The results showed that the distribution of Trichodesmium erythraeum had relationship with the infall of Kuroshio current.
结果表明，红海束毛藻的分布与黑潮涌入有关。
The Kuroshio Current brings a huge variety of fish to Okinawa.
而黑潮洋流则给冲绳带来了品种繁多的鱼类。
Kuroshio intrusion engenders an eddy at the west of Kyushu Island of Japan.
冬季日本九州西侧海域存在一个半封闭的涡旋。
The previously winter Kuroshio SSTA relates greatly to the East Asian summer monsoon (EASM).
前期冬季黑潮区域海温异常与东亚夏季风存在显著的联系。
Theirconveyor belt was the Kuroshio (Black) Current, named after the deep colour ofits waters.
他们的“传送带”是黑潮——因其水流颜色而得名。
The anomalous Kuroshio transport has a close relationship with Pacific Interdecadal Oscillation (PDO) and ENSO.
黑潮输送异常和太平洋年代际振荡（PDO）及ENSO有着非常密切的关系。
The results show that:the SCS branch of the Kuroshio Current is an important part in the north SCS from Jan. to Aug.
模拟结果表明：1～8月，黑潮南海分支是南海北部的一支重要海流；
That the Kuroshio flowing along the vertical direction of PN section is approved byanalyzing current datum from LADCP.
通过LADCP海流资料分析确认研究区域黑潮与PN断面近似垂直。
The powerful Kuroshio shoots warm water northward, allowing coral reefs to thrive where they would not normally be found.
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 relationship of autumn Kuroshio region SSTA with the East Asian winter monsoon and Chinese winter climate is analyzed.
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。
During the winter the kuroshio oceanic current brings warm water of high salinity from the Pacific through the Luzon strait.
冬季期间，黑潮海流把高咸度的温暖海水由太平洋经吕宋海峡带入本港。
Okinawa Churaumi Aquarium, as has the world's third largest water tank, "Kuroshio Sea, " is famous, 7, 500 tons of water tank.
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。
During the winter, the Kuroshio oceanic current brings warm water of high salinity from the Pacific through the Luzon Strait.
冬季期间，黑潮海流把高咸度的温暖海水由太平洋经吕宋海峡带入本港。
Results show that there is a closely relation between the autumn Kuroshio region SSTA and the East Asian winter monsoon index.
结果表明：秋季黑潮区域海温与东亚冬季风指数有明显的正相关关系。
Results reveal that the Kuroshio upper layer temperature experienced slight rise while salinity decreased in the past 50 years.
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。
The selection of level of no motion is a basic problem in calculating the geostrophic flow in the East China Sea Kuroshio area.
零流面的选取是东海黑潮地转流计算中的一个基本问题。
Using the -coordinate POM model, the effects of variation for flow core position and flux on Kuroshio frontal meander are studied.
本文运用简化的坐标POM模式研究了东海黑潮锋面弯曲的产生与成长机制。
This shows that the Kuroshio water exchanges and mixes with the shelf water in horizontal direction in the East China Sea in autumn.
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。
There was no surface branch of the Kuroshio flowing northward and entering the area of the Tsushima Warm Current, southwest of Kyushu.
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。
Our objective is to examine the shift in the path of the Kuroshio and the interaction be-tween land and sea during the last glacial maximum (LGM).
目的在确定末次盛冰期时古黑潮流域模式以及海陆气候相互作用。
The results show that the period within a year during which the ocean releases its heat into the atmosphere is as long as 8 months over the kuroshio area.
结果指出，在黑潮区域，海洋表面每年有八个月向大气释放热量。
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.
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。
This paper USES TKC to reflect the volume transport of Kuroshio through the Tokara strait, analyzes the intra-annual and annual period of the volume of Kuroshio.
利用验潮站海表高度差反演吐噶喇海峡黑潮的流量，分析了黑潮流量的年内和年际变化。
In summer warm water species can also be found in the Yellow Sea but the diversity was much less than that in winter and short of typical species for Kuroshio water.
夏季，在黄海也可以发现许多暖水种，但种类数量远不如冬季多，而且少有黑潮水的典型种。
The main results arc as follows: 1 the thermal fronts appear obviously in the inner side left side of the stream axis of the Kuroshio in the sea area south of Japan.
主要结果：(1)日本以南海域黑潮流轴内侧存在着明显的呈带状分布的温度锋。
In this paper the relationship between ENSO (el Nino Southern Oscillation phenomena) and variability of oceanic front of the Kuroshio in the East China Sea are described.
本文讨论了厄·尼诺、南方涛动现象(ENSO)和东海黑潮锋变异的关系。
The results show that a large meander of the Kuroshio appeared again during 1986—1988. The formation, maturity and decline of this large meander are explored in this study.
指出1986～1988年期间，黑潮又发生一次大弯曲现象，并对这次大弯曲的生成、强盛、衰消过程做了分析。
The results show that a large meander of the Kuroshio appeared again during 1986—1988. The formation, maturity and decline of this large meander are explored in this study.
指出1986～1988年期间，黑潮又发生一次大弯曲现象，并对这次大弯曲的生成、强盛、衰消过程做了分析。
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