Two soundings of deep convection during GATE and two different magnitudes of large-scale lifting have been used as the initial conditions and as the main forcing on the model. The results demonstrate the increase in convective activity and in amount of precipitation with increased intensity of large-scale lifting. The results also show increased occurrence of cloud merger with increased intensity of large-scale lifting. -from Authors
CITATION STYLE
Tao, W. K., & Simpson, J. (1984). Cloud interactions and merging: numerical simulations. Journal of the Atmospheric Sciences, 41(19), 2901–2917. https://doi.org/10.1175/1520-0469(1984)041<2901:CIAMNS>2.0.CO;2
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