Articles | Volume 38, issue 5
https://doi.org/10.5194/angeo-38-1123-2020
https://doi.org/10.5194/angeo-38-1123-2020
Regular paper
 | 
29 Oct 2020
Regular paper |  | 29 Oct 2020

An inter-hemispheric seasonal comparison of polar amplification using radiative forcing of a quadrupling CO2 experiment

Fernanda Casagrande, Ronald Buss de Souza, Paulo Nobre, and Andre Lanfer Marquez

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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
ED: Publish subject to revisions (further review by editor and referees) (18 Feb 2020) by Igo Paulino
AR by Fernanda Casagrande on behalf of the Authors (02 Apr 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (02 Apr 2020) by Igo Paulino
RR by Anonymous Referee #1 (30 Apr 2020)
RR by Anonymous Referee #2 (11 May 2020)
ED: Publish subject to revisions (further review by editor and referees) (11 May 2020) by Igo Paulino
AR by Fernanda Casagrande on behalf of the Authors (08 Jul 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (14 Jul 2020) by Igo Paulino
RR by Anonymous Referee #2 (10 Aug 2020)
ED: Publish subject to technical corrections (10 Aug 2020) by Igo Paulino
AR by Fernanda Casagrande on behalf of the Authors (20 Aug 2020)  Author's response    Manuscript
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Short summary
Polar amplification is possibly one of the most important sensitive indicators of climate change. Our results showed that the polar regions are much more vulnerable to large warming due to an increase in atmospheric CO2 forcing than the rest of the world, particularly during the cold season. Despite the asymmetry in warming between the Arctic and Antarctic, both poles show systematic polar amplification in all climate models.