地區未與季風共伴的遠距颱風降雨個案進行的分析與模擬,結果顯示,臺灣皆位於顯著低壓帶中,低層暖濕空氣伴隨盛行風移入臺灣地區,使迎風面地區易產生強對流系統。亦即,臺灣地形與綜觀環境流場為造成顯著降雨的主要因素;而遠距颱風的存在,僅造成降雨區域的改變,與中緯度預前降雨(Predecessor Rain Events, PREs)的機制明顯不同。西行通過東海並造成臺灣西南部沿海降雨的遠距颱風個案屬於過去研究並未討論的類型,本研究之目的在針對該類個案進行資料診斷分析與數值模擬,討論其中之重要機制與遠距颱風在臺灣降雨事件中所扮演的角色。 針對典型個案(2012年海葵颱風)的分析結果顯示,強降雨期間,綜觀環境一般為對流不穩定,盛行之西南風受地形影響於西南部沿海產生減速輻合,有利對流的發生;水氣通量輻合亦集中於西南沿海,與強降雨區域一致。調整臺灣地形之敏感度實驗結果顯示,若移除臺灣地形,降雨大幅減少且其分佈出現顯著差異。本研究亦分析相似路徑的其他颱風個案,結果顯示當臺灣西南沿海有降雨時,颱風的位置均十分相近;但由於個案的綜觀流場有些許不同,因此降雨區域也不盡相同。比較未與季風共伴的各類遠距颱風降雨個案,結果顯示各類個案的降雨均由綜觀環境及臺灣地形主導。綜合以上分析、模擬及比較結果顯示,臺灣地區之遠距颱風降雨的發生機制,應與環境流場分佈及臺灣地形密切相關,而颱風似扮演較次要的角色。 | zh_TW |
dc.description.abstract | Severe rainfall may occur in Taiwan when typhoons are located around Taiwan but within a certain distance, which is called “Typhoon Remote Rainfall.” Some studies analyzed and simulated a few typhoon remote rainfall cases in Taiwan which were not accompanied by monsoon. Results show that there was a large-scale cyclonic circulation surrounding Taiwan in these cases. Low level warm, humid air flowed into Taiwan-nearby area, making it a favorable environment on the windward side for convection to develop. The synoptic pattern and Taiwan topography are the key factors to typhoon remote rainfall in Taiwan. The existence of remote typhoons, however, seems to lead to the adjustment of rainfall area only. The mechanism of typhoon remote rainfall in Taiwan is apparently different from Predecessor Rain Events (PREs) which occurred in midlatitudes. Some typhoon remote rainfall cases occurred when remote typhoons went westward and passed through the East China Sea. These cases are not discussed before. The purpose of this study is to understand the important process leading to such type of typhoon remote rainfall in Taiwan through synoptic diagnosis and model simulations. Results of a typical case study (typhoon HAIKUI, 2012) show that the synoptic environment was convective unstable during the heavy rainfall hour on the southwestern coast of Taiwan. Speed convergence occurred when southwesterlies encountered Taiwan topography. There was also horizontal moisture flux convergence over the southwest coast of Taiwan, which was consistent with the area of the heavy rainfall. Sensitivity experiments were conducted to understand the effects of Taiwan topography. Results show that the amount and pattern of rainfall changed dramatically when Taiwan topography was removed in the simulation. There are several typhoons with tracks similar to that of typhoon HAIKUI. Results of the comparison between these cases show that the locations of typhoons were similar when rainfall occurred over southwestern Taiwan, but there are still some differences in rainfall area due to the different patterns of synoptic flow. The comparison between different types of typhoon remote rainfall cases which were not accompanied by monsoon was also conducted. Results show that the heavy rainfall in these cases is associated with the synoptic flow and the topography. To sum up, the synoptic-scale pattern and the Taiwan topography play key roles in such typhoon remote rainfall events, which are not accompanied by monsoon. The remote typhoon only plays a secondary role in changing the location of heavy rainfall. | en |
dc.description.provenance | Made available in DSpace on 2023-03-19T23:29:24Z (GMT). No. of bitstreams: 1 U0001-2809202200550500.pdf: 21092465 bytes, checksum: b03398c454f887f0690ccd8bd60896ce (MD5) Previous issue date: 2022 | en |
dc.description.tableofcontents | 口試審定書 i 謝辭 ii 摘要 iii Abstract iv 目錄 v 圖目錄 vii 第一章 前言 1 第二章 使用資料及個案綜觀環境概述 5 2.1 使用資料 5 2.2 海葵颱風概述及綜觀環境分析 5 2.3臺灣西南部8月8日至8月9日降雨歷程與分析 6 2.4 小結 8 第三章 數值模擬與模式校驗 9 3.1 模式簡介 9 3.2 網格設計及參數化設定 10 3.3 模擬結果校驗 11 3.4 小結 12 第四章 海葵颱風伴隨之西南部降雨模擬結果分析 13 4.1 綜觀環境分析 13 4.2 臺灣西南部降雨之分析 14 4.3 調整地形之敏感度實驗結果分析 16 4.4 小結 18 第五章 遠距颱風之分類與比較 20 5.1 遠距颱風分類 20 5.2 艾利颱風(2016)伴隨遠距颱風降雨(A、B類) 21 5.3 哈隆颱風(2014)伴隨遠距颱風降雨(C、D類) 22 5.4 海葵颱風與相似個案比較(E類) 22 5.5 小結 23 第六章 討論與總結 25 參考文獻 29 | |
dc.language.iso | zh-TW | |
dc.title | 遠距颱風伴隨臺灣降雨事件之分析 | zh_TW |
dc.title | A Study of the Typhoon Remote Rainfall in Taiwan | en |
dc.type | Thesis | |
dc.date.schoolyear | 110-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 郭鴻基(Hung-Chi Kuo),楊明仁(Ming-Jen Yang) | |
dc.subject.keyword | 颱風,遠距颱風降雨,沿海降雨,臺灣地形, | zh_TW |
dc.subject.keyword | typhoon,typhoon remote rainfall,coastal rainfall,Taiwan topography, | en |
dc.relation.page | 80 | |
dc.identifier.doi | 10.6342/NTU202204183 | |
dc.rights.note | 同意授權(全球公開) | |
dc.date.accepted | 2022-09-29 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 大氣科學研究所 | zh_TW |
dc.date.embargo-lift | 2022-10-20 | - |
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