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1 Introduction
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2 The equilibrium layer
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3 The reduction of the adiabatic wave equation
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4 The solutions of the wave equation
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5 The dispersion relation of the modes
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6 Discussion of the dispersion relations
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7 Relations to the modes of a polytropic layer with an overlying isothermal atmosphere
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8 The continuous spectrum
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9 Vertically propagating waves
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10 Conclusions
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References
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