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多重衛星影像應用於台灣東部黑潮時空動態指標之建立

  • 日期:98-04-21
  • 年度:2007
  • 領域:漁業領域
  • 主持人:曾振德
  • 研究人員:陳世欽、曾振德、劉姵妤

本研究利用多重衛星遙測影像及現場水文觀測資料,探討台灣東部海域黑潮暖流之時空分佈特性,並解析黑潮動態與鮪延繩釣漁獲分佈之相關性。初步分析結果包含:(1)已完成處理NOAA衛星AVHRR海面水溫資料共1,225幅。另已蒐集處理EOS衛星MODIS海面水溫資料共1,331幅及海洋水色資料共696幅。並已完成處理1997至2006年TOPEX衛星Poseidon月平均海面高度距平值資料共120幅。且所有衛星資料再轉換成ArcGIS地理資訊系統數值圖層。(2)由1987-2006年台灣周邊海域之Argos衛星浮標資料分析結果,顯示台灣東部黑潮表層水之平均流速夏季時期大於冬季時期,夏季之平均流速為125-150cm/sec,最大值發生於台東外海,流速為170cm/sec。冬季之平均流速為75-100cm/sec,最大值發生於蘇澳外海,流速為101cm/sec。(3)由1991-2007年間台灣周邊海域之Sb-ADCP流速流向資料分析結果,顯示水深200米以淺的黑潮水,其流速以夏季時期達最大值,平均流速50cm/sec以上的黑潮水幅寬範圍約75浬。(4)由Argos及Sb-ADCP流速流向資料分析,顯示冬季時期之黑潮暖流於通過台灣東北海域時,有明顯入侵東海陸棚區現象,且並顯示出台灣東部黑潮暖流於北緯24度以北海域,有夏季離岸冬季近岸的季節分佈特性。(5)本研究定義黑潮暖流生態指標-KCCF為SeaWiFS衛星海洋水色濃度0.2 mg m-3等值線,顯示黑潮暖流KCCF指標於台灣東部海域呈現經度向動態變化,於高緯度之日本南方海域,則呈現出顯著的緯度向時空變化。關鍵詞:多重衛星遙測影像、黑潮暖流、地理資訊系統、海面水溫、海洋水色

研究報告摘要(英)


The present study had investigated the relationship between tuna longline fishery and spatio-temporal variations of Kuroshio Current derived from multi-sensor satellite data. The preliminary results were listed as follows: (1) The 1,225 NOAA/AVHRR sea surface temperature (SST) data, 1,331 EOS/MODIS SST data, 696 EOS/MODIS ocean color (chlorophyll-a concentration) data, and the 120 monthly average TOPEX/Poseidon sea surface height anomaly data had been applied and transferred into the ArcGIS point or raster layers in this study. (2) Analyze to the Kuroshio Current velocity measured by the Argos satellite buoys from 1987 to 2006 had shown that the larger average current velocity was 125-150 cm/sec, found in Tai-Dong coastal water during the summer time. Its maximum value was 170 cm/sec. Conversely, the less average current velocity was 75-100 cm/sec, found in Su-Ao coastal water during the winter time, its maximum value was 101 cm/sec. (3) The Sb-ADCP data from 1991 to 2007 was examined to find out the maximum current velocity happened in the summer time from surface to 200m water depth in the Kurosio Current waters off eastern Taiwan. The covering width of Kuroshio Current defined by the high current velocity more than 50cm/sec was about 75 nautical miles. The seasonal Sb-ADCP current vectors also showed the Kuroshio surface and subsurface water usually intruded onto the continental shelf of East Chin Sea in the winter time. (4) The seasonal variations of Kuroshio main stream was examined by the Argos and Sb-ADCP data, and showed that its main axis closed to the eastern Taiwan in the winter time and left for offshore in the summer time. (5) In this study, the Kuroshio Current Chlorophyll Front (KCCF) was defined to be a useful ecological indicator. And the longitudinal migration of the KCCF was evident, found in the eastern Taiwan coastal waters. However, the remarkable latitudinal migration of the KCCF was found in the southern Japan coastal waters.