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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。
A new method of studying shallow-sea circulation is proposed under the condition of strong summer thermocline. The method is based on temporal and spatial variations of ocean temperature and salinity. As well as the exchange of heat and mass from the water layer through its boundary (sea-gas or thermocline), to calculate the velocity and direction of circulation. As an example, experiments were carried out on the South Yellow Sea chilled water mass. The results show that the method is reasonable and feasible.