Title of article :
Decay Rates for a Two-Dimensional Viscous Ocean of Finite Depth
Author/Authors :
Donna Sylvester، نويسنده ,
Issue Information :
دوهفته نامه با شماره پیاپی سال 1996
Pages :
8
From page :
659
To page :
666
Abstract :
In 1888, A. M. Basset ‘‘A Treatise on Hydrodynamics,’’ Deighton, Bell and Co., Cambridge, 1888. gave a formal argument to show that slow modes of decay do not exist for the free surface and velocity field of a linearized, two dimensional, viscous, finite-depth ocean with small viscosity. His dispersion relation for waves of the form eik xqv t was v fO k2 .. His argument did not apply to very small wave- lengths large k.which are important to consider since nonlinear effects can cause small wavelengths to focus and form singularities. In Lamb’s book on hydrodynamics, there is a formal argument which shows that slow modes of decay exist for small wavelengths on the free surface of a linearized, two dimensional, viscous ocean of infinite depth if surface tension is neglected. There, Lamb showed that vfO 1rk.. The lack of boundary conditions on a fixed bottom makes the analysis somewhat easier than for the finite depth case. Lamb’s analysis, as well as Basset’s, relies on physical intuition rather than careful mathematical analysis}the smallness of certain quantities is assumed before the dispersion relation is derived. More importantly, both Basset and Lamb rely on a particular decomposition we will be specific below. of the stream function which becomes degenerate in the small wavelength limit. They obtain dispersion relations by setting to zero a determinant, but the zeros of that determinant do not all correspond to physically nontrivial pressures or velocities. Some zeros merely reflect the degeneracy of the decomposition they used. The purpose of this article is to warn others of this pitfall, while pointing out a simple direct method of calculation which avoids it. Our approach applies equally well to the cases of finite or infinite depth, with or without surface tension. In addition, our method yields a complete asymptotic expansion for the dispersion relation for small wavelengths. In order to obtain a complete expansion from other methods, one would have to decide at which point in the expansion small terms that were dropped would need to be reinserted, etc.
Journal title :
Journal of Mathematical Analysis and Applications
Serial Year :
1996
Journal title :
Journal of Mathematical Analysis and Applications
Record number :
929220
Link To Document :
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