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目前,在海流研究中广泛地采用了Fourier方法,本文尝试用位势理论及象方法,从所解决的问题来看,后者有较广的应用范围,而且求解过程简捷、严密。 文中简捷地给出了无限深度的风海流的解,而且首次求出了有限深度情况中的普遍解。本文还研究了近岸处的风海流。对任意风胁强的情况给出了无限深度与有限深度时所述问题的解。在K.Hidaka的带状风系假定下,解的形式比K.Hidaka的解简单得
At present, the Fourier method is widely used in ocean current research. This paper attempts to use the geopotential theory and image methods. From the perspective of the problems solved, the latter has a wide range of applications and the solution process is simple and tight. In this paper, the solution of infinite depth wind currents is given simply and the general solution in the case of finite depth is obtained for the first time. This paper also studies the wind currents at the nearshore. The solution to this problem is given for infinite depths and finite depths for any windward strong case. In K. Hidaka’s belt-shaped wind assumption, the solution is simpler than K. Hidaka’s solution