Brownian drift-diffusion model for evolution of droplet size distributions in turbulent clouds

نویسندگان

  • Robert McGraw
  • Yangang Liu
چکیده

[1] Effects from turbulence-induced fluctuations in water vapor saturation on cloud droplet growth are examined using a Brownian diffusion model. The model predicts diffusive broadening of the droplet size distribution, tempered by enhanced evaporation-induced drift of droplets to smaller size from vapor depletion, and approach to a stationary condition (Weibull distribution) determined by the balance between size-space diffusion and drift. Monte Carlo simulations of the approach to the stationary limit and of the distribution itself are presented and compared favorably with observation. A key turbulence parameter required by the kinetic potential theory of drizzle formation is estimated using the new results. Citation: McGraw, R., and Y. Liu (2006), Brownian drift-diffusion model for evolution of droplet size distributions in turbulent clouds, Geophys. Res. Lett., 33, L03802, doi:10.1029/ 2005GL023545.

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تاریخ انتشار 2006