Articles | Volume 11, issue 4
https://doi.org/10.5194/tc-11-1685-2017
https://doi.org/10.5194/tc-11-1685-2017
Comment/reply
 | 
21 Jul 2017
Comment/reply |  | 21 Jul 2017

Reply to “Basal buoyancy and fast-moving glaciers: in defense of analytic force balance” by C. J. van der Veen (2016)

Terence J. Hughes

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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 Terence Hughes on behalf of the Authors (31 Mar 2017)  Manuscript 
ED: Referee Nomination & Report Request started (05 Apr 2017) by Frank Pattyn
ED: Reconsider after major revisions (18 May 2017) by Frank Pattyn
AR by Terence Hughes on behalf of the Authors (20 Jun 2017)  Author's response   Manuscript 
ED: Publish subject to technical corrections (27 Jun 2017) by Frank Pattyn
AR by Terence Hughes on behalf of the Authors (29 Jun 2017)  Manuscript 
Short summary
Two approaches to ice-sheet modeling are available. Analytical modeling is the traditional approach. It solves the force (momentum), mass, and energy balances to obtain three-dimensional solutions over time. Geometrical modeling employs simple geometry to solve the force and mass balance in one dimension along ice flow. It is useful primarily to provide the first-order physical basis of ice-sheet modeling for students with little background in mathematics. The two approaches are compared.