Saturday, 16 September 2000: 8:00 AM
A study of the sensitivity of modelled cyclic mesocyclogenesis to microphysics parameterizations was made using a three-dimensional cloud model. The control run used a Kessler warm-cloud microphysics parameterization. Additional model runs used a Lin, Farley, and Orville
bulk ice microphysics parameterization with different constants. These constants represented large hail, regular hail, and graupel densities and particle size distributions. We will examine the differences between
modelled storms and discuss strategies and implications for modelling.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner