Is this applicable to marine cloud brightening? 

http://www.pnas.org/content/early/2013/05/30/1222190110

Abstract

Potential impacts of lightning-induced plasma on cloud ice formation and 
precipitation have been a subject of debate for decades. Here, we report on 
the interaction of laser-generated plasma channels with water and ice 
clouds observed in a large cloud simulation chamber. Under the conditions 
of a typical storm cloud, in which ice and supercooled water coexist, no 
direct influence of the plasma channels on ice formation or precipitation 
processes could be detected. Under conditions typical for thin cirrus ice 
clouds, however, the plasma channels induced a surprisingly strong effect 
of ice multiplication. Within a few minutes, the laser action led to a 
strong enhancement of the total ice particle number density in the chamber 
by up to a factor of 100, even though only a 10-9 fraction of the chamber 
volume was exposed to the plasma channels. The newly formed ice particles 
quickly reduced the water vapor pressure to ice saturation, thereby 
increasing the cloud optical thickness by up to three orders of magnitude. 
A model relying on the complete vaporization of ice particles in the laser 
filament and the condensation of the resulting water vapor on plasma ions 
reproduces our experimental findings. This surprising effect might open new 
perspectives for remote sensing of water vapor and ice in the upper 
troposphere.

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