Home News About Us Contact Contributors Disclaimer Privacy Policy Help FAQ

Home
Search
Quick Search
Advanced
Fulltext
Browse
Collections
Persons
My eDoc
Session History
Login
Name:
Password:
Documentation
Help
Support Wiki
Direct access to
document ID:


          Institute: MPI für Meteorologie     Collection: Atmosphere in the Earth System     Display Documents



  history
ID: 534552.0, MPI für Meteorologie / Atmosphere in the Earth System
Chemistry-Climate Model Simulations of Twenty-First Century Stratospheric Climate and Circulation Changes
Authors:Butchart, N.; Cionni, I.; Eyring, V.; Shepherd, T. G.; Waugh, D. W.; Akiyoshi, H.; Austin, J.; Bruehl, C.; Chipperfiled, M. P.; Cordero, E.; Dameris, M.; Deckert, R.; Dhomse, S.; Frith, S. M.; Garcia, R. R.; Gettelmann, A.; Giorgetta, M. A.; Kinnison, D. E.; Li, F.; Mancini, E.; McLandress, C.; Pawson, S.; Pitari, G.; Plummer, D. A.; Rozanov, E.; Sassi, F.; Scinocca, J. F.; Shibata, K.; Steil, B.; Tian, W.
Language:English
Date of Publication (YYYY-MM-DD):2010
Title of Journal:Journal of Climate
Journal Abbrev.:J. Clim.
Volume:23
Start Page:5349
End Page:5374
Review Status:Peer-review
Audience:Not Specified
Abstract / Description: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 ± 6 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 (similar to 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.
External Publication Status:published
Document Type:Article
Communicated by:Carola Kauhs
Affiliations:MPI für Meteorologie/Atmosphere in the Earth System
Identifiers:DOI:10.1175/2010JCLI3404.1
Full Text:
Sorry, no privileges
The scope and number of records on eDoc is subject to the collection policies defined by each institute - see "info" button in the collection browse view.