Poster's note : This technique could be useful for tweaking the side
effects of SRM. It's useful it works both ways.

http://onlinelibrary.wiley.com/doi/10.1002/2013JD020707/abstract

Keywords:

stratospheric water vapor;overshooting deep convection;vertical
transport;cloud seeding;geoengineering

Abstract

Stratospheric water vapor has an important effect on Earth's climate.
Considering the significance of overshooting deep convection in modulating
the water vapor content (WVC) of the lower stratosphere (LS), we use a
three-dimensional convective cloud model to simulate the effects of various
silver iodide (AgI) seeding scenarios on tropical overshooting deep
convection that occurred on 30 November 2005 in Darwin, Australia. The
primary motivation for this study is to investigate whether the WVC in the
LS can be artificially modified by deliberate cloud seeding. It is found
that AgI seeding done at the early stages of clouds produces significant
effects on cloud microphysical and dynamical properties, and that further
affects the WVC in the LS, while seeding at the mature stages of clouds has
only a slight impact. The response of stratospheric water vapor to changes
in the amount of seeding agent is nonlinear. The seeding with a small
(large) amount of AgI increases (decreases) the WVC in the LS, due to
enhanced (reduced) production and vertical transport of cloud ice from the
troposphere and subsequent sublimation in the stratosphere. The results
show that stratospheric water vapor can be artificially altered by
deliberate cloud seeding with proper amount of seeding agent. This study
also shows an important role of graupel in regulating cloud microphysics
and dynamics and in modifying the WVC in the LS.

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