Abstract
The stability of sound waves in a polytropic atmosphere with thermal diffusion is discussed. Analytic results are obtained using the quasi-adiabatic approximation, and the consequences of using the optically thin and optically thick approximation are compared. An example is given of overstability with a subadiabatic temperature gradient. The quasi-adiabatic results are then compared with fully non-adiabatic numerical results, using a model of the 5-min oscillation of the Sun.

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