The zonal mean solstice circulation of the global middle atmosphere is simulated using a semi-spectral numerical model. Radiative heating and cooling is computed by the algorithm of Wehrbein and Leovy. Mechanical dissipation is represented by the gravity wave breaking parameterization of Lindzen. -from Author
CITATION STYLE
Holton, J. R. (1983). The influence of gravity wave breaking on the general circulation of the middle atmosphere. Journal of the Atmospheric Sciences, 40(10), 2497–2507. https://doi.org/10.1175/1520-0469(1983)040<2497:TIOGWB>2.0.CO;2
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