Articles | Volume 20, issue 11
https://doi.org/10.5194/acp-20-6883-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-6883-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Future trends in stratosphere-to-troposphere transport in CCMI models
Department of Earth Physics and Astrophysics, Universidad Complutense de Madrid, Madrid, Spain
Clara Orbe
NASA Goddard Institute for Space Studies, New York, NY, USA
Douglas E. Kinnison
National Center for Atmospheric Research, Boulder, CO, USA
David Plummer
Climate Research Branch, Environment and Climate Change Canada, Montreal, Canada
Luke D. Oman
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Patrick Jöckel
Deutsches Zentrum für Luft- und Raumfahrt (DLR),
Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
Olaf Morgenstern
National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand
Rolando R. Garcia
National Center for Atmospheric Research, Boulder, CO, USA
Guang Zeng
National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand
Kane A. Stone
School of Earth Sciences, University of Melbourne, Melbourne, Victoria 3010, Australia
ARC Center of Excellence for Climate System Science, University of New South Wales, Sydney, New South Wales 2052, Australia
now at: Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA
Martin Dameris
Deutsches Zentrum für Luft- und Raumfahrt (DLR),
Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
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Latest update: 20 Nov 2024
Short summary
A set of state-of-the art chemistry–climate models is used to examine future changes in downward transport from the stratosphere, a key contributor to tropospheric ozone. The acceleration of the stratospheric circulation results in increased stratosphere-to-troposphere transport. In the subtropics, downward advection into the troposphere is enhanced due to climate change. At higher latitudes, the ozone reservoir above the tropopause is enlarged due to the stronger circulation and ozone recovery.
A set of state-of-the art chemistry–climate models is used to examine future changes in downward...
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