Abstract
It is designed to estimate convective properties using a cloud model that interacts with the mesoscale model in a physically consistent manner. The cloud model is initiated by and interacts with the grid-scale circulation without being constrained in instantaneous equilibrium with the grid-scale flow. The parameterization is designed for use in conjunction with explicit moist processes. -from Authors
Cite
CITATION STYLE
Frank, W. M., & Cohen, C. (1987). Simulation of tropical convective systems. Part I: a cumulus parameterization. Journal of the Atmospheric Sciences, 44(24), 3787–3799. https://doi.org/10.1175/1520-0469(1987)044<3787:SOTCSP>2.0.CO;2
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