Behavior of a moist Kelvin wave packet with nonlinear heating

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Abstract

The unstable perturbation subject to nonlinear heating emerges as a wave packet. A typical amplifying, eastward-moving wave packet is characterized by an asymmetric structure: 1) the ascending branch (wet region) is much narrower than the two descending ones (dry regions); and 2) the circulation cell to the east of the wet region center is smaller and stronger than its counterpart to the west of the center. The wet-dry asymmetry is primarily caused by the nonlinear heating effect, while the east-west asymmetry is a result of the movement of the wave packet relative to mean flow. The existence of Newtonian cooling and Rayleigh friction enhances the structural asymmetries. -from Authors

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Bin Wang, & Yan Xue. (1992). Behavior of a moist Kelvin wave packet with nonlinear heating. Journal of the Atmospheric Sciences, 49(7), 549–559. https://doi.org/10.1175/1520-0469(1992)049<0549:boamkw>2.0.co;2

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