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The Cryosphere, 11, 2773-2782, 2017
https://doi.org/10.5194/tc-11-2773-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
05 Dec 2017
Satellite-derived submarine melt rates and mass balance (2011–2015) for Greenland's largest remaining ice tongues
Nat Wilson et al.
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Review of “Submarine melt rates and mass balance for Greenland’s remaining ice tongues” by Wilson et al. 2017', Anonymous Referee #1, 29 Jul 2017 Printer-friendly Version 
 
RC2: 'review 2', Anonymous Referee #2, 30 Jul 2017 Printer-friendly Version 
 
AC1: 'Author's response', Nat Wilson, 20 Sep 2017 Printer-friendly Version Supplement 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Nat Wilson on behalf of the Authors (07 Oct 2017)  Author's response  Manuscript
ED: Publish subject to technical corrections (23 Oct 2017) by Olivier Gagliardini  
CC BY 4.0
Publications Copernicus
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Short summary
We estimate submarine melt rates from ice tongues in northern Greenland using WorldView satellite imagery. At Ryder Glacier, melt is strongly concentrated around regions where subglacier channels likely enter the fjord. At the 79 North Glacier, we find a large volume imbalance in which melting removes a greater quantity of ice than is replaced by inflow over the grounding line. This leads us to suggest that a reduction in the spatial extent of the ice tongue is possible over the coming decade.
We estimate submarine melt rates from ice tongues in northern Greenland using WorldView...
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