Poster's note : another study showing solar dimming is a risky
approximation to make in SRM models

http://onlinelibrary.wiley.com/doi/10.1002/2014JD022734/abstract

Stratospheric dynamics and midlatitude jets under geoengineering with space
mirrors, and sulfate and titania aerosols

A. J. Ferraro, A. J. Charlton-Perez and E. J. Highwood
DOI: 10.1002/2014JD022734

Journal of Geophysical Research: Atmospheres

Abstract

The impact on the dynamics of the stratosphere of three approaches to
geoengineering by Solar Radiation Management is investigated using
idealized simulations of a global climate model. The approaches are
geoengineering with sulfate aerosols, titania aerosols and reduction in
total solar irradiance (representing mirrors placed in space). If it were
possible to use stratospheric aerosols to counterbalance the surface
warming produced by a quadrupling of atmospheric carbon dioxide
concentrations, tropical lower stratospheric radiative heating would drive
a thermal-wind response which would intensify the stratospheric polar
vortices. In the Northern Hemisphere this intensification results in strong
dynamical cooling of the polar stratosphere. Northern Hemisphere
stratospheric sudden warming events become rare (1 or 2 in 65 years for
sulfate and titania respectively). The intensification of the polar
vortices results in a poleward shift of the tropospheric midlatitude jets
in winter. The aerosol radiative heating enhances the tropical upwelling in
the lower stratosphere, influencing the strength of the Brewer-Dobson
Circulation. In contrast, solar dimming does not produce heating of the
tropical lower stratosphere so there is little intensification of the polar
vortex and no enhanced tropical upwelling. The dynamical response to
titania aerosol is qualitatively similar to the response to sulfate.

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