黑潮

The first SVD mode shows that the anomalous heating in northern Kuroshio is associated with anomalously low geopotential height in the central and western parts of the North Pacific at 500 hPa.

第1对奇异向量占总方差的86.24%，表现为黑潮北部海域异常多的放热和北太平洋中西部的500hPa位势高度场异常低。

During the summer monsoon the center of the anticyclonic eddy, breaking off from the Kuroshio bend, can reach about°E and the eddy shedding periods are mainly 40-120 days.

夏季风期间，从黑潮弯曲中脱落的反气旋涡的中心位置可以达到117°E附近，反气旋涡脱落的周期集中在40-120天间。

E-117. 5°E . During the winter monsoon the location of the centers of the anticyclonic eddies, shedding from the Kuroshio bend are mainly at the east to 118°E and the eddy shedding periods are basically 40-90 days.

冬季风期间，从黑潮弯曲中脱落的反气旋涡的中心位置基本集中在118°E以东，反气旋涡脱落的周期集中在40-90天间。

By analyzing the temperature sections, stream functions and volume transport sections, the results show that the Antarctic Circumpolar Current is the strongest current in the world oceans, the Gulf Stream is stronger than the Kuroshio Current, and all of them are stronger in summer and weaker in winter.

从断面温度场、流函数分布和断面流量场等分析显示：南极绕极流堪称世界最强流，湾流整体强于黑潮，3者都具有夏季增强、冬季减弱的特点。

In this paper, the criteria and results for selecting the level of no motion are determined by comparing and analyzing the calculated geostrophic flow results at PN section in the East China Sea Kuroshio mainstream area corresponding to different selections of level of no motion and taking the main characteristic factors of the East China Sea Kuroshio into consideration.

通过对东海黑潮主流段PN断面上选取不同零流面时地转流计算结果的比较分析，考虑了东海黑潮的主要特征因子，确定了计算零流面的选取标准和选择结果。

In winter, the transport of Kuroshio is stronger than that in summer.

冬季黑潮流量大，黑潮弯曲的程度小，反气旋涡旋脱落的位置在118°E以东，脱落的周期缩短。

The trough is mainly confined by the continental slope to the north and by sloper off the Ryukyu volcanic islands.

东海海水与黑潮水在东海大陆棚坡区交换，而此地区的地形为不规则状，这种地形效应値得进一步探讨其对黑潮边缘交换过程的影响。

The source of the Tsushima Warm Current will change in the year: in January and February the main source is the flow from the Kuroshio; from March to August, the main source gradually changes from the Kuroshio to mixed water of the flow from the Taiwan strait and the Changjiang diluted water; after August, the main source changes back to be the Kuroshio.

对马暖流的来源全年均有所变化，一、二月以黑潮水为主；三月到八月，来源逐步从黑潮水转变为台湾海峡北上海流以及长江冲淡水的混合水；八月到九月，来源重新转变为黑潮水。

By this method, time series MODIS\|SST data were used to extract sea surface warm front of Kuroshio in East China Sea.

本文利用我国自主研发的海洋地理信息系统软件MaXplorer，以黑潮为例，阐述了基于过程的海洋形态特征提取方法，利用VC++，对MODIS水星SST时间序列数据进行海表温度锋抽取，并分析了2003年东海黑潮表层温度锋位置的季节性变迁。

In the northern part of the Okinawa Trough,at about 7.5-7.0kaBP of the early Holocene, this studied region was controlled by the continental shelf water, and at about 7.0aBP Kuroshio water combined with continental shelf water intensively, then the region was controlled by the intensified Kuroshio water with upwellings during 7.0-6.0kaBP; from 6.0-2.0ka BP the upwellings developed stably and the thermocline gradually declined: from 6.0-5.0 kaBP the impact of the upwellings mainly focused on the thermocline and much less on the sea surface, from 5.0-4.0kaBP the SST decreased because the sea surface was influenced by the cool water brought by the intensified upwellings; from 2.0-1.2kaBP, the upwelling declined and the SST increased consequently; since 1.2 kaBP the upwelling increased and the thermocline declined obviously.

冲绳海槽北部、九州西南海区，全新世7.5-7.0ka BP陆源物质影响明显， 7.0kaBP前后黑潮侵入并与陆架水强烈混合，7.0-6.0ka BP期间黑潮影响逐渐控制了该区，上升流开始发生，温跃层开始变浅；约在6.0-2.0ka BP之间上升流持续稳定发育，温跃层深度逐渐下降：6.0-5.0ka BP上升流影响作用于温跃层但对表层影响较小，5.0-4.0ka BP海水表层温度受上升流冷水影响降低；而约2.0-1.2ka BP，上升流减弱，海水表层温度回升；近1200年来上升流加强、温跃层深度减小的趋势更加显著。

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

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。