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Evanescent acoustic gravity modes in the isothermal atmosphere: systematization and applications to the Earth and solar atmospheres

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Figure

Table 2 shows all evanescent modes that coincide with eachother at the points of intersection of the dispersion curves,and between which interaction is possible
Table 1. Properties of different evanescent acoustic-gravity modes.
Table 3. The change in energy density of evanescent modes with height in an infinite isothermal atmosphere.
Fig. 3c, d). The long-wave branch is acoustic, and anotherbranch with kx ≥ 0.4H1 is surface gravity by its physical na-ture.
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