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黑潮

与 黑潮 相关的网络例句 [注:此内容来源于网络,仅供参考]

During the PDO warm phase, however, there is a significant tropospheric biennial oscillation for the coupled interannual oscillations over these regions In addition , it seems to have a stronger correlation with the SST of the tropical eastern Pacific summer.

结果表明PDO冷暖位相中夏季江淮地区降水量与太平洋海温年际耦合振荡周期和强度均存在显著差异PDO冷位相中,夏季江淮地区降水与前期冬季西南太平洋和同期夏季黑潮区海温在7~8a时间尺度上的耦合最显著,而在PDO暖位相中,与这些地区海温呈现极显著的准2a耦合振荡,并且与同期夏季赤道东太平洋地区海温的准2a耦合振荡也迅速加强。

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。

Indicated by many other researchers, may be related to the Holocene Optimum.

许多早期研究揭示的黑潮在7.5-7kaB.P的加强可能与全新世大暖期有关。

By use of the observational and numerical methods, the interaction of Kuroshio SSTA and the East Asian monsoon are studied in this paper.

本文利用统计分析和数值模拟的方法研究了黑潮区域海温异常与东亚季风之间的相互作用,得到了以下结论。

This study is part of research on the Kuroshio edge exchange process.

本研究为黑潮边缘交换过程大型计划之部分。

Therefore, the former divergence in the understanding of the Kuroshio deformation is solved.

本文的研究结果系统地论述了吕宋海峡黑潮形变的时空分布特征和形成机制,统一了前人对该问题的不同认识。

A process of detaching of a warm ring from the Kuroshio is simulated successfully.

模拟出了黑潮分离流环的形成和脱离过程。

The most powerful ocean current in Pacific Ocean is Kuroshio.

太平洋中最强大的海流就是黑潮

The results show that Kuroshio deformation takes the perpetual shape of'loop'in Luzon Strait.

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。

When the north transport of Kuroshio is large, the west transport through Luzon Strait is small.

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。

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The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

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