Accessibility navigation

Stratospheric heating by potential geoengineering aerosols

Ferraro, A.J., Highwood, E.J. and Charlton-Perez, A.J. (2011) Stratospheric heating by potential geoengineering aerosols. Geophysical Research Letters, 34. L24706. ISSN 0094-8276

Full text not archived in this repository.

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

To link to this item DOI: 10.1029/2011GL049761


A fixed dynamical heating model is used to investigate the pattern of zonal-mean stratospheric temperature change resulting from geoengineering with aerosols composed of sulfate, titania, limestone and soot. Aerosol always heats the tropical lower stratosphere, but at the poles the response can be either heating, cooling, or neutral. The sign of the change in stratospheric Pole-Equator temperature difference depends on aerosol type, size and season. This has implications for modelling geoengineering impacts and the response of the stratospheric circulation.

Item Type:Article
Divisions:Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
ID Code:25221
Publisher:American Geophysical Union

University Staff: Request a correction | Centaur Editors: Update this record

Page navigation