Collision Rate of Small Graupel and Water Drops
Authors:
- A. KhainAKA. Khain
- M. PinskyMPM. Pinsky
- M. ShapiroMSM. Shapiro
- A. PokrovskyAPA. Pokrovsky
Open Access
- 1 September 2001
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 58 (17) , 2571-2595
Abstract
An approach permitting one to calculate the collision efficiency and the collision kernel of spherical particles of different densities for Reynolds numbers up to 100 (300-μm-radius drops, or 700-μm-radius graupel) is presented. It is used for the calculation of graupel–drop collision efficiencies and collision kernels in calm air for low-, medium-, and high-density graupel at 750- and 500-mb pressure levels. Low-density graupel interacts with water droplets in a way similar to ice crystals: there exists a cutoff size, below which graupel cannot collect water droplets. The authors have shown that the cutoff size decreases with the growth of graupel density, so that medium- and high-density graupel is able to collect droplets with the radii exceeding a certain minimum size. The graupel–drop collision efficiency increases with the drop size up to a maximum value and then sharply decreases to zero, when the drops' terminal velocity approaches the terminal velocity of graupel. As soon as the terminal... Abstract An approach permitting one to calculate the collision efficiency and the collision kernel of spherical particles of different densities for Reynolds numbers up to 100 (300-μm-radius drops, or 700-μm-radius graupel) is presented. It is used for the calculation of graupel–drop collision efficiencies and collision kernels in calm air for low-, medium-, and high-density graupel at 750- and 500-mb pressure levels. Low-density graupel interacts with water droplets in a way similar to ice crystals: there exists a cutoff size, below which graupel cannot collect water droplets. The authors have shown that the cutoff size decreases with the growth of graupel density, so that medium- and high-density graupel is able to collect droplets with the radii exceeding a certain minimum size. The graupel–drop collision efficiency increases with the drop size up to a maximum value and then sharply decreases to zero, when the drops' terminal velocity approaches the terminal velocity of graupel. As soon as the terminal...Keywords
This publication has 26 references indexed in Scilit:
- Drop Inertia and Its Contribution to Turbulent Coalescence in Convective Clouds. Part I: Drop Fall in the Flow with Random Horizontal VelocityJournal of the Atmospheric Sciences, 1995
- On the Relative Efficiency of Coalescence and RimingJournal of the Atmospheric Sciences, 1987
- The Effect of Vertical Turbulent Fluctuations in the Atmosphere on the Collection of Aerosol Particles by Cloud DropsJournal of the Atmospheric Sciences, 1985
- A Quantitative Assessment of the Accuracy of Techniques for Calculating Graupel GrowthJournal of the Atmospheric Sciences, 1985
- Collection and coalescence efficiencies for accretionJournal of Geophysical Research: Atmospheres, 1984
- The Effects of Altitude and Electrical Force on the Terminal Velocity of HydrometeorsJournal of the Atmospheric Sciences, 1980
- Numerical Simulation of Graupel DevelopmentJournal of the Atmospheric Sciences, 1978
- Terminal Velocity and Shape of Cloud and Precipitation Drops AloftJournal of the Atmospheric Sciences, 1976
- Production of secondary ice particles during the riming processNature, 1974
- Viscous flow around fluid spheres at intermediate reynolds numbersThe Canadian Journal of Chemical Engineering, 1962