衛星資料估算颱風旋轉及強度變化在熱帶氣旋定量降雨預測之研究

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研究生：	陳嬿如 Yen-ju Chen
論文名稱：	衛星資料估算颱風旋轉及強度變化在熱帶氣旋定量降雨預測之研究 Typhoon Quantitatiive Precipitation Forecast with Satellite-Derived Rotation and Intensity Variation of Tropical Cyclone
指導教授：	劉振榮 Gin-rong Liu
口試委員:
學位類別：	碩士 Master
系所名稱：	地球科學學院 - 大氣物理研究所 Graduate Institute of Atmospheric Physics
畢業學年度：	95
語文別：	中文
論文頁數：	106
中文關鍵詞：	熱帶降雨潛勢、熱帶氣旋
外文關鍵詞：	tropical cyclone, TRaP(Tropical Rainfall Potential)
相關次數：	點閱：9 下載：0
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查詢本校圖書館目錄查詢臺灣博碩士論文知識加值系統勘誤回報

近年來，因颱風造成的災害越來越嚴重。颱風挾帶的豪大雨和衍生的土石流，常導致人員和財產的重大損失。因此颱風定量降水預報為目前防災最重要的課題之一。
Kidder等(2005)利用SSM/I、TMI及AMSU等被動式微波資料估算熱帶氣旋降雨，參考官方預報颱風路徑資料，利用平移方法預測24小時後豪大雨的潛勢預報(Topical Rainfall Potential，TRaP)，此技術提供一種快速又實用的方法估算定量降雨，應用此方法預測降雨比數值模式的預測更接近於實際觀測(Ferraro等，2005)，但是TRaP仍然有許多待改進的空間，例如:TRaP方法中，假設颱風降雨的空間分布不會改變，忽略了颱風會旋轉且強度會改變的事實。
TRaP是美國官方目前使用預報颶風24小時累積降雨量的方法。本篇研究希望改進TRaP方法的假設，考慮颱風旋轉及強度變化的影響。本研究使用SSM/I衛星觀測資料反演降雨率，並用同步衛星紅外線資料估算颱風的旋轉角度及強度變化，預測颱風未來6小時內的累積降雨量，最後和島嶼測站的降雨資料相比較。研究結果發現考慮颱風的旋轉及強度變化對於改進降雨的估算能提升準確度，只考慮颱風的平移時，其累積降雨和測站真實觀測的相關係數為0.79，若同時考慮平移、旋轉與強度變化相關係數可增加為0.96。

In recent year, the damages caused by typhoons are more and more serious.The heavy rainfall from typhoons often causes inland flooding and mudslides that threaten lives and property which affect the livelihood of people. One of the most important areas of typhoon research focuses on the quantitative prediction of a typhoon’s precipitation.
The forecasting from American agencies use the TRaP method to predict a hurricane’s accumulated rainfall for the next 24 hours. This technique is considered fast and practical. The main purpose of this study is to also apply the TRaP method, but take into account the influence from a typhoon’s rotation and intensity variation. This research uses SSM/I data, GOES-9 data and MTSAT data to estimate the instant rainfall brought forth by typhoons between 2003~2005 around Taiwan. The accumulated rainfall is projected every six hours, and compared with the actual rainfall data recorded from the island’s weather stations. The study’s results indicate that by also considering the rotation and intensity of a typhoon, it will further improve the accuracy of the rainfall estimates. The correlation coefficient of accumulated rainfall between station and the method only concern about advection is 0.79.If we consider the advection, rotation and intensity variation of typhoon, the correlation coefficient can increase to 0.96.

摘要....................................................................................................................I
致謝.................................................................................................................III
目錄.................................................................................................................VI
表目錄...........................................................................................................VII
圖目錄.............................................................................................................IX
第一章 緒論.....................................................................................................1
1 前言..............................................................................................1
2 文獻回顧......................................................................................2
3 研究動機與目的..........................................................................5
第二章 資料蒐集與處理.................................................................................8
1 GOES-9和MTSAT衛星資料.......................................................8
1.1  GOES-9衛星.....................................................................8
1.2  MTSAT衛星.....................................................................9
2 GOES-9與MTSAT相關性分析.................................................10
3 SSM/I衛星資料..........................................................................12
4 JTWC最佳路徑資料..................................................................14
5 島嶼測站雨量資料....................................................................14
第三章 研究方法...........................................................................................15
1 降雨反演式介紹........................................................................15
2 決定颱風移動方向與移動速度................................................17
3 估算熱帶氣旋旋轉角度............................................................18
4 估算熱帶氣旋強度變化............................................................19
4.1 去除任一參數之測試結果.............................................20
4.2 參數1之測試結果(半徑100~300公里之亮溫標準差)…
………………………………………………………….20
4.3 參數2之測試結果(半徑50~200公里亮溫小於-20˚C之面
積百分比)……………...……………………………….21
4.4 參數3之測試結果(半徑0~30公里之最大亮溫)……21
4.5 參數4之測試結果(半徑0~30公里最大亮溫之距離)…22
4.6 參數5之測試結果(半徑20~120公里之最小亮溫)……23
4.7 參數6之測試結果(半徑20~120公里最小亮溫之距離)…
………………………………………………………….23
5 熱帶氣旋強度與降雨之關係....................................................24
第四章 結果分析與討論.............................................................................. 26
1 估算熱帶氣旋強度變化之結果討論........................................26
1.1  2003年南卡颱風...........................................................27
1.2  2003年蘇迪勒颱風.......................................................28
1.3  2003年莫拉克颱風.......................................................28
1.4  2003年杜鵑颱風...........................................................29
1.5  2004年敏督利颱風.......................................................29
1.6  2004年艾利颱風...........................................................30
1.7  2005年瑪莎颱風…………………...............................31
2 考慮颱風旋轉與強度變化預測降雨之結果............................31
2.1  2003年南卡颱風...........................................................32
2.2  2003年蘇迪勒颱風.......................................................32
2.3  2003年莫拉克颱風.......................................................33
2.4  2003年杜鵑颱風...........................................................34
2.5  2004年敏督利颱風.......................................................34
2.6  2004年艾利颱風...........................................................35
2.7  2005年瑪莎颱風...........................................................36
3 綜合討論....................................................................................36
第五章 結論與未來展望...............................................................................38
參考文獻.........................................................................................................41
附表.................................................................................................................45
附圖.................................................................................................................63

                                

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