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Cloud processing, cloud evaporation and Angström exponent
Cloud processing cloud evaporation Angströ m exponent
2009/3/12
With a cloud parcel model we investigate how cloud processing and cloud evaporation modify the size distribution and the Angström exponent of an aerosol population. Our study provides a new expla...
Technical Note: Evaporation of polar stratospheric cloud particles, in situ, in a heated inlet
polar stratospheric cloud particles situ heated inlet
2009/1/23
In December 2001 and 2002 in situ aerosol measurements were made from balloon-borne platforms within polar stratospheric clouds (PSC) which contained particles of supercooled ternary solution (STS), n...
The evaporation rate of D2O has been determined by Raman thermometry of a droplet train (12–15 μm diameter) injected into vacuum (~10-5 torr). The cooling rate measured as a function of time in vacuu...
Aerosols' influence on the interplay between condensation, evaporation and rain in warm cumulus cloud
Aerosols' influence interplay condensation evaporation warm cumulus cloud
2008/10/24
A numerical cloud model is used to study the influence of aerosol on the microphysics and dynamics of moderate-sized, coastal, convective clouds that develop under the same meteorological conditions....