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研究生:朱芳儀
研究生(外文):Chu,Fang-Yi
論文名稱:亞洲邊緣海域海表面溫度變化研究
論文名稱(外文):Variations of Sea Surface Temperature in the Asian Marginal Seas
指導教授:何宗儒何宗儒引用關係
指導教授(外文):Ho,Chung-Ru
口試委員:郭南榮鄭志文
口試日期:2019-07-03
學位類別:碩士
校院名稱:國立臺灣海洋大學
系所名稱:海洋環境資訊系
學門:自然科學學門
學類:海洋科學學類
論文種類:學術論文
論文出版年:2019
畢業學年度:107
語文別:中文
論文頁數:37
中文關鍵詞:海表面溫度亞洲邊緣海域線性迴歸趨勢
外文關鍵詞:sea surface temperatureAsian marginal seaslinear regressiontrend
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本研究使用1982至2017年衛星海洋表面溫度資料,探討亞洲七個邊緣海域,包括日本海、黃海、東海、南海、泰國灣、安達曼海和孟加拉灣的海表面溫度變化趨勢。所使用的數據是取自美國海洋暨大氣總署系列衛星的先進極高解析度輻射儀,以非線性演算法推導出的海表面溫度資料。研究結果顯示緯度高低對於溫度變化趨勢有影響,各邊緣海域溫升趨勢為日本海上升0.0384 ℃/年、黃海上升0.0240 ℃/年、東海上升0.0288 ℃/年、南海上升0.0192℃/年、泰國灣上升0.0108 ℃/年、安達曼海上升0.0120 ℃/年、孟加拉灣上升0.0144 ℃/年,整體而言中緯度的邊緣海域海表面溫度上升趨勢較低緯度邊緣海域快。同樣現象也出現在每年最高溫及最低溫的趨勢,中緯度的邊緣海域在每年最高溫的上升趨勢較快,而低緯度的邊緣海域則是在每年最低溫的上升趨勢較快,惟最高溫的上升趨勢較為明顯。再比較夏季和冬季的平均上升值,中緯度的日本海、黃海和東海在夏季平均上升值較高,低緯度的南海、泰國灣、安達曼海和孟加拉灣則是在冬季平均上升值較高。
This study used satellite sea surface temperature (SST) data from 1982 to 2017 to explore the SST trends in seven Asia marginal seas, including the Japan Sea, the Yellow Sea, the East China Sea, the South China Sea, the Gulf of Thailand, the Andaman Sea, and the Bay of Bengal. The SST data are derived using nonlinear algorithms derived from the Advanced Very High Resolution Radiometer onboard the US Oceanic and Atmospheric Administration (NOAA) series of satellites. Research results show the SST trends are related to latitude. The SST is rising at each marginal sea with a rate about 0.0384 ℃/year for the Sea of Japan, 0.0240 ℃/year for the Yellow Sea, 0.0288 ℃/year for the East China Sea, 0.0192 ℃/year for the South China Sea, 0.0108 ℃/year for the Gulf of Thailand, 0.0120℃/year for the Andaman Sea, and 0.0144 ℃/year for the Bay of Bengal. Generally, the SSTs rise faster in the marginal seas at mid-latitude than that at low-latitude. The same phenomenon also occurs in the trend of the annual highest SST and the annual lowest SST. The SST rising trends are higher with the annual highest SST at mid-latitude marginal seas, while are higher with the annual lowest SST at low-latitude marginal seas. However, the rising trend of the annual highest SST is more obvious. Comparing the average rising trend in summer and winter, the marginal seas at mid-latitude have a higher value of average SST trend in summer, while the marginal seas at low-latitude have a higher value of average SST trend in winter.
誌謝......I
摘要......II
Abstract......III
目錄......IV
圖目錄......V
表目錄......VI
第一章 前言與研究目的......1
1.1研究動機......1
1.2研究區域概述......1
第二章 文獻回顧與探討......4
第三章 研究資料與方法......7
3.1 研究資料......7
3.2 研究方法......8
第四章 研究結果與討論......11
第五章 結論......34
參考文獻......36
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