Articles | Volume 8, issue 10
https://doi.org/10.5194/gmd-8-3199-2015
https://doi.org/10.5194/gmd-8-3199-2015
Development and technical paper
 | 
08 Oct 2015
Development and technical paper |  | 08 Oct 2015

A new sub-grid surface mass balance and flux model for continental-scale ice sheet modelling: testing and last glacial cycle

K. Le Morzadec, L. Tarasov, M. Morlighem, and H. Seroussi

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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
AR by Lev Tarasov on behalf of the Authors (28 Jul 2015)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (17 Aug 2015) by Didier Roche
RR by Anonymous Referee #2 (04 Sep 2015)
RR by Fuyuki Saito (09 Sep 2015)
ED: Publish subject to minor revisions (Editor review) (11 Sep 2015) by Didier Roche
AR by Lev Tarasov on behalf of the Authors (16 Sep 2015)  Author's response   Manuscript 
ED: Publish as is (22 Sep 2015) by Didier Roche
AR by Lev Tarasov on behalf of the Authors (24 Sep 2015)
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Short summary
A long-term challenge for any model of complex large-scale processes is accounting for the impact of unresolved sub-grid (SG) processes. We quantify the impact of SG mass-balance and ice fluxes on glacial cycle ensemble results for North America. We find no easy solutions to accurately capture these impacts. We show that SG process representation and associated parametric uncertainties can have significant impact on coarse resolution model results for glacial cycle ice sheet evolution.