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warm current相关的网络例句

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与 warm current 相关的网络例句 [注:此内容来源于网络,仅供参考]

By using the NCEP reanalysis data to run POM, the basical characteristics of the Kuroshio Current, the large-scale anticyclonic warm vortex on the right of it, and the SCS warm current are well simulated. The feature of the great influence of the monsoon on the SCS currents is also shown.

4使用NCEP再分析资料驱动区域海洋模式POM,较好地模拟出了黑潮海流、黑潮右侧的大尺度反气旋性暖涡及南海暖流等海流的基本特征,并反映出南海海流受季风影响较大的特点。

The wind forcing is the most important factor(80%) for generating the JB cyclonic gyre In addition the wind forcing drives the Liman Current and damos the East Korean warm Current in the Winter , and generates the UTB eddies along the Japan Nearshore Branch in all seasons .

风强迫是产生日本海盆气旋性式涡旋的最重要的因素(80%)。此外,风强迫在冬季驱动了Liman Cold Current流,抑制了东朝鲜暖流,并且在全年都产生UTB涡旋和沿着日本近岸分支的一些涡旋。

The wind forcing is the most important factor(80%) for generating the JB cyclonic gyre In addition the wind forcing drives the Liman Current and damos the East Korean warm Current in the Winter , and generates the UTB eddies al ong the Japan Nearshore Branch in all seasons .

风强迫是产生日本海盆气旋性式涡旋的最重要的因素(80%)。此外,风强迫在冬季驱动了Liman Cold Current流,抑制了东朝鲜暖流,并且在全年都产生UTB涡旋和沿着日本近岸分支的一些涡旋。

The high density area of Sagitta enflata was distributed at the warm current side of the mixed waters formed by Taiwan Warm Current and Chinese Coastal Current and that of Sagitta nagae was located at the side of northern Chinece Coastal Current.

肥胖箭虫高丰度区往往位于台湾暖流与浙江沿岸流交汇处偏暖水的一侧,海龙箭虫高丰度区位于暖流与沿岸流交汇处偏冷水团的一侧。

The climatological mean and seasonal variability of the current systems are well inverted, especially the Tsushima Warm Current and its bifurcation, the East Korean Warm Current, the Japan nearshore branch, the confluence of the EKWC, and the North Korean Cold Current near the Korean coast and flows northeastward along the subpolar front, and a mesoscale anticyclonic eddy in the Ulleng/Tsushima Basin.

日本海的环流系统的季节变化都作了较好的模拟,特别是对马暖流和它的分叉、东朝鲜暖流,日本近岸分支、东朝鲜暖流汇流、朝鲜半岛沿岸的本朝鲜寒流、以及一个Tsushima海盆中尺度顺时针涡旋。

The Taiwan Warm Current and the Tsushima Warm Current flow northward over the shelf in the East China Sea.

台湾暖流和对马暖流均为沿中国东部海域大陆架的北向流。

The water of the Tsushima Warm Current is of multi source in summer: the Taiwan Warm Current, the branch of the Kuroshio, the mixed water of the Yangtse Diluted Water with the West Korea Coast Current.

夏季进入朝鲜海峡的对马暖流的来源是多方面的,其中有:台湾暖流、黑潮分支、长江冲淡水与西朝鲜沿岸流的混合水。

In this paper, a general description of circulation in the Japan Sea is made, some controversial issues including the origin and structure of the Tsushima Warm Current are summarized, and some scientific problems with the Japan Sea remain un solved, these problems include the long-term variations and variation causes of volume transport of the Tsushima Warm Current, the disappearance of the East Korean Warm Current and its mechanism, the transport path and affecting factors of the Japan Sea Proper Water, and the causes for some variations in the Japan Sea and their responses to the global changes.

概述了日本海环流状况,着重介绍了对马海峡、郁陵海盆环流情形和日本海特征水团;总结了目前仍存在的争议问题,如对马暖流源头、对马暖流空间结构等;指出了目前日本海尚待解决的科学问题,如对马暖流流量的长期变化及其原因、东韩暖流消失现象及其机制、日本海特征水的传播路径及其影响因素、日本海的某些变化产生原因及其与全球变化的响应等。

Including several factors, the circulation numerical experiment in the Yellow Sea and East China Sea reconstructed the Kuroshio, the Taiwan Warm Current, the Tsushima Warm Current, the Yellow Sea Warm Current, coast currents and so on fairly well.

在各因素共同作用下的黄海东海环流数值模拟中,模式较好地再现了黑潮、台湾暖流、对马暖流、黄海暖流和沿岸流等各环流流系。

The numerical experiment reconstructed fairly successfully the circulation patterns of the Kuroshio, the Taiwan Warm Current, the Tsushima Warm Current and coast currents.

各因素共同作用下的黄海东海总流场数值模拟中,模式较好的再现了黑潮、台湾暖流、对马暖流、黄海暖流和沿岸流等各环流流系。

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然而,正如其名字所指出的那样,CD盘不能写,也不能用任何方式改变其内容。

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