片语

Kuroshio intrusion黑潮流套

kuroshio region黑潮海区

Kuroshio path黑潮路径

Kuroshio loop黑潮流套

Kuroshio extension黑潮尾；黑潮延伸；[海洋] 黑潮续流；气球测标

Kuroshio SSTA黑潮区域海温异常

the kuroshio黑潮

Kuroshio countercurrent黑潮反流

Kuroshio Ichiba黑潮市场

英汉例句

• 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。

• 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 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 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 results show that Kuroshio intrudes onto the continental shelf of East China sea in large scale and during its flow water is exchanged ceaselessly with outer sea along Ryukyu Island.

  模拟结果表明黑潮在东海陆架有大规模的入侵，其在沿东海陆坡流动途中沿着沖绳岛与外海不断的进行水体交换。

• 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。

• 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。

• 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。

• 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着的联系。

• 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。

• 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。

• 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。

• 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 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蕩（PDO）及ENSO有着非常密切的关系。

• 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。

• 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 Kuroshio Loop and the circulation being induced in northern SCS may be affected by the variation of the Kuroshio itself and the subtropical circulation, as well as the width of the strait.

  吕宋海峡黑潮流套及南海北部的诱生环流之流型，会因黑潮本身以及副热带环流整体的变化而变化，也与海峡的宽度有关。

• 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。

• Three branches separating from Kuroshio flow toward the interior of the Yellow Sea, and formate three eddies respectively.

  冬季，黄海东部朝鲜沿岸流南下过程中，有三分支脱离其主体向黄海内部流动并形成三个涡旋。

• 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。

• The result shows that in North Pacific, ocean surface gains heat in summer and loses heat in winter, the net heat loss reaches its maximum, especially in Kuroshio Extension.

  分析结果表明：北太平洋海洋夏季凈得热，冬季凈失热，且黑潮及其延伸体区失热最大。