Snow and ice scavenging. [Aerosol scavenging]
Theoretical or semi-empirical relations were evaluated for several microphysical attachment mechanisms as applied to snow and ice scavenging of aerosols. It was found that inertial impaction is usually the dominant mechanism if the aerosol particle Stokes number exceeds a critical value. For smaller aerosol particles, electrostatic deposition is the dominant mechanism if the bodies are oppositely charged of mean thunderstorm charge. The remaining mechanisms investigated yield about three orders of magnitude lower scavenging kernals. A numerical model was developed and utilized to incorporate inertial, hydrodynamic, gravitational and electrostatic (coulombic) forces in order to determine trajectories of aerosol particles about snowflakesmore »