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Chemistry–Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes

Butchart, Neal and Cionni, I. and Eyring, V. and Shepherdyring, T.G. and Waugh, D.W. and Akiyoshi, H. and Austin, J. and Brühl, C. and Chipperfield, M. and Cordero, E. and Dameris, M. and Deckert, R. and Dhomse, S. and Frith, S. and Garcia, R.R. and Gettelman, A. and Giorgetta, A. and Kinnison, D. E. and Li, F. and Mancini, E. and McLandress, C. and Pawson, S. and Pitari, G. and Plummer, D.A. and Rozanov, E. and Sassi, F. and Scinocca, J.F. and Shibata, K. and Steil, B. and Tian , W. (2010) Chemistry–Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes. Journal of Climate, 23, pp. 5349-5374. DOI: 10.1175/2010JCLI3404.1 .

Full text not available from this repository.

Official URL: http://journals.ametsoc.org/doi/full/10.1175/2010JCLI3404.1

Abstract

The response of stratospheric climate and circulation to increasing amounts of greenhouse gases (GHGs) and ozone recovery in the twenty-first century is analyzed in simulations of 11 chemistry–climate models using near-identical forcings and experimental setup. In addition to an overall global cooling of the stratosphere in the simulations (0.59 ± 0.07 K decade−1 at 10 hPa), ozone recovery causes a warming of the Southern Hemisphere polar lower stratosphere in summer with enhanced cooling above. The rate of warming correlates with the rate of ozone recovery projected by the models and, on average, changes from 0.8 to 0.48 K decade−1 at 100 hPa as the rate of recovery declines from the first to the second half of the century. In the winter northern polar lower stratosphere the increased radiative cooling from the growing abundance of GHGs is, in most models, balanced by adiabatic warming from stronger polar downwelling. In the Antarctic lower stratosphere the models simulate an increase in low temperature extremes required for polar stratospheric cloud (PSC) formation, but the positive trend is decreasing over the twenty-first century in all models. In the Arctic, none of the models simulates a statistically significant increase in Arctic PSCs throughout the twenty-first century. The subtropical jets accelerate in response to climate change and the ozone recovery produces a westward acceleration of the lower-stratospheric wind over the Antarctic during summer, though this response is sensitive to the rate of recovery projected by the models. There is a strengthening of the Brewer–Dobson circulation throughout the depth of the stratosphere, which reduces the mean age of air nearly everywhere at a rate of about 0.05 yr decade−1 in those models with this diagnostic. On average, the annual mean tropical upwelling in the lower stratosphere (70 hPa) increases by almost 2% decade−1, with 59% of this trend forced by the parameterized orographic gravity wave drag in the models. This is a consequence of the eastward acceleration of the subtropical jets, which increases the upward flux of (parameterized) momentum reaching the lower stratosphere in these latitudes.

Document Type:Article
Title:Chemistry–Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes
Authors:
AuthorsInstitution or Email of Authors
Butchart, Neal Met Office Hadley Centre, Exeter, UK
Cionni, I.DLR-PA
Eyring, V.DLR-PA
Shepherdyring, T.G.Univ. of Toronto, CND
Waugh, D.W.Johns Hopkins Univ., Baltimore, MD, USA
Akiyoshi, H.Univ Toronto, CND
Austin, J.Geophysical Fluid Dynamics Lab., Princeton, NJ, USA
Brühl, C.MPIC, Mainz
Chipperfield, M.Univ. of Leeds, UK
Cordero, E.San Jose State Univ., San Jose, CA, USA
Dameris, M.DLR-PA
Deckert, R.DLR-PA
Dhomse, S.Univ. of Leeds, UK
Frith, S.Science Systems and Applications, Inc., Lanham, MD, USA
Garcia, R.R.NCAR, Boulder, CO, USA
Gettelman, A.NCAR, Boulder, CO, USA
Giorgetta, A.MPIM, Hamburg
Kinnison, D. E. NCAR, Boulder, CO, USA
Li, F. Univ. of Maryland, Baltimore, MD, USA
Mancini, E.Univ. L’Aquila, L’Aquila, I
McLandress, C.Univ. of Toronto, CND
Pawson, S.NASA, Greenbelt, MD, USA
Pitari, G.Univ. L’Aquila, L’Aquila, I
Plummer, D.A.Environment Canada, Toronto, CND
Rozanov, E.Physical–Meteorological Observ., Davos, CH
Sassi, F.Naval Research Laboratory, Washington, D.C, USA
Scinocca, J.F.Univ. of Victoria, Victoria, BC, CND
Shibata, K.Meteorological Research Inst., Tsukuba, J
Steil, B.MPIC, Mainz
Tian , W.Univ. of Leeds, UK
Date:2010
Journal or Publication Title:Journal of Climate
Refereed publication:Yes
In Open Access:No
In SCOPUS:Yes
In ISI Web of Science:Yes
Volume:23
DOI:10.1175/2010JCLI3404.1
Page Range:pp. 5349-5374
Status:Published
Keywords:Chemistry, atmospheric, Climate models, Stratosphere, Greenhouse gases, Ozone
HGF - Research field:Aeronautics, Space and Transport (old)
HGF - Program:Space (old)
HGF - Program Themes:W EO - Erdbeobachtung
DLR - Research area:Space
DLR - Program:W EO - Erdbeobachtung
DLR - Research theme (Project):W - Vorhaben Atmosphären- und Klimaforschung (old)
Location: Oberpfaffenhofen
Institutes and Institutions:Institute of Atmospheric Physics > Atmospheric Dynamics
Deposited By: Jana Freund
Deposited On:05 Jan 2011 14:12
Last Modified:26 Mar 2013 13:25

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