Articles | Volume 13, issue 10
https://doi.org/10.5194/tc-13-2633-2019
https://doi.org/10.5194/tc-13-2633-2019
Research article
 | 
10 Oct 2019
Research article |  | 10 Oct 2019

Ice shelf basal melt rates from a high-resolution digital elevation model (DEM) record for Pine Island Glacier, Antarctica

David E. Shean, Ian R. Joughin, Pierre Dutrieux, Benjamin E. Smith, and Etienne Berthier

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (15 Aug 2019) by Ben Galton-Fenzi
AR by David Shean on behalf of the Authors (20 Aug 2019)  Manuscript 
ED: Publish as is (04 Sep 2019) by Ben Galton-Fenzi
AR by David Shean on behalf of the Authors (04 Sep 2019)
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Short summary
We produced an 8-year, high-resolution DEM record for Pine Island Glacier (PIG), a site of substantial Antarctic mass loss in recent decades. We developed methods to study the spatiotemporal evolution of ice shelf basal melting, which is responsible for ~ 60 % of PIG mass loss. We present shelf-wide basal melt rates and document relative melt rates for kilometer-scale basal channels and keels, offering new indirect observations of ice–ocean interaction beneath a vulnerable ice shelf.