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K. V. Beard, “Ice Initiation in Warm-Base Convective Clouds: An Assessment of Microphysical Mechanisms,” Atmospheric Research, Vol. 28, No. 2, 1992, pp. 125-152. doi:10.1016/0169-8095(92)90024-5

has been cited by the following article:

• TITLE: A Review of Termo- and Diffusio-Phoresis in the Atmospheric Aerosol Scavenging Process. Part 1: Drop Scavenging

  AUTHORS: Gianni Santachiara, Franco Prodi, Franco Belosi

  KEYWORDS: Thermophoresis; Diffusiophoresis; Impaction

  JOURNAL NAME: Atmospheric and Climate Sciences, Vol.2 No.2, April 26, 2012

  ABSTRACT: The role of phoretic forces in providing in-cloud and below-cloud scavenging due to falling drop is reviewed by considering published papers dealing with theoretical models, laboratory and field measurements. Theoretical analyses agree that Brownian diffusion appears to dominate drop scavenging of aerosol with radius less than 0.1 μm, and inertial impaction dominates scavenging of aerosol with radius higher than 1 μm. Thus, there is a minimum collection efficiency for particles in the approximate range 0.1 μm - 1 μm, where phoretic forces are felt. Generally speaking, published papers report not uniform evaluations of the contribution of thermo- and diffusiophoretic forces. This disagreement is partially due to the different laboratory and field conditions, and different theoretical approaches.