Articles | Volume 16, issue 3
https://doi.org/10.5194/tc-16-941-2022
https://doi.org/10.5194/tc-16-941-2022
Research article
 | 
14 Mar 2022
Research article |  | 14 Mar 2022

PISM-LakeCC: Implementing an adaptive proglacial lake boundary in an ice sheet model

Sebastian Hinck, Evan J. Gowan, Xu Zhang, and Gerrit Lohmann

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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 (further review by editor and referees) (31 May 2021) by Kerim Nisancioglu
AR by Sebastian Hinck on behalf of the Authors (19 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (20 Aug 2021) by Kerim Nisancioglu
RR by Anonymous Referee #3 (31 Aug 2021)
RR by Tijn Berends (05 Sep 2021)
ED: Reconsider after major revisions (further review by editor and referees) (05 Oct 2021) by Kerim Nisancioglu
AR by Sebastian Hinck on behalf of the Authors (15 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (09 Jan 2022) by Kerim Nisancioglu
AR by Sebastian Hinck on behalf of the Authors (19 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (04 Feb 2022) by Kerim Nisancioglu
AR by Sebastian Hinck on behalf of the Authors (04 Feb 2022)  Author's response    Manuscript
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Short summary
Proglacial lakes were pervasive along the retreating continental ice margins after the Last Glacial Maximum. Similarly to the marine ice boundary, interactions at the ice-lake interface impact ice sheet dynamics and mass balance. Previous numerical ice sheet modeling studies did not include a dynamical lake boundary. We describe the implementation of an adaptive lake boundary condition in PISM and apply the model to the glacial retreat of the Laurentide Ice Sheet.