1) South China Sea warm current
南海暖流
1.
Some observed discoveries in SCS in winter such as the South China Sea Warm Current (SCSWC)which is against wind flow.
冬季南海的一些观测事实在模式结果里得到了很好的反映 ,像冬季逆风向东北方向流动的“南海暖流”和一些中尺度涡旋 。
2.
Theresults are: (1) when driven by wind force, the flow state in the above area, especiallyTaiwan Shrait is seasonal, but the South China Sea Branch of Kuroshio is not shown,thereappears no existence of South China Sea Warm Current, but there exists an allyear cycloniceddy near Dongsha Islands.
利用1个正压的数值模式研究风应力、黑潮对南海东北部及台湾海峡环流的影响，结果为：（1）以风应力为驱动机制时其流态特别是在台湾海峡的流动具有季节性，但未反映南海黑潮分支的存在；在冬季也未见有南海暖流出现，但在东沙群岛附近海域终年存在着1个气旋涡；（2）以黑潮为驱动机制时，黑潮通过巴士海峡侵入南海海域，并导致东沙群岛附近气旋性涡旋的形成。
2) The Continental Shelf Warm Current in the East China Sea and South China Sea
东、南海陆架暖流
3) the South China Sea warm water
南海暖水
1.
In this paper why we should study the South China Sea warm water is explained and today s research results are described and some questions which should be studied about seasonal and interannual variability of the South China Sea warm water are proposed.
阐述了研究南海暖水的意义 ,综述了关于南海暖水的现状 ,提出了关于南海暖水季节和年际变化方面应该研究的问
4) South China Sea warm pool
南海暖池
5) Yellow Sea Warm Current
黄海暖流
1.
Zooplankton indication of the Yellow Sea Warm Current in winter;
冬季黄海暖流的浮游动物指示
2.
Diagnostic Computation of the Yellow Sea Warm Current in Winter;
冬季黄海暖流的诊断计算
3.
Study on Seasonal and Inter-annual Variations of the Yellow Sea Warm Current;
黄海暖流季节和年际变化研究
6) Huanghai Warm Current
黄海暖流
1.
On the origin and path of the Huanghai Warm Current during winter and early spring;
冬至初春黄海暖流的路径和起源
2.
In winter the Huanghai warm current has a great effect.
冬季的黄海暖流在渤海中的作用是非常显著的，它是使冬季渤海中部及南部水温明显高于北部辽东湾水温的重要原因。
补充资料：巴西暖流
南大西洋西部南美洲沿岸的暖流。大西洋南赤道洋流的南支，沿巴西东岸南流，在南纬40°附近，与西风漂流汇合。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条