Articles | Volume 12, issue 3
Earth Syst. Dynam., 12, 783–795, 2021
https://doi.org/10.5194/esd-12-783-2021
Earth Syst. Dynam., 12, 783–795, 2021
https://doi.org/10.5194/esd-12-783-2021

Research article 12 Jul 2021

Research article | 12 Jul 2021

Modelling sea-level fingerprints of glaciated regions with low mantle viscosity

Alan Bartholet et al.

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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: Reconsider after major revisions (08 Feb 2021) by Gerrit Lohmann
AR by Glenn Milne on behalf of the Authors (07 Apr 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (01 Jun 2021) by Gerrit Lohmann
AR by Glenn Milne on behalf of the Authors (04 Jun 2021)  Author's response    Manuscript

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Glenn Milne on behalf of the Authors (09 Jul 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (10 Jul 2021) by Gerrit Lohmann
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Short summary
Improving the accuracy of regional sea-level projections is an important aim that will impact estimates of sea-level hazard around the globe. The computation of sea-level fingerprints is a key component of any such projection, and to date these computations have been based on the assumption that elastic deformation accurately describes the solid Earth response on century timescales. We show here that this assumption is inaccurate in some glaciated regions characterized by low mantle viscosity.
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