西风漂流
大洋海水在盛行西风的吹送下，大规模自西向东流动形成的海流。狭义的西风漂流即为南极绕极环流；广义的还包括北半球因受地理条件制约，分别在大西洋、印度洋、太平洋所形成的区域性海流，如北大西洋海流、北太平洋海流等。
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contributed at 2011-10-13
Classification(s)
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Earth System(in Chinese) Marine geology
Detailed Description
| English |
|---|
| Name | west wind drift |
| Chinese |
|---|
| Name | 西风漂流 |
| Description | 大洋海水在盛行西风的吹送下，大规模自西向东流动形成的海流。狭义的西风漂流即为南极绕极环流；广义的还包括北半球因受地理条件制约，分别在大西洋、印度洋、太平洋所形成的区域性海流，如北大西洋海流、北太平洋海流等。 |
How to Cite
NNU_Group (2011). 西风漂流, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/a6328e2d-2224-49f9-b6f7-15c92dfc2423
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