J. Hienola et al., Condensation and evaporation of water vapor in mixed aerosols of liquid droplets and ice: numerical comparison of growth rate expressions, J AEROS SCI, 32(3), 2001, pp. 351-374
We compare four different H2O mass flux descriptions in simulations of the
evolution of mixed water/ice aerosol populations undergoing condensational
growth. It is shown that the Maxwellian description, ignoring condensation
heat release, overestimates the growth rates severely when compared with an
exact numerical description. The well-known Mason equation predicts the gr
owth rates somewhat better, but still in an inadequate manner as far as clo
ud drop formation is considered: after 100 s growth the drop radii are over
estimated by up to a factor of 3 at -30 degreesC, An analytical mass flux f
ormulation by Lehlinen et al. (1998) (J, Aerosol Sci. 29, 1035), on the oth
er hand, compares very well with the exact description while requiring only
one percent of computing time needed for the exact numerical calculations.
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