請用此 Handle URI 來引用此文件:
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/35848
完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 陳泰然 | |
dc.contributor.author | Sau-Wa Chang | en |
dc.contributor.author | 曾秀樺 | zh_TW |
dc.date.accessioned | 2021-06-13T07:13:27Z | - |
dc.date.available | 2005-07-29 | |
dc.date.copyright | 2005-07-29 | |
dc.date.issued | 2005 | |
dc.date.submitted | 2005-07-26 | |
dc.identifier.citation | 王時鼎、鄭俠、徐晉准及丘台光,1985:五、六月間台灣地區暴雨 環境條件。天氣分析與預報研討會論文彙編,中央氣象局,55–77。
林松錦與王溫和,1992:梅雨鋒面之鋒生過程。大氣科學,21,63–78。 侯喜真與陳泰然,2001:梅雨季伴隨華南西南風爆發之低壓發展。大氣科學,29,203–228。 陳泰然,1988:東亞梅雨鋒面之綜觀氣候特徵研究。大氣科學,16,435–446。 ______與紀水上,1978:台灣梅雨鋒面之中幅度結構。大氣科學,5,35–47。 ______與蒲金標,1985:華南春季低層噴流之形成與台灣北部地區豪雨之個案分析。大氣科學,12,23–32。 Akiyama, T., 1973: Ageostropic low-level jet stream in the Baiu season associated with heavy rainfalls over the sea area. J. Meteor. Soc. Japan, 51, 205–208. Bretherton, F. P., 1966: Critical layer instability in baroclinic flows. Quart. J. Roy. Meteor. Soc., 92, 325–334. Chen, G. T. J., 1977:A synoptic case study on mean structure of Mei-Yu Taiwan. Atmos. Sci., 4, 38–47. ______, 1979: Mesoscale analysis for a Mei-Yu case over Taiwan. Papers Meteor. Res., 2, 63–74. ______, 1983: Observational aspects of the Mei-Yu phenomena in subtropical China. J. Meteor. Soc. Japan, 61, 306–312. ______, 2004: Research on the phenomena of Meiyu over China and Taiwan during the past quarter century: An overview. World Scientific Series for Meteorology of East Asia Vol. 2, East Asian Monsoon, C. P. Chang, Ed., World Scientific Publishing Co., 357–403. ______, and C. P. Chang, 1980: The structure and vorticity budget of an early summer monsoon trough (Mei-Yu) over southeastern China and Japan. Mon. Wea. Rev., 108, 942–953. ______ and S. S. Chi, 1980: On the frequency and speed of Mei-Yu front over southern China and the adjacent areas. Ppaers Meteor. Res., 3, 1&2, 31–42. ______, C. C. Wang, and S. C. –S. Liu, 2003: Potential vorticity diagnostics of a Mei-Yu front case. Mon. Wea. Rev., 131, 2680–2696. ______, C. C. Wang, and D. T. W. Lin, 2005: Characteristics of low-level jets over northern Taiwan in Mei-Yu season and their relationship to heavy rain events. Mon. Wea. Rev., 133, 20–43. ______, and C. C. Yu, 1988: Study of low-level jet and extremely heavy reainfall over northern Taiwan in the Mei-Yu season. Mon. Wea. Rev., 116, 884–891. Chen, S. J., Y. H. Kuo, W. Wang, X. Y. Tao, and B. Cui, 1998: A modeling case study of heavy rainstorms along the Mei-Yu front. Mon. Wea. Rev., 126, 2330–2351. Chen, X. –A., and Y. –L. Chen, 1995: Development of low-level jets during TAMEX. Mon. Wea. Rev., 123, 1695–1719. Chen, Y. –L., X. –A. Chen, and Y. –X. Zhang, 1994: A diagnostic study of the low-leve jet during TAMEX IOP 5. Mon. Wea. Rev., 122, 2257–2284. Cho, H. R., and G. T. J. Chen, 1995: Mei-Yu frontogenesis. J. Atmos. Sci., 52, 2109–2120. Chou, L. C., C. P. Chang, and R. T. Williams, 1990: A numerical simulation of the Mei-Yu front and the associated low level jet. Mon. Wea. Rev., 118, 1408–1428. Davis, C. A., 1992a: A potential-vorticity diagnosis of the importance of initial structure and condensational heating in observed extratropical cyclogenesis. Mon. Wea. Rev., 120, 2409–2427. ______, 1992b: Piecewise potential vorticity inversion. J. Atmos. Sci., 49, 1397–1411. ______, and K. A. Emanuel, 1991: Potential vorticity diagnostics of cyclongenesis. Mon. Wea. Rev., 119, 1929–1953. ______, E. D., Grell, and M. A. Shapiro, 1996: The balanced dynamical nature of a rapid intensifying oceanic cyclone. Mon. Wea. Rev., 121, 2309–2330. Holton, J. R., 1992: An Introduction to Dynamic 8Meteorology. Third ed., Academic Press, 511 pp. Hsu, W. –R., and W. Y. Sun, 1994: A numerical study of a low-level jet and its accompanying secondary circulation in a Mei-Yu system. Mon. Wea. Rev., 122, 324–340. Huo, Z., D. L. Zhang, and J. Gyakum, 1998: An application of potential vorticity inversion to improving the numerical prediction of the March 1993 superstorm. Mon. Wea. Rev., 126, 424–436 Kuo, Y. H., and G. T. J. Chen, 1990: The Taiwan Area Mesoscale Experiment (TAMEX): An overview. Bull. Amer. Meteor. Soc., 71, 488–503. ______, and R. A. Anthes, 1982: Numerical simulation of a Mei-Yu system over southeastern Asia. Pap. Meteor. Res., 5, 15–36. Matsumoto, S., 1972: Unbalanced low-level jet and solenoidal circulation associated with heavy rainfalls. J. Meteor. Soc. Japan, 50, 194–203. ______, 1973:Lower tropospheric wind and precipitation activity. J. Meteor. Soc. Japan, 51, 101–107. Nagata, M., and Y. Ogura, 1991: A modeling case study of interaction between heavy precipitation and a low-level over Japan in the Baiu season. Mon. Wea. Rev., 119, 1309–1336. Ninomiya, K., 1984: Characteristics of Baiu front as a predominant subtropical front in the summer northern hemisphere. J. Meteor. Soc. Japan, 62, 880–894. _______, and T. Akiyama, 1974: Band structure of mesoscale echo cluster associated with low-level jet stream. J. Meteor. Soc. Japan, 52, 300–313. Tao, S. –Y., and L. X. Chen, 1987: A review of recent research on the East Asian summer monsoon in China. Monsoon Meteorology, Edited by C. P. Chang, and T. N. Krishnamurti, Eds., Oxford University Press, 60–92. Yanai, M., S. Esbensen, and J. –H. Chu, 1973: Determination of bulk properties of tropical cloud clusters from large-scale heat and moisture budgets. J. Atmos. Sci., 30, 611–627. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/35848 | - |
dc.description.abstract | 2003年6月6∼7日華南與台灣地區受梅雨鋒面影響,衛星雲圖顯示中尺度對流系統(MCSs)於鋒面及其南側持續發展,且水平覆蓋範圍廣泛。伴隨對流發展,850 hPa鋒面區之相對渦度相對增強, MCSs南側亦有LLJ形成並隨時間增強。隨後MCSs持續發展並東移影響台灣地區,造成中、南部豪(大)雨。本文主要目的為探討此個案梅雨鋒面上持續發展之MCSs與鋒面強度維持和其南側LLJ形成與增強之機制。
綜觀分析顯示,個案期間除了低層鋒面系統外,並無其他明顯高層槽脊系統或噴流位於台灣及華南地區,顯然鋒面為主要造成台灣中、南部地區豪(大)雨之環流系統。本個案中梅雨鋒面結構為垂直近乎不傾斜的淺系統,鋒面水平溫度梯度微弱,具有強水平氣旋式風切及顯著之水氣梯度,中對流層並有暖心存在,與Chen and Chang(1980)分析個案中之西段鋒面結構相似。 有關本個案鋒面強度之維持與發展,本文利用逐段位渦反演診斷鋒面上相對渦度之增強,發現主要來自於中低層與潛熱釋放有關之位渦擾動所貢獻。另外,從渦度收支之分析結果亦得知,低層輻合為鋒面上渦度維持之主要過程。本個案雖發生於25°N以南之區域,但由於對流系統水平尺度夠大且發展時間持久,使對流潛熱釋放能有效加熱大氣,透過非線性CISK過程,導致鋒面上相對渦度由8 × 10-5 s-1增強至16 × 10-5 s-1。顯然對流潛熱釋放與輻合過程對梅雨鋒面的發展與維持,均扮演重要的角色。 此外,由逐段位渦反演之結果顯示,與中低層潛熱釋放有關之位渦擾動引發氣旋式環流,增強MCSs南側局部風場而形成 LLJ。就調整觀點而言,MCSs潛熱釋放造成局部氣壓梯度增強,因而增強地轉風;同時,潛熱釋放亦有利低層輻合之增強,產生非地轉風,再透過科氏加速增強西南風並疊加於地轉風上,使LLJ形成與發展。 | zh_TW |
dc.description.provenance | Made available in DSpace on 2021-06-13T07:13:27Z (GMT). No. of bitstreams: 1 ntu-94-R92229013-1.pdf: 6577875 bytes, checksum: 8d598e62bcc650501d3dda7240301fd3 (MD5) Previous issue date: 2005 | en |
dc.description.tableofcontents | 目 錄--------------------- I
摘 要--------------------- III 圖 說--------------------- IV 第一章 前言--------------- 1 第二章 資料來源與分析方法- 6 一、資料來源--------------- 6 二、分析方法--------------- 6 第三章 綜觀天氣形勢------- 12 一、地面分析--------------- 12 二、高空分析--------------- 13 三、衛星雲圖分析----------- 14 四、小結------------------- 15 第四章 梅雨鋒面結構------- 17 一、水平結構--------------- 17 二、垂直結構--------------- 20 三、小結------------------- 22 第五章 鋒面強度維持機制--- 24 一、逐段位渦反演----------- 24 二、渦度收支--------------- 26 三、小結------------------- 28 第六章 LLJ形成與增強機制-- 30 一、MCSS 與LLJ------------- 30 二、逐段位渦反演----------- 31 三、非地轉風分析----------- 33 四、小結------------------- 34 第七章 討論--------------- 35 第八章 總結--------------- 40 誌 謝--------------------- 42 參考文獻------------------- 43 圖-------------------------47 | |
dc.language.iso | zh-TW | |
dc.title | 梅雨鋒面個案之診斷分析 | zh_TW |
dc.type | Thesis | |
dc.date.schoolyear | 93-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 李清勝,周仲島,林松錦,王重傑 | |
dc.subject.keyword | 梅雨鋒面,位渦擾動,低層噴流,潛熱釋放,非線性第二類條件不穩度, | zh_TW |
dc.subject.keyword | Meiyu front,potential vorticity anomaly,low-level jet,conditional instability of the second kind (CISK), | en |
dc.relation.page | 81 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2005-07-26 | |
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 |
文件中的檔案:
檔案 | 大小 | 格式 | |
---|---|---|---|
ntu-94-1.pdf 目前未授權公開取用 | 6.42 MB | Adobe PDF |
系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。