Abstract

The expressions for the velocity potential and the surface elevation are obtained for the three dimensional motion on surface waves generated by a surface pressure F(x, y)ei ωt, t>0, on the surface of a deep sea. The wave integrals are asymptotically evaluated for large distances and times by the method of stationary phase. By a direct passage to the limit t→∞, the steady state solution of the problem is evaluated in exact terms. The results are illustrated for a class of physically plansible pressure distributions on the surface. Some features of the wave motions are discussed.

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