Progressive internal waves on slopes

Author:

Wunsch Carl

Abstract

The refraction of progressive internal waves on sloping bottoms is treated for the case of constant Brunt—Väisälä frequency. In two dimensions simple, explicit expressions for the changing wavelengths and amplitudes are found. For small slopes, the solutions reduce to simple propagating waves at infinity.The singularity along a characteristic is shown to be removable, though the solutions are now inhomogeneous waves. The viscous boundary layers of the wedge geometry are briefly considered with the inviscid solutions remaining as interior solutions.A theory valid for small slopes is obtained for three-dimensional waves. The waves are refracted in the usual manner, turning parallel to the beach in shallow water.

Publisher

Cambridge University Press (CUP)

Subject

Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics

Reference8 articles.

1. Wunsch, C. 1968 On the propagation of internal waves up a slope Deep-Sea Res. 25,251–258.

2. Gaul, R. D. 1961 Observations of internal waves near Hudson Canyon J. Geophys. Res. 66,3821–30.

3. Sandstrom, H. 1966 On the importance of topography in generation and propagation of internal waves. Ph.D. Thesis,Univ. of California at San Diego.

4. Lee, O. S. 1961 Observations of internal waves in shallow water Limnol. Oceanogr. 6,312–21.

5. Phillips, O. M. 1966 The Dynamics of the Upper Ocean .Cambridge University Press.

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