江苏近海的环流动力研究进展  

Advances in the Offshore Circulating Current of Jiangsu

作　　者：秦毅[1] 

机构地区：[1]河海大学海岸灾害及防护教育部重点实验室,环境海洋实验室,南京210098

出　　处：《科学技术与工程》2009年第12期3389-3394,共6页Science Technology and Engineering

基　　金：教育部博士学科点专项基金(200502940009)

摘　　要：江苏海域地形复杂,既有中部的辐射沙洲地形,又有北部的海州湾水下浅滩地形,具有特殊的海洋动力条件。全面了解江苏沿海的环流动力机制,包括江苏近海的冷水锋、江苏外海的冷水团、沿岸流、海州湾和吕泗海区的上升流以及江苏近海的激流现象等,以便进一步研究江苏沿海的地形形成的动力机制,这对于江苏沿海的开发利用具有很大的实用价值。The sea area terrain of the Jiangsu Province, including the radial sand ridges in the middle and the shoal topography in the Haizhou Bay to the north, is complex, therefore with the specific dynamics conditions of the marine. To know more about the offshore circulation and its dynamics of Jiangsu, consisting of the cold water front, the cold water mass,the longshore current,the upwelling in the Haizhou Bay and the Lvsi sea area, and the storm current, then it couid study further about the dynamics conditions of forming the coastal topography of Jiangsu. It will be widely worthy to exploiting and utilizing the Jiangsu coast practically.

关 键 词：江苏近海 冷水锋 冷水团 沿岸流 上升流 激流 

分 类 号：P731.21[天文地球—海洋科学]