Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-377-2019
https://doi.org/10.5194/cp-15-377-2019
Research article
 | 
26 Feb 2019
Research article |  | 26 Feb 2019

Interhemispheric effect of global geography on Earth's climate response to orbital forcing

Rajarshi Roychowdhury and Robert DeConto

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (24 Nov 2017) by Pascale Braconnot
AR by Rajarshi Roychowdhury on behalf of the Authors (07 Feb 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (12 Mar 2018) by Pascale Braconnot
RR by Anonymous Referee #3 (09 Apr 2018)
RR by Anonymous Referee #2 (09 May 2018)
ED: Reconsider after major revisions (13 May 2018) by Pascale Braconnot
AR by Rajarshi Roychowdhury on behalf of the Authors (26 Oct 2018)  Manuscript 
ED: Referee Nomination & Report Request started (15 Nov 2018) by Pascale Braconnot
RR by Anonymous Referee #3 (27 Nov 2018)
RR by Anonymous Referee #2 (21 Dec 2018)
ED: Publish subject to minor revisions (review by editor) (29 Dec 2018) by Pascale Braconnot
AR by Rajarshi Roychowdhury on behalf of the Authors (09 Jan 2019)  Author's response   Manuscript 
ED: Publish as is (18 Jan 2019) by Pascale Braconnot
AR by Rajarshi Roychowdhury on behalf of the Authors (25 Jan 2019)
Download
Short summary
The climate response of the Earth to orbital forcing shows a distinct hemispheric asymmetry, and one of the reasons can be ascribed to the unequal distribution of land in the Northern Hemisphere and Southern Hemisphere. We show that a land asymmetry effect (LAE) exists, and that it can be quantified. By using a GCM with a unique geographic setup, we illustrate that there are far-field influences of global geography that moderate or accentuate the Earth's response to orbital forcing.