| 东海黑潮主段环流子结构研究 |
| |
| 引用本文： | 陈红霞,袁业立,华锋,熊学军,郭炳火.东海黑潮主段环流子结构研究[J].海洋科学进展,2006,24(2):137-145. |
| |
| 作者姓名： | 陈红霞 袁业立 华锋 熊学军 郭炳火 |
| |
| 作者单位： | 国家海洋局,第一海洋研究所,山东,青岛266061;海洋环境科学和数值模拟国家海洋局重点实验室,山东,青岛266061 |
| |
| 基金项目： | 国家重点基础研究发展规划项目——东海黑潮结构变异及其与陆架水的相互作用(G1999043802)，国家海洋局青年海洋科学基金——东海黑潮主流段环流子结构及其动力机制初步研究(G2003201)，国家高技术研究发展计划项目——LADCP/LADP测量和资料处理技术(2002AA639590) |
| |
| 摘 要： | 通过对多种调查资料的综合分析,提出了东海黑潮主段子环流系统的物理模型,它是由较稳定的东海黑潮主段、经常出现(大概率)的右侧逆流和有条件出现(小概率)的外陆架逆流所构成的一个双环环流结构。部分黑潮水由主段北部进入陆架区形成外陆架逆流,或转向黑潮以东海域形成右侧逆流;由主段南部进入黑潮的陆架水,一部分来自外陆架逆流闭合了双环结构的外陆架部分;黑潮右侧逆流水大部分形成反气旋流动重新进入主流,闭合了双环结构的东部部分。
|
| 关 键 词： | 东海黑潮主段 外陆架逆流 右侧逆流 双环结构 |
| 文章编号： | 1671-6647(2006)02-0137-09 |
| 收稿时间： | 2005-11-26 |
| 修稿时间： | 2005年11月26 |
Study on Circulation Substructure in the Main Part of the Kuroshio in the East China Sea |
| |
| CHEN Hong-xia,YUAN Ye-li,HUA Feng,XIONG Xue-jun,GUO Bing-huo.Study on Circulation Substructure in the Main Part of the Kuroshio in the East China Sea[J].Advances in Marine Science,2006,24(2):137-145. |
| |
| Authors: | CHEN Hong-xia YUAN Ye-li HUA Feng XIONG Xue-jun GUO Bing-huo |
| |
| Institution: | 1. First Institute of Oceanography, SOA, Qingdao 266061, China; 2. Key Lab of Marine Science and Numerical Modeling, SOA, Qingdao 266061, China |
| |
| Abstract: | In this paper,a physical pattern of subcirculation system in the main part of the Kuroshio in the East China Sea is suggested by analyzing different survey data,and the subcirculation system is a double-loop circulation structure consisting of a relatively stable main stream of the Kuroshio,a frequently occu-ring right side countercurrent and a conditionally occurring outer shelf countercurrent.Part of the Kuroshio water from the north part of the Kuroshio main stream flows into the shelf area to form the outer shelf countercurrent,or turns to flow into the sea area east of the Kuroshio to form the right side countercurrent;part of shelf water coming from the outer shelf countercurrent flows into the Kuroshio from the south part of the Kuroshio main stream to close the outer shelf branch of double-loop structure,and most of the Kuroshio right side countercurrent water forms anti-cyclonic flow and returns to the Kuroshio main stream to close the east branch of double-loop structure. |
| |
| Keywords: | main part of the Kuroshio outer shelf countercurrent right side countercurrent double-loop structure |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
