• 温跃层声纳探测有着重要影响。

    The thermocline is important to the sonar detection.

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  • 沿南美洲西海岸温跃层十年间变化

    Interdecadal variability of the thermocline along the west coast of South America.

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  • 介绍大洋环流理论通风温跃层研究主要进展

    This paper introduces the major advances in the studies of the ventilated thermocline theory of ocean circulation.

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  • 温跃层对于潜艇水下航行战斗具有十分重要的意义。

    Thermocline is important for submarine in underwater navigation and action.

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  • 使海洋温跃层得以保持合理厚度一个重要原因

    This is an important factor in the maintenance of a reasonable thickness of thermocline.

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  • 分析结果对认识海域海洋温跃层分布特征可以提供有益参考

    The analysis results provide beneficial reference for deeper under standing of the distribution characteristics of the thermocline in this ocean area.

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  • 这种温跃层异常上升事件期间此区西风异常的出现赤道两侧应力旋度增大有着密切关系

    The anomalous lift of the thermoclines was associated closely with the west wind anomaly and intensification of positive wind stress curl on both sides of the equator.

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  • 较强陆坡区超临界地形上生成,并沿波射线方向传播,导致半日潮全日能量密度陆坡区温跃层较强。

    The semi-diurnal and diurnal internal tide energy densities are large on the continental shelf and in the thermocline of the deep sea.

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  • 揭示了当赤道东印度洋海区温跃层变浅时,温跃层反馈作用会加强由此引起IOD模态强度增加其他特征改变

    With a shoaling of the EEIO thermocline, the thermocline feedback strengthens, and this leads to an increase in IOD variance and other characteristics changing.

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  • 主要结果如下:海表应力影响温跃层动力因子,对季节性温跃层深度强度重大影响,但大洋温跃层的影响不大;

    The main conclusions are as follow: 1. The wind stress of sea surface is one dynamical factor of thermocline, which has important effect on intensity and depth of the seasonal thermocline.

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  • 第四章对历年表层流资料进行统计分析,给出了开辟区的温盐和表层流的分布特征和年变化特征:(1)表层水温夏季南高特点,温盐跃层薄,中心位置50~120之间变化;

    In summer, the temperature of the south part of the area is higher than the north part. Both the main thermocline and the main halocline are thin and their depths range from 50 to 120m.

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  • 第四章对历年表层流资料进行统计分析,给出了开辟区的温盐和表层流的分布特征和年变化特征:(1)表层水温夏季南高特点,温盐跃层薄,中心位置50~120之间变化;

    In summer, the temperature of the south part of the area is higher than the north part. Both the main thermocline and the main halocline are thin and their depths range from 50 to 120m.

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