Abstract
The dissipation parameterizations developed for higher-order closure are used to parameterize lateral entrainment and detrainment in a mass-flux model. In addition, a subplume-scale turbulence scheme is included to represent fluxes not captured in the conventional mass-flux framework. These new parameterizations are tested by simulating trade wind cumulus from the Barbados Oceanographic and Meteorological Experiment (BOMEX).
Corresponding author address: Dr. Cara-Lyn Lappen, Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523. Email: lappen@atmos.colostate.edu