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浅海环流研究的一种新方法
引用本文:杨殿荣,魏皓,徐静琦.浅海环流研究的一种新方法[J].中国海洋大学学报(自然科学版),1994(3).
作者姓名:杨殿荣  魏皓  徐静琦
摘    要:提出在较强夏季跃层存在条件下的一种研究浅海环流的新方法。该方法是根据海洋温度和盐度的时间和空间变化资料.以及该水层通过其边界(海-气或跃层)所进行的热量和质量交换,计算环流的流速和流向。作为实例,对南黄海冷水团区进行了试验,结果表明,该方法合理、可行。

关 键 词:浅海  环流  新方法  温跃层  贯跃层混合  卷挟速度

A NEW METHOD FOR THE STUDY OF CIRCULATION SHALLOW SEA
Yang Dianrong, Wei Hao, Xu Jingqi.A NEW METHOD FOR THE STUDY OF CIRCULATION SHALLOW SEA[J].Periodical of Ocean University of China,1994(3).
Authors:Yang Dianrong  Wei Hao  Xu Jingqi
Institution:College of Physical and Environmental Oceanography
Abstract:A new method for studying the circulation in a shallow sea with thermolines in Summer is described. Using the temporal and spatial variations of the temperature and salinity, and the heat and mass exchanges between the layer and its surroundings through the boundaries, the current speed and direction can be calculated. As an example, the circulation of the cold waters in the South Huanghai Sea is calculated. The results show that this method is feasible.
Keywords:Shallow sea  circulation  new method  thermocline  cross thermocline mixing  entrainment velocity
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