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- W2077881132 startingPage "2003" @default.
- W2077881132 abstract "The problem considered is that of small amplitude vertical oscillations of a viscous isothermal atmosphere. The viscosity coefficient μ is assumed to be constant. It is shown that in any fixed z interval (z being the vertical coordinate) for frequencies below a critical frequency, the solution approaches (as μ → 0) the solution of the inviscid problem for which the kinetic energy in a column of fluid is finite. For frequencies higher than the critical one, however, viscosity not only damps the motion at large altitudes, but also reflects waves downward. The solution does not go to a Iimit as μ → 0, but the ratio of the amplitudes of the reflected and the incident wave approaches exp(−πβ), where β is the ratio of the vertical scale height to the wavelength. For small β, therefore, the solution of the inviscid problem satisfying the radiation condition is not accurate." @default.
- W2077881132 created "2016-06-24" @default.
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- W2077881132 date "1967-06-01" @default.
- W2077881132 modified "2023-09-27" @default.
- W2077881132 title "EFFECT OF VISCOSITY ON VERTICAL OSCILLATIONS OF AN ISOTHERMAL ATMOSPHERE" @default.
- W2077881132 cites W2255212672 @default.
- W2077881132 doi "https://doi.org/10.1139/p67-157" @default.
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