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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 許晃雄 | |
| dc.contributor.author | C.-W. June Chang | en |
| dc.contributor.author | 張瓊文 | zh_TW |
| dc.date.accessioned | 2021-06-14T16:55:01Z | - |
| dc.date.available | 2008-08-05 | |
| dc.date.copyright | 2008-08-05 | |
| dc.date.issued | 2008 | |
| dc.date.submitted | 2008-07-30 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/40661 | - |
| dc.description.abstract | 本研究運用模式資料分析南海及菲律賓海的海洋表層動力對海溫年際變化之影響。對南海區域的海平面高度作EOF分析，得到的前兩個mode與ENSO有極高的相關性。第一個mode的高峰值發生在12月，影響南海的冬季環流，在聖嬰年南海的冬季上層海洋環流減弱，海溫異常增暖。第二個mode的高峰值發生在8月，使聖嬰發展年的夏天，越南外海向東的冷平流強度(約12°N)增強，海溫下降；聖嬰衰減年的夏天，越南外海向東的冷平流強度減弱，海溫上升。由於El Niño Modoki 年(例如1994、2002年)的海溫分佈特徵，使得西北太平洋夏季季風(WNPSM)較1997年強，南海的上層海洋環流受到增強的西風影響，帶來較強的冷平流。
利用模式資料分析1997/1998年聖嬰事件，發現大氣對海洋有正的熱通量，但海溫出現負距平，可見海溫的變化被海洋動力所主導。分析1955到2004年海洋上層400米之海洋熱容量顯示，菲律賓海的溫躍層有顯著的年際變化。在聖嬰年，西太平洋溫躍層的舉升可將冷海水帶至較表層區域，當有混合作用產生，則可將溫躍層的冷水混合至表面，是使表層海溫呈負距平的主要可能因素。而溫躍層舉升的機制為其對應North Equatorial Current與North Equatorial Counter Current兩洋流強度及位置變化產生的地轉調整，與受來自中太平洋羅士培波的影響。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-06-14T16:55:01Z (GMT). No. of bitstreams: 1 ntu-97-D92229005-1.pdf: 4094061 bytes, checksum: 6ae2893d8531325f820c8775d9017dd3 (MD5) Previous issue date: 2008 | en |
| dc.description.tableofcontents | Table of Content
ABSTRACT I 中文摘要 IV TABLE OF CONTENT V LIST OF TABLES VII LIST OF FIGURES VIII LIST OF FIGURES VIII CHAPTER 1 - INTRODUCTION 1 CHAPTER 2 - INTERANNUAL VARIABILITY OF THE SOUTH CHINA SEA IN A DATA ASSIMILATION MODEL 5 2.2. MODEL DESCRIPTION 6 2.3. EOF ANALYSIS OF SSH 8 2.4. CORRELATION WITH ENSO 10 2.5. WINTER UPWELLING MECHANISM 12 2.6. SUMMARY 14 CHAPTER 3 - INTERANNUAL MODE OF SEA LEVEL IN THE SOUTH CHINA SEA AND THE ROLES OF EL NIÑO AND EL NIÑO MODOKI 21 3.1. INTRODUCTION 21 3.2. EL NIÑO-RELATED CIRCULATION AND SST 23 3.3. ANOMALOUS ATMOSPHERIC CONDITIONS DURING THE SUMMERS OF 1994, 1997 AND 2002 25 3.4. REGRESSED WIND FIELD ON EL NIÑO AND EL NIÑO MODOKI 29 3.5. SUMMARY AND DISCUSSIONS 31 CHAPTER 4 - UPPER OCEANIC PROCESSES IN THE PHILIPPINES SEA AND THEIR RELATIONS TO THE INTERANNUAL SEA SURFACE TEMPERATURE VARIABILITY 38 4.2 OBSERVATIONS 41 4.2.1 Covariability of SST and thermocline depth 42 4.2.2 Heat Content analysis 42 4.2.3 Variations of TAO ocean temperature along 8°N 43 4.2.4 Interannual variations of zonal current velocity and NECC Trough 44 4.3 MODELING STUDIES OF THE 1997/98 EL NIÑO 45 4.3.1 Model Description 45 4.3.2 SST Anomalies and Surface Heat Flux 46 4.3.3 Vertical Structure 48 4.3.4 Non-local Rossby waves 50 4.3.5 SST Cooling 51 4.4 SUMMARY 52 REFERENCE 69 APPENDIX - MODEL VALIDATION 81 A.1 THERMOCLINE STRUCTURE IN THE EQUATORIAL PACIFIC OCEAN 81 A.2 INTERCOMPARISON OF TAO ARRAY BUOY, JEDAC AND OFES SIMULATIONS OF TEMPERATURE ANOMALY 82 | |
| dc.language.iso | en | |
| dc.title | 南海及菲律賓海之海洋上層環流對海表面溫度年際變化的影響 | zh_TW |
| dc.title | Influence of upper oceanic dynamics on Sea Surface Temperature in the Philippine Sea and the South China Sea: structure and interannual variability | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 96-2 | |
| dc.description.degree | 博士 | |
| dc.contributor.oralexamcommittee | 柯文雄,隋中興,鄒治華,余嘉裕,唐存勇,曾于恆 | |
| dc.subject.keyword | 南海,菲律賓,海洋環流,海表面溫度,年際變化, | zh_TW |
| dc.subject.keyword | South China Sea,Philippine Sea,sea surface temperature,upper ocean dyanmics,interannual variability, | en |
| dc.relation.page | 79 | |
| dc.rights.note | 有償授權 | |
| dc.date.accepted | 2008-07-30 | |
| 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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