Vertical oscillations in a viscous and thermally conducting isothermal atmosphere

The presence of dissipation in an isothermal atmosphere may cause upwardpropagating small amplitude waves to be reflected downward. For an atmosphere with small dynamic viscosity μ this was demonstrated in Yanowitch (1967b); this will be referred to as case II. Here two problems will be investigated...

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Veröffentlicht in:	Journal of fluid mechanics 1974-11, Vol.66 (2), p.273-288
Hauptverfasser:	Lyons, Patrick, Yanowitch, Michael
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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