东澳大利亚暖流
太平洋南赤道洋流在向西流动的过程中，受澳大利亚大陆，新几内亚岛等陆地的阻挡，大部分海水转向高纬流动，即沿澳大利亚东岸南下，然后汇入西风飘流，东澳大利亚暖流的温度和盐度较高，表层海水温度：南部约1 5℃；北部约25℃。盐度在3 5‰以上。
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contributed at 2011-12-26
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●
Earth System(in Chinese) Marine Geography
Detailed Description
| English |
|---|
| Name | East Ausrtrajian Current |
| Chinese |
|---|
| Name | 东澳大利亚暖流 |
| Description | 太平洋南赤道洋流在向西流动的过程中，受澳大利亚大陆，新几内亚岛等陆地的阻挡，大部分海水转向高纬流动，即沿澳大利亚东岸南下，然后汇入西风飘流，东澳大利亚暖流的温度和盐度较高，表层海水温度：南部约1 5℃；北部约25℃。盐度在3 5‰以上。 |
How to Cite
NNU_Group (2011). 东澳大利亚暖流, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/964ce6e5-2856-42c7-97b9-5a411a7a19be
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