Articles | Volume 1, issue 1
Weather Clim. Dynam., 1, 155–174, 2020
Weather Clim. Dynam., 1, 155–174, 2020

Research article 15 Apr 2020

Research article | 15 Apr 2020

Decomposing the response of the stratospheric Brewer–Dobson circulation to an abrupt quadrupling in CO2

Andreas Chrysanthou et al.


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 Andreas Chrysanthou on behalf of the Authors (30 Mar 2020)  Author's response    Manuscript
ED: Publish as is (06 Apr 2020) by Paulo Ceppi
Short summary
We perform 50-year-long time-slice experiments using the Met Office HadGEM3 global climate model in order to decompose the Brewer–Dobson circulation (BDC) response to an abrupt quadrupling of CO2 in three distinct components, (a) the rapid adjustment, associated with CO2 radiative effects; (b) a global uniform sea surface temperature warming; and (c) sea surface temperature patterns. This demonstrates a potential for fast and slow timescales of the response of the BDC to greenhouse gas forcing.