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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 林和,周佳 | |
| dc.contributor.author | Chiung-Yin Chang | en |
| dc.contributor.author | 張瓊尹 | zh_TW |
| dc.date.accessioned | 2021-06-07T23:43:34Z | - |
| dc.date.copyright | 2014-07-29 | |
| dc.date.issued | 2014 | |
| dc.date.submitted | 2014-07-17 | |
| dc.identifier.citation | Arakawa, A., and W. H. Schubert, 1974: Interaction of a Cumulus Cloud Ensemble with the Large-Scale Environment, Part I. J. Atmos. Sci., 31, 674-701.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/16684 | - |
| dc.description.abstract | Vertical structures associated with tropical convection are of vital importance to tropical climate and weather phenomena, especially the convective feedbacks to large-scale environment as manifested by them. In this thesis, we explore their relationship with precipitation intensity. We first propose a simple diagnostic framework to assess these profiles in ERA-Interim, in order to remedy previous studies’ deficiencies. By considering these profiles with multiple perspectives, we discuss the prominent characteristics of deep and shallow convection, as well as the corresponding variations in large-scale flows. We then shift our focus to their roles in the intensity changes of precipitation extremes. We find that under interannual tropical tropospheric warming, extreme rainfall strengthens due to enhanced moisture convergence and reduced gross moist stability. Analyzing the vertical structures of moist static energy and vertical motion, we argue that both a decrease of deep convective energy transport via enhanced low-level moisture and increase of shallow convection partitioning can account for these changes. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-07T23:43:34Z (GMT). No. of bitstreams: 1 ntu-103-R01229005-1.pdf: 2282901 bytes, checksum: 1af092f783f97d7e8c10a49f56255220 (MD5) Previous issue date: 2014 | en |
| dc.description.tableofcontents | 摘要 ii
Abstract iii Acknowledgements iv Contents v List of Figures vii List of Tables x 1 Introduction 1 2 Data 6 2.1 Reanalysis dataset . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 2.2 Field campaign datasets . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 2.3 Satellite datasets . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 3 Vertical Structures Associated with Tropical Convection 9 3.1 A unified assessment on tropical deep and shallow convection . . . . . . . . 9 3.2 The dependence of convective vertical structures on rain rate . . . . . . . . . 11 3.2.1 Heat source and moisture sink . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 3.2.2 Temperature, moisture, and vertical motion . . . . . . . . . . . . . . . . . 15 3.3 Observational evidences from field campaigns . . . . . . . . . . . . . . . . . . . . 18 3.4 Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20 4 Convective Feedbacks for Precipitation Extremes in Warming Tropics 22 4.1 Intensity of precipitation extremes and tropical tropospheric temperature: interannual relationship from observations . . . . . . . . . . . . . 22 4.2 Analysis of moisture and moist static energy budgets . . . . . . . . . . . . . . . 26 4.2.1 Moisture budget . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26 4.2.2 Moist static energy budget . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 28 4.3 Impacts of vertical structures on gross moist stability 30 4.3.1 Regime I: M'<0 contributed by 〈-Ω ‾∂p h'〉<0 . . . . . . . . . . . 30 4.3.2 Regime II: M'<0 contributed by 〈-Ω'∂p h ‾ 〉<0 . . . . . . . . . . 32 4.3.3 Regime III: M'>0 contributed by 〈-Ω ‾∂p h'〉>0 . . . . . . . . . . 34 4.3.4 Regime IV: M'>0 contributed by 〈-Ω'∂p h ‾ 〉>0 . . . . . . . . . . 34 4.4 Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35 5 Conclusions and Future Directions 37 A Appendix A 39 A.1 Heat source and moisture sink: calculation and concept . . . . . . . . . . . . . 39 A.2 Comparison between three reanalysis datasets . . . . . . . . . . . . . . . . . . . . . 40 B Appendix B 41 B.1 Calculation of precipitation extremes . . . . . . . . . . . . . . . . . . . . . . . . . . . . 41 B.2 Surface fluxes and cloud-radiative feedbacks . . . . . . . . . . . . . . . . . . . . . 42 Bibliography 44 | |
| dc.language.iso | en | |
| dc.subject | 極端降雨 | zh_TW |
| dc.subject | 熱帶對流 | zh_TW |
| dc.subject | 垂直結構 | zh_TW |
| dc.subject | 對流回饋過程 | zh_TW |
| dc.subject | 降雨強度 | zh_TW |
| dc.subject | convective feedback | en |
| dc.subject | vertical structure | en |
| dc.subject | tropical convection | en |
| dc.subject | precipitation intensity | en |
| dc.subject | precipitation extreme | en |
| dc.title | 熱帶對流的垂直結構與降雨強度 | zh_TW |
| dc.title | Vertical Structures Associated with Tropical Convection and Precipitation Intensity | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 102-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 陳維婷,黃彥婷 | |
| dc.subject.keyword | 熱帶對流,垂直結構,對流回饋過程,降雨強度,極端降雨, | zh_TW |
| dc.subject.keyword | tropical convection,vertical structure,convective feedback,precipitation intensity,precipitation extreme, | en |
| dc.relation.page | 76 | |
| dc.rights.note | 未授權 | |
| dc.date.accepted | 2014-07-17 | |
| 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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