摘要
1983午5月至1984年5月,我所对台湾海峡中、北部海域(24°30′N—26°00′N、121°00′E以西)进行了综合调查,对所取得的温、盐度及定点测流资料分析得出:6月至8月间,在调查海域西侧近岸海区存在着上升流现象,与上升流现象有关的近表层海水低温、高盐和高密(σ(?))出现在海坛岛附近海区。初步分析,调查海区西侧近岸海区上升流现象的成因,是来自海峡南部的海峡暖流水从海峡南部北上,经过调查海域时,由于受海底地形的影响,使近岸海区水文状况发生变化。
Based on analysis of the data collected by Fujian Oceanology Institute in the middle and north Taiwan Strait (in the area west of 121°E between 24°30′ and 26°N) from May 1983 to July 1984, the distributions of temperature. Salinity and density reveal coastal upwelling in the middle and north-western area of Taiwan Strait between June and August. The analysis shows that the upwelling is induced by the interaction of the northward warm water and the local seabed topography.
出处
《海洋湖沼通报》
CSCD
北大核心
1989年第4期8-12,共5页
Transactions of Oceanology and Limnology
