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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 劉平妹 | |
| dc.contributor.author | Yung-Chiang Lin | en |
| dc.contributor.author | 林永強 | zh_TW |
| dc.date.accessioned | 2021-06-07T17:54:12Z | - |
| dc.date.copyright | 2012-08-20 | |
| dc.date.issued | 2012 | |
| dc.date.submitted | 2012-08-16 | |
| dc.identifier.citation | Akitomo, K., Ooi, M., Awaji, T., and Kutsuwada, K., 1996, Interannual variability of the Kuroshio transport in response to the wind stress field over the north Pacific: Its relation to the path variation south of Japan: Journal of Geophysical Research-Oceans, v. 101, p. 14057-14071.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/15873 | - |
| dc.description.abstract | 本研究分析了台灣鄰近海域的潮位資料及衛星測高資料，希望能夠了解近五十年來西北太平洋的海水面長期變動速率，及造成其變動之原因。另外與北太平洋多個氣候指數比較討論其相關性，希望能歸納海水面週期性變動的原因。
根據潮位資料，台灣鄰近海域的海水面變化在1969-2009、1975-2009、以及1993-2009三個時段的海水面變化速率，分別為2.4mm/yr、2.7mm/yr以及4.9mm/yr，另外衛星資料顯示本研究區域內的平均海水面變化速率為5.0mm/yr明顯大於全球平均3.4mm/yr。而密度變化的海水面變化則為0.79mm/yr，1mm/yr以及3.1mm/yr同樣呈現變快的現象。並由衛星資料與密度資料的平均相關係數高達0.8，可知密度變化為造成近期海水面變化之主因。但是海水面的變化趨勢，會隨時間變動，多數測站在1991年之後海水面呈現加速上升的現象，代表利用現在的海水面變化速率去推估未來的變化有其不確定性。空間分布上，衛星資料1993-2009期間顯示海水面變大致為低緯度速率大於高緯度的，但是潮位站的結果則不明顯。 影響西太平洋的氣候指數可簡單分為三類，分別是PDO-NPI-PNA，NPGO-NPO-WP以及ENSO，反映的是熱帶海溫之變化及阿留申低壓的強度變化及中心位置之經度變化。而低頻的氣候指數的影響，只有在北緯30度以北的測站較為明顯，可能是低頻的氣候變動，在溫帶地區較為明顯，抑或是因為潮位只有單點且影響因子眾多，不能明確表達區域海水面與氣候變動之關係。衛星資料與氣候指數的相關係數分布，顯示台灣鄰近海域的海水面變化明顯受到海洋物理參數及太平洋的氣壓變化所影響，造成海洋環流的增強或減弱，進而影響了海水面的變化，這點可能說明了ENSO與台灣東邊的黑潮之相關性。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2021-06-07T17:54:12Z (GMT). No. of bitstreams: 1 ntu-101-R97224215-1.pdf: 3832102 bytes, checksum: 626710bfadd0ba8a01bdd1291e19810e (MD5) Previous issue date: 2012 | en |
| dc.description.tableofcontents | 誌謝 I
摘要 II 目錄 III 圖目錄 VI 表目錄 IX 第一章 簡介 1 1.1前言 1 1.1.1 海水面之量測與全球海水面變化回顧 1 1.1.2西太平洋及台灣海水面變化文獻回顧 2 1.2氣候指數及其與西北太平洋氣候連動之文獻回顧 3 1.2.1 海洋表面物理參數 3 1.2.2海平面氣壓 5 1.2.3區域平均重力位高度 6 1.3研究目的 7 第二章 研究資料及研究方法 8 2.1研究資料 8 2.1.1 潮位站資料 8 2.1.2衛星資料 8 2.1.3上層海水溫度資料 8 2.1.4 地轉流速度資料 9 2.2研究方法 9 2.2.1初步資料檢驗 9 2.2.2線性迴歸 10 2.2.3 LOESS 10 2.2.4 移動平均 10 2.2.5相關係數的計算 10 2.2.6 EEMD 10 第三章 研究結果 13 3.1海水面的變化 13 3.1.1潮位站海水面長期變動 13 3.1.2衛星資料表示之海水面長期變動 13 3.1.3密度變化造成的海水面變化 13 3.2 EEMD結果 14 3.3觀測資料之間的相關性 14 3.3.1潮位站資料與衛星資料的比較 15 3.3.2 密度資料與衛星資料的相關性 15 3.4西北太平洋洋流流速變化 15 第四章 討論 17 4.1海水面變化的時間與空間差異 17 4.1.1不同時間區段變動速率之變化 17 4.1.2不同區域變化速率分布 17 4.2資料之間的相關 18 4.2.1潮位資料與衛星資料之相關性 18 4.2.2實際海水面變化與密度變化造成的海水面變化之比較 18 4.3西北太平洋與全球海水面變化之比較 18 4.4 EEMD結果之討論 19 4.4.1潮位站之間比較 19 4.4.2氣候指數之間的比較 20 4.4.3潮位站資料與氣候指數比對之討論 21 4.5冬天資料之比對 21 4.6衛星資料與氣候指數之比較 22 4.6.1衛星海表高與氣候指數之比較 22 4.6.2海流流速與氣候指數的相關性 24 第五章 結論 26 參考文獻 28 附圖 34 | |
| dc.language.iso | zh-TW | |
| dc.title | 台灣鄰近海域的海水面變化及其與北太平洋氣候連動之初探 | zh_TW |
| dc.title | The preliminary study of sea level variation around the regional sea of Taiwan and its connection with North Pacific climate | en |
| dc.type | Thesis | |
| dc.date.schoolyear | 100-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.coadvisor | 曾于恆 | |
| dc.contributor.oralexamcommittee | 謝孟龍 | |
| dc.subject.keyword | 海水面變化,北太平洋,氣候指數,潮位站,衛星測高,阿留申低壓,黑潮, | zh_TW |
| dc.subject.keyword | Sea level variation,North Pacific,Climate Index,Tide gauge,Satellite Altimetry,Aleutian Low,Kuroshio, | en |
| dc.relation.page | 73 | |
| dc.rights.note | 未授權 | |
| dc.date.accepted | 2012-08-17 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 地質科學研究所 | zh_TW |
| 顯示於系所單位： | 地質科學系 | |
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