Articles | Volume 15, issue 3
Geosci. Model Dev., 15, 1355–1373, 2022
https://doi.org/10.5194/gmd-15-1355-2022
Geosci. Model Dev., 15, 1355–1373, 2022
https://doi.org/10.5194/gmd-15-1355-2022

Development and technical paper 16 Feb 2022

Development and technical paper | 16 Feb 2022

Capturing the interactions between ice sheets, sea level and the solid Earth on a range of timescales: a new “time window” algorithm

Holly Kyeore Han 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 gmd-2021-126', Wouter van der Wal, 23 Aug 2021
  • RC2: 'Comment on gmd-2021-126', Volker Klemann, 25 Aug 2021
  • EC1: 'Proceed with revisions', Andrew Wickert, 25 Aug 2021
  • AC1: 'Response to Reviewer1's specific comment on gmd-2021-126', Holly Han, 08 Oct 2021
  • AC2: 'Response to Reviewer2's specific comment on gmd-2021-126', Holly Han, 08 Oct 2021
  • AC3: 'Response to Reviewer1&2's general comment on gmd-2021-126',', Holly Han, 08 Oct 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Holly Han on behalf of the Authors (13 Oct 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (19 Nov 2021) by Andrew Wickert
RR by Volker Klemann (25 Nov 2021)
RR by Wouter van der Wal (06 Dec 2021)
ED: Publish subject to technical corrections (08 Dec 2021) by Andrew Wickert
AR by Holly Han on behalf of the Authors (13 Dec 2021)  Author's response    Manuscript
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Short summary
Interactions between ice sheets, sea level and the solid Earth occur over a range of timescales from years to tens of thousands of years. This requires coupled ice-sheet–sea-level models to exchange information frequently, leading to a quadratic increase in computation time with the number of model timesteps. We present a new sea-level model algorithm that allows coupled models to improve the computational feasibility and precisely capture short-term interactions within longer simulations.