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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 周仲島 | |
| dc.contributor.author | Ji-Shiang Cho | en |
| dc.contributor.author | 卓智祥 | zh_TW |
| dc.date.accessioned | 2021-06-13T04:29:56Z | - |
| dc.date.available | 2006-07-26 | |
| dc.date.copyright | 2006-07-26 | |
| dc.date.issued | 2006 | |
| dc.date.submitted | 2006-07-20 | |
| dc.identifier.citation | 參考文獻：
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Lin, 2005: Effects of Moist Froude Number and CAPE on a Conditionally Unstable Flow over a Mesoscale Mountain Ridge. Journal of the Atmospheric Sciences: Vol. 62, No. 2, pp. 331–350. Chisholm, A. J., and J. H. Renick, 1972: The kinematics of multicell and supercell Alberta hailstorms, Alberta Hail Studies, 1972. Research Council of Alberta Hail Studies Rep. NO. 72-2, 24-31. Cotton, W. R., and R. A. Anthes, 1989: Storm and cloud dynamics. Edited by R. Dmqwska and J. R. Holton. Academic Press, Inc. 540-558pp.,463-472pp.883pp. Droegemeier, K. K., and R. B. Wilhelmson. 1985: Three-Dimensional Numerical Modeling of Convection Produced by Interacting Thunderstorm Outflows. Part I: Control Simulation and Low-Level Moisture Variations. Journal of the Atmospheric Sciences: Vol. 42, No. 22, pp. 2381–2403. Goff, R. C. 1976: Vertical Structure of Thunderstorm Outflows. Monthly Weather Review: Vol. 104, No. 11, pp. 1429–1440. Houze, R. A. Jr., B. F. Smull and P. 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Schreiber. 1986: Initiation of Convective Storms at Radar-Observed Boundary-Layer Convergence Lines. Monthly Weather Review: Vol. 114, No. 12, pp. 2516–2536. Wilson, J. W., T. M. Weckwerth, J. Vivekanandan, R. M. Wakimoto and R. W. Russell. 1994: Boundary Layer Clear-Air Radar Echoes: Origin of Echoes and Accuracy of Derived Winds. Journal of Atmospheric and Oceanic Technology: Vol. 11, No. 5, pp. 1184–1206. Xin, L., G. Recuter, and B. Larochelle, 1997: Reflectivity-rain rate relationship for convective rainshowers in Edmonton. Atmos. Ocean,35, 513-521. Ziegler, C. L., and E. N. Rasmussen. 1998: The Initiation of Moist Convection at the Dryline: Forecasting Issues from aCase Study Perspective. Weather and Forecasting: Vol. 13, No. 4, pp. 1106–1131. | |
| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/33222 | - |
| dc.description.abstract | 本研究針對2004和2005年梅雨季(5、6月)，依北部地面測站有雷暴紀錄，選取在大台北和雪山山脈北支地區發生於內陸而非海上移入之雷暴系統，進行中尺度分析。依據雷暴主要發展與影響地理區域，將之區分為主要影響台北盆地的盆地型、主要影響雪山山脈北支的山區型、以及兩地區皆有影響的混合型。其中，分別個案數依序為3、5、5個。
利用板橋探空資料分析個案環境的對流可用位能和垂直風切，結果顯示發生於不同區域的雷暴，對流可用位能分布較無規律，但垂直風切有明顯區別。山區型垂直風切皆大於10 以上，盆地型則小於8 以下，而混合型則介於兩種類型之間。午後雷暴初期發展的地點分析結果顯示，影響台北盆地的雷暴系統主要在雪山山脈上發展後移入，有時也會在盆地內發展。 三類型各選取一個案進行分析，盆地型(04/05/29)和山區型(04/05/13)雷暴雷達回波有明顯的差異。盆地型(04/05/29)個案為單胞型雷暴，山區型(04/05/13)個案為組織性多胞雷暴。盆地型(04/05/29)個案回波發展高度達12km以上，遠高於山區型(04/05/13)個案的回波高度6~7km。由雷達回波估計之降水生命期也顯示盆地型雷暴生命期較短，山區型雷暴生命期較長。 混合型(04/06/23)個案中，地面測站顯示盆地東南側為乾燥地區，因此使得斜坡上的雷暴系統強度快速減弱。而盆地內雷暴發展時，其低層徑向風場有輻合現象，地面測站也顯示有海風環流特徵。由於隨後斜坡雷暴系統移入盆地，與盆地之雷暴系統合併，其外流區和海風環流所形成輻合帶有益於盆地內的雷暴系統的維持與再發展。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-06-13T04:29:56Z (GMT). No. of bitstreams: 1 ntu-95-R93229009-1.pdf: 5555919 bytes, checksum: ef32b342178923d2db12839148351a2c (MD5) Previous issue date: 2006 | en |
| dc.description.tableofcontents | 目 錄
摘要----------------------------------------------------------------------------------I 致謝---------------------------------------------------------------------------------II 目錄------------------------------------------------------------------------------- IV 表錄------------------------------------------------------------------------------- VI 圖錄------------------------------------------------------------------------------ VII 第一章 前言---------------------------------------------------------------------- 1 1-1 論文回顧--------------------------------------------------------------- 1 1-1-1 對流胞的激發與傳播---------------------------------------- 1 1-1-2 環境垂直風切------------------------------------------------- 4 1-1-3 台灣地區的研究---------------------------------------------- 6 1-2 研究動機與目的------------------------------------------------------ 7 第二章 資料來源與處理方法------------------------------------------------- 9 2-1 資料來源--------------------------------------------------------------- 9 2-2 都卜勒雷達資料------------------------------------------------------ 9 2-2-1 五分山都卜勒雷達------------------------------------------- 9 2-2-2 中正機場都卜勒雷達---------------------------------------10 2-3 雷達資料處理方法--------------------------------------------------11 第三章 北台灣梅雨季雷暴系統(2004和2005年)-----------------------12 3-1 個案選取------------------------------------------------------------- 12 3-1-1 選取條件與方法---------------------------------------------12 3-1-2 選取個案簡介------------------------------------------------13 3-2 特徵分類------------------------------------------------------------- 14 3-2-1 平均雷達回波特徵------------------------------------------15 3-2-2 環境條件------------------------------------------------------20 3-2-3 雷暴初期發展位置------------------------------------------21 3-2-4 移動方向與盛行風相關性---------------------------------21 3-2-5 地面測站特點------------------------------------------------22 3-3 小結------------------------------------------------------------------- 23 第四章 個案分析---------------------------------------------------------------26 4-1 環境條件---------------------------------------------------------------26 4-1-1 可見光衛星雲圖分析----------------------------------------26 4-1-2 地面天氣圖分析---------------------------------------------- 27 4-1-3 環境探空分析------------------------------------------------- 27 4-1-4 地面雨量觀測分析------------------------------------------- 28 4-2 雷達回波隨時間的演變特徵---------------------------------------28 4-2-1 盆地型個案和山區型個案回波特徵----------------------29 4-2-2 盆地型和山區型結構特徵的差異-------------------------30 4-2-3 混合型個案：2004年6月23日--------------------------32 4-2-4 盆地地區內的乾區和低層輻合帶-------------------------35 第五章 討論---------------------------------------------------------------------37 5-1 台北盆地地面測站分析------------------------------------------- 37 5-2 環境的對流可用位能---------------------------------------------- 37 5-3 雷暴的傳播或移動方向特徵------------------------------------- 38 第六章 結論---------------------------------------------------------------------40 參考文獻--------------------------------------------------------------------------42 附表圖-----------------------------------------------------------------------------47 附錄：2004、2005年各類型雷達回波統整------------------------------122 | |
| dc.language.iso | zh-TW | |
| dc.subject | 都卜勒雷達 | zh_TW |
| dc.subject | 雷暴 | zh_TW |
| dc.subject | Thunderstorm | en |
| dc.subject | Doppler Radar | en |
| dc.title | 梅雨季北台灣雷暴系統之中尺度分析 | zh_TW |
| dc.title | The mesoscale characteristic of Thunderstorms occurred in Northern Taiwan during Meiyu season | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 94-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 柯文雄,簡芳菁,游政谷,許武榮 | |
| dc.subject.keyword | 雷暴,都卜勒雷達, | zh_TW |
| dc.subject.keyword | Thunderstorm,Doppler Radar, | en |
| dc.relation.page | 131 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2006-07-21 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 大氣科學研究所 | zh_TW |
| 顯示於系所單位： | 大氣科學系 | |
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