Simulations of Cloud Condensation Droplet Nucleation and Growth.

摘要

The CAMP (Cloud Atmospheric MicroPhysics code) is used to demonstrate the calculation of condensation growth on both fully soluble and insoluble but wettable distributions of aerosol particles. A ''standard'' atmosphere case is considered as well as cases with aerosol loadings that might be expected over large fires supposedly ignited by nuclear blasts. 16 refs., 13 figs.