长江口海区上升流现象的数值模拟  

NUMERICAL SIMULATION OF UPWELLING IN THE CHANGJIANG RIVER MOUTH AREA

作　　者：赵保仁[1] 李徽翡[1] 杨玉玲[1] 

机构地区：[1]中国科学院海洋研究所

出　　处：《海洋科学集刊》2003年第1期64-76,共13页Studia Marina Sinica

基　　金：国家自然科学基金资助项目;496762 79号;国家重点研究发展规划资助项目;G1 9990 43 80 8号

摘　　要：With the vertical velocity obtained by POM for simulating the circulation in the East China Seas,the upwelling and downwelling in the Changjiang River Mouth area are discussed. This simulation showed convincingly that upwelling exists in the area of the northern part of the Changjiang River Mouth; and that the downwelling which exists in its southern part which separates the upwelling at the Changjiang River Mouth from the Men and Zhe coastal upwelling. This simulation showed that the upwelling at the Changjiang River Mouth is caused by interaction of the Taiwan Warm Current with the slope bottom topography; and that southwest the monsoon in summer can strengthen the upwelling at the Changjiang River Mouth and the Men and Zhe coastal upwelling.With the vertical velocity obtained by POM for simulating the circulation in the East China Seas,the upwelling and downwelling in the Changjiang River Mouth area are discussed. This simulation showed convincingly that upwelling exists in the area of the northern part of the Changjiang River Mouth; and that the downwelling which exists in its southern part which separates the upwelling at the Changjiang River Mouth from the Men and Zhe coastal upwelling. This simulation showed that the upwelling at the Changjiang River Mouth is caused by interaction of the Taiwan Warm Current with the slope bottom topography; and that southwest the monsoon in summer can strengthen the upwelling at the Changjiang River Mouth and the Men and Zhe coastal upwelling.

关 键 词：上升流 下降流 台湾暖流 流速分布 真光层 盐度分布 数值模拟 长江冲淡水 初级生产力 近岸环流 

分 类 号：P731.27[天文地球—海洋科学]