Manipulating marine stratocumulus cloud amount and albedo: a process-
modelling study of aerosol-cloud-precipitation interactions in
response to injection of cloud condensation nuclei
For those who are interested.


Phil


H. Wang1, P. J. Rasch1, and G. Feingold2
1Pacific Northwest National Laboratory, Atmospheric Sciences & Global
Change Division, Richland, WA, USA
2NOAA Earth System Research Laboratory, Chemical Sciences Division,
Boulder, CO, USA

Abstract. We use a cloud-system-resolving model to study marine-cloud
brightening. We examine how injected aerosol particles that act as
cloud condensation nuclei (CCN) are transported within the marine
boundary layer and how the additional particles in clouds impact cloud
microphysical processes, and feedback on dynamics. Results show that
the effectiveness of cloud brightening depends strongly on
meteorological and background aerosol conditions. Cloud albedo
enhancement is very effective in a weakly precipitating boundary layer
and in CCN-limited conditions preceded by heavy and/or persistent
precipitation. The additional CCN help sustain cloud water by
weakening the precipitation substantially in the former case and
preventing the boundary layer from collapse in the latter. For a given
amount of injected CCN, the injection method (i.e., number and
distribution of sprayers) is critical to the spatial distribution of
these CCN. Both the areal coverage and the number concentration of
injected particles are key players but neither one always emerges as
more important than the other. The same amount of injected material is
much less effective in either strongly precipitating clouds or
polluted clouds, and it is ineffective in a relatively dry boundary
layer that supports clouds of low liquid water path. In the polluted
case and "dry" case, the CCN injection increases drop number
concentration but lowers supersaturation and liquid water path. As a
result, the cloud experiences very weak albedo enhancement, regardless
of the injection method.

Full paper at

http://www.atmos-chem-phys-discuss.net/11/885/2011/acpd-11-885-2011.html

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