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使用南岛语系的人与黑潮的图。The picture of the Austronesian languages human and Kuroshio.

冬季日本九州西侧海域存在一个半封闭的涡旋。Kuroshio intrusion engenders an eddy at the west of Kyushu Island of Japan.

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黑潮分支大约是该涡旋的主要动力因子。The branch of Kuroshio is the direct dynamic factor of the formation of this eddy.

此外，流经本区的黑潮对自生铁锰微结核的富集具有重要影响。In addition, Kuroshio plays a significant role in the enrichment of Fe-Mn micro-nodules.

黑潮延续体另一显著特征是主轴南北两侧的多涡结构。The eddy structure in both sides of the Kuroshio Extension is another distinct character.

研究结果表明，黑潮在吕宋海峡的形变以“流套”的形式常年存在。The results show that Kuroshio deformation takes the perpetual shape of'loop'in Luzon Strait.

未能观测到黑潮表层水和黑潮次表层水。And the Kuroshio Surface Water and the Kuroshio Subsurface water have not been found in winter.

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当黑潮源头向北的流量较大时，通过吕宋海峡向西的净流量偏小。When the north transport of Kuroshio is large, the west transport through Luzon Strait is small.

有些海域，例如黑潮区与气旋之间存在着交替影响的关系。There exists alternative influence from both factors in some oceanic areas such as Kuroshio region.

春季，黑潮对东海的影响范围较大，且各层次相差较小。In spring, Kuroshio occupies the most area of the East China Sea with little diversity in each layer.

强大的黑潮向北发送暖流，使珊瑚能够在通常难以被发现的地方茁壮成长。The powerful Kuroshio shoots warm water northward, allowing coral reefs to thrive where they would not normally be found.

分析了秋季黑潮区域海表温度异常与东亚冬季风以及我国冬季气候的关系。The relationship of autumn Kuroshio region SSTA with the East Asian winter monsoon and Chinese winter climate is analyzed.

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冲绳美丽海水族馆，因为拥有全世界第三大水缸“黑潮之海”而闻名于世，缸内含水7500吨。Okinawa Churaumi Aquarium, as has the world's third largest water tank, "Kuroshio Sea, " is famous, 7, 500 tons of water tank.

观测和数值模式研究都发现吕宋海峡局地季风风场在吕宋海峡黑潮流套的形成中不起决定作用。Both observations and model research attest local monsoon in Luzon Strait is not the critical dynamics factor to Kuroshio loop.

结果表明，在过去50年内，东海黑潮上层海温呈上升趋势，而上层盐度略呈下降趋势。Results reveal that the Kuroshio upper layer temperature experienced slight rise while salinity decreased in the past 50 years.

虽发现有黑潮水穿越巴上海峡进入南海，但其势力甚弱。Though the Kuroshio Water was found to enter into the South China Sea passed through the Bashi Channel, its influence was weak.

说明秋季东海同样存在陆架水与黑潮水在水平方向交换与混合。This shows that the Kuroshio water exchanges and mixes with the shelf water in horizontal direction in the East China Sea in autumn.

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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.

该冷水块是黑潮次表层水涌升的结果，是黑潮对我国近海海洋环境影响的典型实例之一。The cold water body results from the upwelling of subsurface Kuroshio water, which shows the influence of the Kuroshio on the Chinese marine environment.

另外，闽南地区后汛期降水量与同期NINO西海区和黑潮海区的海温成正相关关系。Otherwise, the normat correlation exists between the corresponding SST in west sea area of NINO and the Kuroshio and the summer rainfall in southern Fujian.