elib
DLR-Header
DLR-Logo -> http://www.dlr.de
DLR Portal Home | Impressum | Kontakt | English
Schriftgröße: [-] Text [+]

Influence of ozone recovery and greenhouse gas increases on Southern Hemisphere circulation

Karpechko, A.Y. und Gillett, N.P. und Gray, L.J. und Dall'Amico, M. (2010) Influence of ozone recovery and greenhouse gas increases on Southern Hemisphere circulation. Journal of Geophysical Research, 115 (D22117), Seiten 1-15. DOI: 10.1029/2010JD014423.

[img]
Vorschau
PDF - Requires a PDF viewer such as GSview, Xpdf or Adobe Acrobat Reader
1MB

Offizielle URL: http://www.agu.org/journals/jd/jd1022/2010JD014423/

Kurzfassung

Stratospheric ozone depletion has significantly influenced the tropospheric circulation and climate of the Southern Hemisphere (SH) over recent decades, the largest trends being detected in summer. These circulation changes include acceleration of the extratropical tropospheric westerly jet on its poleward side and lowered Antarctic sea level pressure. It is therefore expected that ozone changes will continue to influence climate during the 21st century when ozone recovery is expected. Here we use two contrasting future ozone projections from two chemistry�climate models (CCMs) to force 21st century simulations of the HadGEM1 coupled atmosphere�ocean model, along with A1B greenhouse gas (GHG) concentrations, and study the simulated response in the SH circulation. According to several studies, HadGEM1 simulates present tropospheric climate better than the majority of other available models. When forced by the larger ozone recovery trends, HadGEM1 simulates significant deceleration of the tropospheric jet on its poleward side in the upper troposphere in summer, but the trends in the lower troposphere are not significant. In the simulations with the smaller ozone recovery trends the zonal mean zonal wind trends are not significant throughout the troposphere. The response of the SH circulation to GHG concentration increases in HadGEM1 includes an increase in poleward eddy heat flux in the stratosphere and positive sea level pressure trends in southeastern Pacific. The HadGEM1�simulated zonal wind trends are considerably smaller than the trends simulated by the CCMs, both in the stratosphere and in the troposphere, despite the fact that the zonal mean ozone trends are the same between these simulations.

Dokumentart:Zeitschriftenbeitrag
Titel:Influence of ozone recovery and greenhouse gas increases on Southern Hemisphere circulation
Autoren:
AutorenInstitution oder E-Mail-Adresse der Autoren
Karpechko, A.Y.Univ. of East Anglia, Norwich, UK
Gillett, N.P.Environment Canada, Victoria, CND
Gray, L.J.Univ. of Reading, Reading, UK
Dall'Amico, M.DLR
Datum:2010
Erschienen in:Journal of Geophysical Research
Referierte Publikation:Ja
In Open Access:Nein
In SCOPUS:Ja
In ISI Web of Science:Ja
Band:115
DOI :10.1029/2010JD014423
Seitenbereich:Seiten 1-15
Status:veröffentlicht
Stichwörter:ozone depletion; greenhouse gases; stratosperic circulation; tropospheric circulation
HGF - Forschungsbereich:Verkehr und Weltraum (alt)
HGF - Programm:Weltraum (alt)
HGF - Programmthema:W EO - Erdbeobachtung
DLR - Schwerpunkt:Weltraum
DLR - Forschungsgebiet:W EO - Erdbeobachtung
DLR - Teilgebiet (Projekt, Vorhaben):W - Vorhaben Atmosphären- und Klimaforschung (alt)
Standort: Oberpfaffenhofen
Institute & Einrichtungen:Institut für Physik der Atmosphäre > Dynamik der Atmosphäre
Hinterlegt von: Dr.rer.nat. Michael Ponater
Hinterlegt am:07 Jan 2011 14:10
Letzte Änderung:23 Jan 2014 11:36

Nur für Mitarbeiter des Archivs: Kontrollseite des Eintrags

Blättern
Suchen
Hilfe & Kontakt
Informationen
electronic library verwendet EPrints 3.3.12
Copyright © 2008-2013 Deutsches Zentrum für Luft- und Raumfahrt (DLR). Alle Rechte vorbehalten.