Abstract
In a non-adiabatic, viscous, atmosphere, a finite number of lower (large-scale) modes of motion determines all the remaining modes, since the higher (small-scale) modes are strongly damped due to frictional force and dissipation function and only replicate with decreased amplitude the fundamental modes of oscillation (in particular, they have the same kind of spectrum).
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(1991). Deterministic Chaotic Behaviour of Atmospheric Motions. In: Meteorological Fluid Dynamics. Lecture Notes in Physics Monographs, vol 5. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-38386-4_9
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DOI: https://doi.org/10.1007/978-3-540-38386-4_9
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