亲潮
又称千岛寒流，是北太平洋气旋型环流的组成部分。起源于白令海，从堪察加半岛沿着千岛群岛自东北流向西南，在北纬40°附近（日本北海道附近）与日本暖流相遇。亲潮主流的流速在1m/s以下，表面水温低于1 9℃，水色低，透明度小。
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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 | oyoshio |
| Chinese |
|---|
| Name | 亲潮 |
| Description | 又称千岛寒流，是北太平洋气旋型环流的组成部分。起源于白令海，从堪察加半岛沿着千岛群岛自东北流向西南，在北纬40°附近（日本北海道附近）与日本暖流相遇。亲潮主流的流速在1m/s以下，表面水温低于1 9℃，水色低，透明度小。 |
How to Cite
NNU_Group (2011). 亲潮, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/8f53b1b3-bb6c-455a-80e3-3f94ef8a117f
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