Articles | Volume 13, issue 4
Earth Syst. Dynam., 13, 1417–1435, 2022
https://doi.org/10.5194/esd-13-1417-2022
Earth Syst. Dynam., 13, 1417–1435, 2022
https://doi.org/10.5194/esd-13-1417-2022
Research article
17 Oct 2022
Research article | 17 Oct 2022

Process-based estimate of global-mean sea-level changes in the Common Era

Nidheesh Gangadharan et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on esd-2022-2', Anonymous Referee #1, 18 Mar 2022
    • AC1: 'Reply on RC1', Nidheesh Gangadharan, 21 May 2022
  • RC2: 'Comment on esd-2022-2', Anonymous Referee #2, 12 Apr 2022
    • AC2: 'Reply on RC2', Nidheesh Gangadharan, 21 May 2022
  • RC3: 'Comment on esd-2022-2', Anonymous Referee #3, 15 Apr 2022
    • AC3: 'Reply on RC3', Nidheesh Gangadharan, 21 May 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (06 Jun 2022) by Jadranka Sepic
AR by Nidheesh Gangadharan on behalf of the Authors (22 Jun 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (07 Jul 2022) by Jadranka Sepic
RR by Piecuch Christopher (17 Jul 2022)
RR by Anonymous Referee #1 (20 Jul 2022)
RR by Anonymous Referee #2 (26 Jul 2022)
ED: Publish subject to minor revisions (review by editor) (12 Aug 2022) by Jadranka Sepic
AR by Nidheesh Gangadharan on behalf of the Authors (28 Aug 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (13 Sep 2022) by Jadranka Sepic
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Short summary
We describe the contributions of ocean thermal expansion and land-ice melting (ice sheets and glaciers) to global-mean sea-level (GMSL) changes in the Common Era. The mass contributions are the major sources of GMSL changes in the pre-industrial Common Era and glaciers are the largest contributor. The paper also describes the current state of climate modelling, uncertainties and knowledge gaps along with the potential implications of the past variabilities in the contemporary sea-level rise.
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