Abstract
It is shown that the equations governing low-frequency acoustic-gravity waves in a stable stratified atmosphere can have localized dipole-vortex solutions (modons). They propagate in the horizontal direction with a speed that is larger than that of all possible linear internal waves.
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Stenflo, L., Stepanyants, Y.A. Acoustic-gravity modons in the atmosphere. Annales Geophysicae 13, 973–975 (1995). https://doi.org/10.1007/s00585-995-0973-3
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DOI: https://doi.org/10.1007/s00585-995-0973-3