Excellent post. Sadly, the effect likely has the opposite sign to that
required, as high, cold cirrus clouds tend to cause warming. If the effect
could be made short lived, then activating it during daytime sun only may
be viable, which may give a reverse effect.

I'd be interested to see if the energy input calculations scale to
something sensible.

One potential use of this technology would be to create temporary warming
to counteract excessive cooling from SRM. (Much like an amphetamine addict
taking tranquilisers to sleep.) This could give a degree of spatial and
temporal control not otherwise possible in a stratospheric SRM regime.

Regardless of the science, I love the dystopian Sci-fi aesthetic of laser
induced clouds saving us from an uninhabitably polluted world. :-)

A
On Jun 6, 2013 12:35 AM, "Dr D" <[email protected]> wrote:

> 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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