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1
題名:The Kuroshio Fronts and Cold Eddies off Northeastern Taiwan Observed by NOAA-AVHRR Imageries    
以NOAA衛星AVHRR影像觀測臺灣東北海域黑潮鋒面及冷水?之研究
著者:Chi-Yuan Lin(林志遠) ;Chung-Zen Shyu(徐崇仁) ;Wen-Hung Shih(施文鴻)
出版地區:台灣
出版城市:台北市
學科:地球科學
刊名:Terrestrial, Atmospheric and Oceanic Sciences
卷期:3卷3期(1992.9)
頁碼:225-242
語言:英語
摘要: 中文摘要PDF ; 英文摘要PDF

自1989年10月至1989年12月間,共選用百餘張AVHHR-HRPT衛星水溫影像,用以觀測和分析臺灣東北海域之表層水文動態(以北緯26度,東經123度?中心,東西約350公里,南北約280公里),以下?結果摘要: 在本觀測海域(KEEP海域),黑潮鋒面型態可歸納?三型:(A)黑潮鋒面自臺灣東北一帶沿岸向東北方向延伸。(B)黑潮鋒面自臺灣東北一帶沿岸往東北方向前進,而後形成一反時鍾方向之曲折渦流。(C)黑潮鋒面順著北臺灣沿岸往外海先向西繞了一個圓弧形後再轉向東方。另外,臺灣東北外海的冷水團也是一主要之水文現象。在本海域的冷水團亦依其相對於黑潮鋒面之關係而劃分?三種型式:(A)冷水團形成於無明顯鋒面時。(B)冷水團形成於黑潮鋒面之冷水側(西側)。(C)冷水團形成於黑潮鋒面之暖水側(東側)。 黑潮鋒面A型主要盛行於夏季時,至於其他三個季節,三種鋒面均有可能發生且有所變動,而其侵入陸棚之程度亦有所不同。至於冷水團,最常出現的是B型,於各季節均有可能發生|其次是A型,較盛行於夏季;最少出現的是C型,較常出現於冬季。對黑潮鋒面和冷水團之關系,最常出現的情形是冷水團B型伴隨著黑潮鋒面A型。
Over a hundred AVHRR-HRPT thermal imageries of NOAA satellites which covered dimensions 350 Km (columns)×280 Km (rows) with center point at 26°N and 123°E, period from October 1989 to December 1990, had been derived to observe the surface features of waters off northeasern Taiwan. The patterns of Kuroshio fronts in this water (KEEP area) can be generalized to three types: (A) front extending away from northeastern Taiwan northeastwardly, (B) front extending away from northeastern Taiwan north- eastwardly, then turning into an anticlockwise frontal eddy, and (C) front extending westward along coast of northern Taiwan then away with an arcuate curve and turning to east. The locations of cold eddies, another major phenomenon in this area, can also be generalized to three types related to Kuroshio fronts: (A) eddy formed with no Kuroshio fronts around, (B) eddy located on cool (west) side of fronts, and (C) eddy located on warm (east) side of fronts. Front Type-A is the dominant and most stable pattern in summer. On the contrary, in other seasons, all three front types are variable and have different degrees of intrusion onto shelf waters. Regarding the cold eddies, the most common is Type-B, probably existing in each season. The next most common is Type-A, which prevails in summer. The least common is Type-C, which usually appears in winter. Regarding the relationship between front types and eddy types, the most prevailing composition is the cold eddy Type-B associated with the front Type-A.




本卷期目次
Terrestrial, Atmospheric and Oceanic Sciences 3卷3期 (1992.9)
The Kuroshio Fronts and Cold Eddies off Northeastern Taiwan Observed by NOAA-AVHRR Imageries/ Chi-Yuan LinChung-Zen ShyuWen-Hung Shih
The Year-Round Upwelling at the Shelf Break Near the Northern Tip of Taiwan as Evidenced by Chemical Hydrography/ Kon-Kee LiuGwo-Ching GongSaulwood LinChao-Yeuh YangChing-Ling WeiSu-Cheng PaiChong-Kung Wu
The Variability of Hydrographic Fields at Kuroshio's Turning on Northeast of Taiwan/ Jian-Hwa HuJia-Leh Chang
On the Characteristics of Bottom Tidal Currents in Northeast Taiwan/ Chong-Kung Wu
Summer Phytoplankton Community Structure in the Kuroshio Current-Related Upwelling Northeast of Taiwan/ Yuh-Ling Lee
Quantity and Quality of Summer Surface Net Zooplankton in the Kuroshio Current-Induced Upwelling Northeast of Taiwan/ Houng-Yung ChenYuh-Ling Lee
Comparison of Ichthyoplankton Guild in the Kuroshio Edge Exchange Area/ Chih-Shin ChenTai-Sheng Chiu
Larval Fish Composition, Distribution and Assemblages by Scientific Sounder from Eight Stations off Northeastern Taiwan/ Shinn-Pyng Yeh
Distribution of Organic Carbon in the KEEP Area Continental Margin Sediments/ S. LinK. K. LiuM. P. ChenP. ChenF. Y. Chang
Lead-210 and Polonium-210 Across the Frontal Region between the Kuroshio and the East China Sea, Northeast of Taiwan/ Chao-Yeuh YangHui-Ching Lin
Composition and Texture of Surface Sediment Indicating the Depositional Environments off Northeast Taiwan/ Min-Pen ChenKen-Ling LinShen-Chung Lo
Physiographic Characteristics of the Continental Margin, Northeast Taiwan/ Ho-Shing YuEason Hong
A Preliminary Study of the Echo Characters and Sedimentary Processes along the Continental Margin, Northeast of Taiwan/ Eason HongHo-Shing YuI-Shih-Chen
 
   
 
   

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