对马暖流

在九州西南海域，黑潮表层流并无分支北上进入对马暖流区。

There was no surface branch of the Kuroshio flowing northward and entering the area of the Tsushima Warm Current , southwest of Kyushu .

日本海海水表层温度的变化主要是与东亚季风、对马暖流的流量、亚极地锋的位置变化等因素密切相关。

The glacial-interglacial SST variation in the Japan Sea is considered to be closely related to changes in the East Asian monsoon system , the volume transport of the Tsushima Warm Current ( TWC ) and the position of the sub-polar front ( SPF ) .

另外，在这支上面提到的海流路径上31°N附近有时会出现逆流，这主要受对马暖流流入朝鲜海峡的流量大小控制。

Sometimes a countercurrent appears on the path of the above mentioned current near 31 ° N , which is mainly controled by the flow of the Tsushima Current passing through the Korea Strait .

对马暖流为在黑潮主干西侧沿100～200m等深线流动的一支海流与黄海大陆沿岸流的混合。

The Tsushima is a mixture of the current flowing along the 100-200m isobath on the west side of the Kuroshio and the coastal current in the Yellow Sea .

而对马暖流的季节变化，局地强迫和遥强迫都起着重要作用。

Both local and remote forcings play important roles in the seasonal variation .

研究结果进一步验证了台湾-对马暖流系统的存在。

The research validates the existence of " TSWC-TWC system " further more .

夏季对马暖流区黑潮水与陆架水的相互作用&兼论对马暖流的起源

Interaction of Kuroshio water and shelf water in the Tsushima Current region in summer

对马暖流（表层）来源的探讨

On source of Tsushima current in surface layer

同时，模式很好地模拟了该海域的黑潮、台湾暖流、对马暖流、黄海暖流以及沿岸流等主要环流。

The model has simulated Kuroshio , Taiwan Warm Current , Tsushima Current , the Yellow Sea Warm Current , and Coast Current .

对马暖流西侧的水体是东海混合水，而其东侧为黑潮分支。

The water in the west side of Tsushima Warm Current is a mixed water of East China Sea and the water in its east side is a branch water coming from the Kuroshio .

研究结果更加清晰、形象、直观地展示了黑潮及其向对马暖流的分支，台湾暖流的分叉，和黄海暖流、长江冲淡水及涡旋发达海区的若干主要特征。

The results demonstrate more clearly and directly some main features about the Kuroshio and its branch ( to the Tsushima Warm Current ), the separation of the Taiwan Warm Current , the Huanghai Sea Warm Current , the Changjiang diluted water and the eddy developing area .

台湾岛东北海域内潮响应强烈主要是受黑潮锋和地形的影响。对马暖流西侧的水体是东海混合水，而其东侧为黑潮分支。

The northeast of the Taiwan Island is due to the Kuroshio and its topography . The water in the west side of Tsushima Warm Current is a mixed water of East China Sea and the water in its east side is a branch water coming from the Kuroshio .