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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 林依依(I-I Lin) | |
| dc.contributor.author | Nan-Hsun Chi | en |
| dc.contributor.author | 紀南薰 | zh_TW |
| dc.date.accessioned | 2021-06-15T05:56:02Z | - |
| dc.date.available | 2012-08-19 | |
| dc.date.copyright | 2010-08-19 | |
| dc.date.issued | 2010 | |
| dc.date.submitted | 2010-08-17 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/47349 | - |
| dc.description.abstract | The nearly synchronizing genesis and intensification of the dual supertyphoons Ivan and Joan (1997) was a very distinctive event in history. Ivan and Joan formed within two days in the vast cloud cluster over the tropical Central Pacific (CP) during October 1997, the mature phase of the strongest El Nino on record. Afterward, they maintained 20° latitude apart and intensified to 160 kt within the same day prior to recurvature. Based on statistics, Ivan and Joan were two of the four 160 kt extremely intense TCs over the Western North Pacific (WNP) in the past 30 years.
The time and space background of this special event is analyzed in this study. Result shows that the intense westerly wind events of the 20 to 25 day time scale variability during El Nino autumn provided a favorable environment for cyclogenesis over tropical CP. However, the mechanisms for intensification seem to differ from each other. Ivan was predominantly intensified by large divergence of the pre-existing weak upper level PV maxima while Joan principally intensified under very weak vertical wind shear. The fast enough translation speed of Ivan and Joan was also remarkable for the TCs intensification through a shallower upper warm ocean layer in WNP during El Nino. Interestingly, Ivan and Joan were characterized by their relatively small size in horizontal. The result also indicates that the radial relative humidity distribution may be critical to the radial distribution of the convective activities. And it may in turn affect the intensity and intensity change. Ivan and Joan are suggested to be the integrated products which were contributed from interannual to intraseasonal variability, as well as to certain lucky coincidence. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-15T05:56:02Z (GMT). No. of bitstreams: 1 ntu-99-R97229024-1.pdf: 15580422 bytes, checksum: c087b90ed9f0799f883eb102599fcc75 (MD5) Previous issue date: 2010 | en |
| dc.description.tableofcontents | Acknowledgment…………………………………………………………………….. i
Abstract…………………………………………………………………………….... ii 摘要………………………………………………………………………………….. iv Table of Contents……………………………………………………………………. v List of Tables……………………………………………………………………....... vi List of Figures………………………………………………………….…………... vii Chapter 1 Introduction…………………………………………………………. 1 1.1 Motivation…………………………………………………………………. 1 1.2 Scientific background……………………………………………………... 1 1.2.1 Cyclogenesis…………………………………………………….. 1 1.2.2 Cyclone intensification…………….………….……………….... 3 1.2.3 Climate and typhoons…………………………………………… 7 Chapter 2 Data and method…………………………………………………... 10 2.1 Data………………………………………………………………………. 10 2.2 Method…………………………………………………………………… 14 Chapter 3 Results and discussion……………………………………………... 16 3.1 Genesis environment……………………………………………………... 16 3.1.1 Contribution of tropical interannual variability: why this late season? ………………………………………………………... 17 3.1.2 Contribution of twin cyclogenesis: southern hemisphere interaction……………………………………………………... 21 3.2 Intensification environment……………………………………………..... 22 3.2.1 Large scale ocean environment……………………………....... 22 3.2.2 Large scale atmosphere environment…………………….……. 25 3.2.3 Cyclone characteristic…………………………………………. 29 Chapter 4 Conclusion…………………………………………………………. 33 References………………………………………………………………………….. 36 | |
| dc.language.iso | en | |
| dc.subject | 氣旋大小 | zh_TW |
| dc.subject | 超級颱風 | zh_TW |
| dc.subject | 聖嬰現象 | zh_TW |
| dc.subject | 氣旋生成 | zh_TW |
| dc.subject | 氣旋增強 | zh_TW |
| dc.subject | El Nino | en |
| dc.subject | Supertyphoon | en |
| dc.subject | cyclone size | en |
| dc.subject | cyclone intensification | en |
| dc.subject | cyclogenesis | en |
| dc.title | 1997年艾凡和喬安雙超級颱風大氣海洋前置條件 | zh_TW |
| dc.title | Atmosphere and Ocean Pre-conditions of the Dual Supertyphoons, Ivan and Joan, 1997 | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 98-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 許晃雄(Huang-Hsiung Hsu) | |
| dc.contributor.oralexamcommittee | 吳俊傑(Chun-Chieh Wu),隋中興(Chung-Hsing Sui),鄒治華(Chih-Hua Tsou) | |
| dc.subject.keyword | 超級颱風,聖嬰現象,氣旋生成,氣旋增強,氣旋大小, | zh_TW |
| dc.subject.keyword | Supertyphoon,El Nino,cyclogenesis,cyclone intensification,cyclone size, | en |
| dc.relation.page | 84 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2010-08-18 | |
| 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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