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自从V.W.Ekman提出著名的风漂流理论,以及B.Helland-Hansen提出著名的梯度流公式以来,海流理论获得了极其迅速的发展。K.Hidka and Y.Akiba,J.J.O’Brienand R.O.Reid,J.E.Geisler,B.丑.Ry~oB,C.Cooper and B.Pearce等已经做了十分有意义的台风流的现场观测、数值模拟和理论研究工作。 本文为台风海流研究的初始阶段结果。其目的在于,探讨轴对称定常台风作用下的海流结构,从而使我们对它的流速和水温的空间分布,有些探索性的了解。
Since the famous theory of wind drift by V.W.Ekman and the famous gradient flow formula proposed by B.Helland-Hansen, the theory of ocean current has developed extremely rapidly. K. Hidka and Y. Akiba, JJ O’Brien and ROReid, JEGeisler, B. U. Ry-oB, C. Cooper and B. Pearce, et al. Have made very significant observations and numerical simulations of typhoon currents Theoretical research. This article is the initial stage result of typhoon current study. The purpose is to explore the ocean current structure under the action of axisymmetric steady typhoon, so that we can make some exploratory understandings on the spatial distribution of its velocity and water temperature.