北大西洋暖流
墨两哥湾暖流到达西经45º附近以后，继续向东北运行，斜穿大西洋，形成北大西洋暖流。在北纬50º，西经20º附近分为三支，一支向南流，形成加那利寒流，一支向西北，叫伊尔明格海流，流向冰岛南部；一支流向东北，沿挪威海岸流动，形成挪威暖流。北大西洋暖流对西欧和北欧的气候有很大影响。
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contributed at 2011-12-26
Classification(s)
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Earth System(in Chinese) Marine Geography
Detailed Description
| English |
|---|
| Name | North Atlantic Current |
| Chinese |
|---|
| Name | 北大西洋暖流 |
| Description | 墨两哥湾暖流到达西经45º附近以后，继续向东北运行，斜穿大西洋，形成北大西洋暖流。在北纬50º，西经20º附近分为三支，一支向南流，形成加那利寒流，一支向西北，叫伊尔明格海流，流向冰岛南部；一支流向东北，沿挪威海岸流动，形成挪威暖流。北大西洋暖流对西欧和北欧的气候有很大影响。 |
How to Cite
NNU_Group (2011). 北大西洋暖流, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/f15ce6da-7dd3-47fe-8982-2bd189e9a75f
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