Articles | Volume 11, issue 1
https://doi.org/10.5194/tc-11-541-2017
https://doi.org/10.5194/tc-11-541-2017
Research article
 | 
15 Feb 2017
Research article |  | 15 Feb 2017

Models for polythermal ice sheets and glaciers

Ian J. Hewitt and Christian Schoof

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Ian Hewitt on behalf of the Authors (21 Dec 2016)  Author's response   Manuscript 
ED: Publish subject to technical corrections (02 Jan 2017) by Olivier Gagliardini
AR by Ian Hewitt on behalf of the Authors (02 Jan 2017)  Manuscript 
Download
Short summary
Many glaciers contain ice both below and at the melting temperature. Predicting the evolution of temperature and water content in such ice masses is important because they exert a strong control on the flow of the ice. We present two new models to calculate these quantities, demonstrate a number of example numerical calculations, and compare the results with existing methods. The novelty of the new methods is the inclusion of gravity-driven water transport within the ice.