http://onlinelibrary.wiley.com/doi/10.1002/jgrd.50622/abstract

Keywords:

Stratosphere;Geoengineering;Aerosol;Numerical diffusion;Atmospheric
modeling;Sedimentation

Abstract

[1] Gravitational settling has been considered to be one of the limiting
factors to stratospheric aerosol lifetime and therefore to the
practicability and effectiveness of stratospheric solar radiation
management (S-SRM, which is one of the approaches being considered for
planetary scale geoengineering or climate engineering). Given the property
of numerical diffusion that is associated with sedimentation as a transport
process on a discretized global grid, it is important to represent this
process as accurately as possible. In this paper newly developed
sedimentation schemes are presented and validated against an analytical
solution. Sensitivity studies with an Aerosol-Chemistry-GCM are conducted
with monodisperse aerosol particles of fixed size and follow two main aims:
first, to evaluate the relevance of sedimentation for the aerosol lifetime
and distribution in the stratosphere as a function of particle size, and
second, to explore the influence of numerical diffusion on these patterns.
The relevance of sedimentation is explored further with respect to other
relevant particle properties, such as shape and density. It is shown that
the role of sedimentation in determining stratospheric particle lifetime is
a complex function of all particle properties combined. Especially with
respect to sulphate aerosol, the influence of sedimentation is conditioned
by the temporal evolution of particle size. Although large enough particles
for considerable sedimentation mediated removal are observed in the context
of volcanic eruptions, it seems uncertain whether secondary particles of an
equivalent size would be obtained in the context of S-SRM, pointing to the
need for an accurate representation of aerosol growth dynamics.

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