Articles | Volume 20, issue 11
Research article
11 Jun 2020
Research article |  | 11 Jun 2020

Future trends in stratosphere-to-troposphere transport in CCMI models

Marta Abalos, Clara Orbe, Douglas E. Kinnison, David Plummer, Luke D. Oman, Patrick Jöckel, Olaf Morgenstern, Rolando R. Garcia, Guang Zeng, Kane A. Stone, and Martin Dameris


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Marta Abalos on behalf of the Authors (10 Feb 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (24 Feb 2020) by Peter Hess
RR by Anonymous Referee #2 (12 Mar 2020)
RR by Anonymous Referee #1 (23 Mar 2020)
ED: Publish as is (24 Mar 2020) by Peter Hess
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.
Final-revised paper