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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 林依依(I-I Lin) | |
| dc.contributor.author | Feng-Chin Wang | en |
| dc.contributor.author | 王鳳琴 | zh_TW |
| dc.date.accessioned | 2021-06-13T03:31:30Z | - |
| dc.date.available | 2008-12-31 | |
| dc.date.copyright | 2006-07-31 | |
| dc.date.issued | 2006 | |
| dc.date.submitted | 2006-07-27 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/32095 | - |
| dc.description.abstract | Information of air-sea turbulent fluxes is critical in air-sea interaction research. Satellite-based flux estimation is currently the most viable way to obtain such flux data over vast oceans at frequent intervals. This work use recently-available advanced remote sensing data sets (including sea surface temperature from TRMM/TMI and AMSR-E, ocean surface wind vectors from QuikSCAT and ADEOS2-SeaWinds) to improve the existing Goddard Satellite Based Surface Turbulent Fluxes version 2 scheme. Thus, spatial resolution is improved from 1∘by 1∘to 0.25 ∘by 0.25 ∘and temporal resolution is improved from daily to 2-4 times daily.
Air-sea surface fluxes of sensible and latent heat provide energy to tropical cyclone; they are vital role in typhoon-ocean interaction research. To obtain such flux information under cyclone’s wind condition, the latest high-wind transfer coefficients from field and laboratory experiments are used. Also, impact of typhoon’s self-induced SST cooling is incorporated in the flux estimation to obtain more realistic fluxes. With the high-wind flux estimations, all 40 tropical cyclones, including depression, tropical storm, and typhoons during July to September from 2003-2005 are studied. Wind shear is also estimated and jointly analyzed with the flux data to study typhoon’s intensity change. It is found that typically typhoons can intensify under wind shear value of less than 10 ms-1. When vertical wind shear is small and with sufficient flux supply, typhoons may rapidly intensify. Insufficient flux supply from ocean or moving to high wind shear region or landfall are the causes for typhoon’s intensity decay. | en |
| dc.description.provenance | Made available in DSpace on 2021-06-13T03:31:30Z (GMT). No. of bitstreams: 1 ntu-95-R93229012-1.pdf: 1520468 bytes, checksum: 90e040a42d78e79094aa5a1967528c7c (MD5) Previous issue date: 2006 | en |
| dc.description.tableofcontents | Table of Contents
List of Tables……………………………………………………..ii List of Figures……………………………………………………iii Chapter 1 Introduction….…………………………………………1 Chapter 2 Improvement on air-sea flux estimation under normal condition…………………………………………………….4 2.1 Introduction………………………………………….……4 2.2 The Goddard Satellite-based Surface Turbulent Fluxes, version 2 scheme…………………………………………………… 5 2.2.1 Basic description………………………………… 5 2.2.2 GSSTF2’s near surface air humidity and other input data derived from SSM/I……………………………………8 2.3 Improvement on GSSTF2 flux estimation…………… 12 2.3.1 Improvement on sea surface temperature…… 12 2.3.2 Improvement on surface wind……………………14 2.4 Summary of improvements……………………………… 15 2.5 Validation of the estimated fluxes…………………15 Chapter 3 Estimation of air-sea fluxes under typhoon condition...............................................18 3.1 Introduction………………………………………………18 3.2 Transfer coefficients under high wind condition…19 3.3 Incorporation of inner-core sea surface temperature cooling in flux estimation……………………… 20 Chapter 4 Application on typhoon intensity change…………24 4.1 Introduction……………………………………………… 24 4.2 Estimation of vertical wind shear…………………………24 4.3 Typhoon’s intensification…………………………… 26 4.3.1 Average condition for shear and flux…………26 4.3.2 Case study1: Comparison of two cases both under weak shear but of different flux supply…………… 27 4.3.3 Case study 2: cases showing intensification once wind shear decreases…………………………………………27 4.4 Typhoon’s decay………………………………………… 28 4.4.1 Intensity decay due to land…………………… 28 4.4.2 Intensity decay due to increase in shear……28 4.4.3 Intensity decay due to insufficient flux……29 Chapter 5 Conclusion……………………………………………… 30 References…………………………………………………………… 32 | |
| dc.language.iso | en | |
| dc.title | 利用衛星估算海氣通量及其與颱風強度的關係 | zh_TW |
| dc.title | Estimation of Air-sea Fluxes by Remote Sensing-
Improvements and Application on Typhoon Intensity Change | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 94-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 劉振榮,周佳,吳俊傑,吳清吉 | |
| dc.subject.keyword | 海氣通量, | zh_TW |
| dc.subject.keyword | air-sea flux, | en |
| dc.relation.page | 72 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2006-07-28 | |
| 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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