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本文是文献[3]研究工作的继续。利用文献[3]中所用的海-气边界层模式,重点考虑海深和底坡的影响,将该文的研究成果直接推广到有限深海的情形,和无限深海情形下所获得的相应结果进行比较,简洁地阐明两者的异同,并就海底摩擦以及浅海风暴潮的估值和导致风暴潮的发生和发展的大气强迫力作一简短讨论。
This article is the continuation of the literature [3]. Based on the sea-gas boundary layer model used in reference [3], the influence of sea depth and bottom slope is mainly considered, and the research result of this paper is directly extended to the limited deep sea case and the corresponding result obtained under the infinite deep sea condition Compare and briefly explain the similarities and differences between the two, and give a short discussion on the valuation of the seabed friction and the shallow-sea storm surges and the atmospheric coercion that has led to the occurrence and development of the storm surge.