埃尔尼诺现象与东海黑潮区及其邻近海域水文结构和环流的变异──东海黑潮区及其邻近海区ENSO渔场学问题之一  

VARIATION OF HYDROLOGIC STRUCTURE AND CIRCULATION IN RELATION TO ENSO EVENTS IN THE KUROSHIO AREA IN THE EAST CHINA SEA AND ITS ADJACENT SEAS

作　　者：何发祥[1] 洪华生[2] 

机构地区：[1]厦门大学海洋系 [2]厦门大学环科中心

出　　处：《海洋湖沼通报》1999年第1期16-24,共9页Transactions of Oceanology and Limnology

摘　　要：本文阐明ENSO现象与台湾岛东北部冷涡关系，在EN年（包括EN2年次年）夏季仅能出现东北型及该型双涡Ⅰ型，而非EN年和EN年（除夏季外）则出现东侧型和西侧型及双涡Ⅱ，Ⅲ型。此外还在前人研究基础上，给出东海东北部（非EN年和EN年除夏季外）环流图式和在EN年（包括EN2年次年）夏季环流图式。还对海洋锋等进行初步讨论。The relationship between ENSO events and the cold eddies northeast of Taiwan is described and interpretated. The northeastern boundary eddy and its double eddy Type Ⅰ were only found in the summer of EN years and/or the next year while the eastern boundary eddy, western boundary eddy, and double eddy types Ⅱ and Ⅲ occurred in non-ENSO years as well as other seasons (except summer).Based on the data of previous researchers, the authors generalize the circulation patterns in northeastern East China Sea and preliminerily discuss the problem of oceanic fronts.

关 键 词：埃尔尼诺 黑潮区 东海 水文结构 环流 

分 类 号：P731.1[天文地球—海洋科学] P732.6