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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 詹森(Sen Jan) | |
| dc.contributor.author | Yi-Chen Cheng | en |
| dc.contributor.author | 鄭伊宸 | zh_TW |
| dc.date.accessioned | 2022-11-23T08:58:50Z | - |
| dc.date.available | 2021-11-03 | |
| dc.date.available | 2022-11-23T08:58:50Z | - |
| dc.date.copyright | 2021-11-03 | |
| dc.date.issued | 2021 | |
| dc.date.submitted | 2021-10-27 | |
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/79359 | - |
| dc.description.abstract | 本研究探討臺灣東北海域湧升流區與東海南部大陸棚海域鎖管資源量年變化的物理海洋原因和背後的動力過程。研究中使用佈放於臺灣東北海域之彭佳嶼溫壓站資料,配合衛星影像資料、氣象資料及鎖管捕捉量等資料,以資料相關分析和海洋動力理論為基礎,探討臺灣東部黑潮主流的變動、東北海域湧升流區水溫及水位變動、季風變化、臺灣海峽北向流、冬季中國大陸沿岸南向流、北太平洋西行中尺度渦旋等動力過程的互制和影響鎖管資源量之關係。 研究結果顯示,在年際變化上鎖管的資源量與彭佳嶼水溫(資源量資料的前一年10月及同年4月)有正相關性,由於鎖管主要會在每年的3−5月與10−12月洄游至湧升流區附近海域繁殖產卵,通常較高的水溫有助於幼體發育,進而可以提高鎖管的資源量。透過衛星遙測海面溫度與絕對動力高度推算之絕對地轉流資料的分析,可以歸納出在鎖管主要產卵時期常常會有發生黑潮入侵東海南部大陸棚區的狀態,黑潮表層相對溫暖的海水被帶進湧升流區造成表水溫異常升高;再從風場資料與地轉流場、海面高度、海表溫的變動時序分析,推論造成黑潮入侵的原因包括:冬季在東北季風持續作用下向岸(向西北)的艾克曼輸送、東海陸棚水因冷空氣南移而冷卻下沉並順應大陸坡地形流出陸棚區,表層黑潮水作為補償向湧升流區靠近以及中尺度渦旋向西位移影響黑潮等。另外2012年與2016年沿著中國大陸東南海岸南下的中國大陸沿岸流比較強,為湧升流區帶來更多冷水,結果造成鎖管資源量在這兩年比較低的主要原因。由本研究分析得到的結果,希望可以做為預測臺灣東北部黑潮是否能入侵陸棚區的依據,並進一步做為預估鎖管資源量的參考。 | zh_TW |
| dc.description.provenance | Made available in DSpace on 2022-11-23T08:58:50Z (GMT). No. of bitstreams: 1 U0001-2610202109121000.pdf: 24063378 bytes, checksum: 21ab5a758ab6d738a81ce2bce45ac0e0 (MD5) Previous issue date: 2021 | en |
| dc.description.tableofcontents | 口試委員會審定書……………………………………………………………………...i 致謝……………………………………………………………………………………..ii 摘要……………………………………………………………………………………..iii Abstract………………………………………………………………………………….iv 目錄……………………………………………………………………………………..vi 圖目錄與表目錄………………………………………………………………………viii 第一章 前言…………………………………………………………………………….1 第二章 資料與分析方法……………………………………………………………….6 2-1 研究區域…………………………………………………………………..6 2-2 資料來源…………………………………………………………………..7 2-2-1 劍尖槍魷年別CPUE資料………………………………………...7 2-2-2 溫鹽壓儀資料……………………………………………………...8 2-2-3 氣象資料………………………………………………………….11 2-2-4 衛星遙測資料…………………………………………………….12 2-3 分析方法…………………………………………………………………14 2-3-1 迴歸分析………………………………………………………….14 2-3-2 相關分析………………………………………………………….14 2-3-3 同調性分析……………………………………………………….15 2-3-4 低通濾波………………………………………………………….15 2-4 分析結果…………………………………………………………………16 2-4-1 迴歸分析結果…………………………………………………….16 2-4-2 相關分析結果…………………………………………………….18 2-4-3 同調性分析結果………………………………………………….20 2-4-4 低通濾波結果…………………………………………………….21 2-5 黑潮入侵指標……………………………………………………………23 第三章 結果與討論…………………………………………………………………...25 3-1 黑潮入侵期間之衛星影像分析結果……………………………………25 3-2 造成劍尖槍魷資源降低之原因討論……………………………………55 第四章 結論與建議…………………………………………………………………...69 參考文獻……………………………………………………………………………….71 | |
| dc.language.iso | zh-TW | |
| dc.title | 東海南部大陸棚鎖管捕捉量與臺灣東北部湧升流區變動的關係及動力機制研究 | zh_TW |
| dc.title | Environmental dynamics for controlling the catch of swordtip squid off the northeast coast of Taiwan | en |
| dc.date.schoolyear | 109-2 | |
| dc.description.degree | 碩士 | |
| dc.contributor.oralexamcommittee | 曾于恒(Hsin-Tsai Liu),張明輝(Chih-Yang Tseng),王慧瑜 | |
| dc.subject.keyword | 劍尖槍魷,鎖管捕捉量,湧升流區,黑潮入侵,冷水入侵, | zh_TW |
| dc.subject.keyword | swordtip squid,catch of squid,upwelling area,Kuroshio intrusion,cold water intrusion, | en |
| dc.relation.page | 74 | |
| dc.identifier.doi | 10.6342/NTU202104200 | |
| dc.rights.note | 同意授權(全球公開) | |
| dc.date.accepted | 2021-10-28 | |
| dc.contributor.author-college | 理學院 | zh_TW |
| dc.contributor.author-dept | 海洋研究所 | zh_TW |
| 顯示於系所單位: | 海洋研究所 | |
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