Articles | Volume 14, issue 4
https://doi.org/10.5194/tc-14-1399-2020
https://doi.org/10.5194/tc-14-1399-2020
Research article
 | 
27 Apr 2020
Research article |  | 27 Apr 2020

Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet

Wei Wei, Donald D. Blankenship, Jamin S. Greenbaum, Noel Gourmelen, Christine F. Dow, Thomas G. Richter, Chad A. Greene, Duncan A. Young, SangHoon Lee, Tae-Wan Kim, Won Sang Lee, and Karen M. Assmann

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
ED: Publish subject to revisions (further review by editor and referees) (12 Dec 2019) by Kenichi Matsuoka
ED: Publish subject to revisions (further review by editor and referees) (17 Feb 2020) by Kenichi Matsuoka
AR by Wei Wei on behalf of the Authors (19 Feb 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (21 Feb 2020) by Kenichi Matsuoka
RR by Anonymous Referee #2 (21 Feb 2020)
ED: Publish subject to minor revisions (review by editor) (27 Feb 2020) by Kenichi Matsuoka
AR by Wei Wei on behalf of the Authors (08 Mar 2020)  Author's response   Manuscript 
ED: Publish as is (10 Mar 2020) by Kenichi Matsuoka
AR by Wei Wei on behalf of the Authors (16 Mar 2020)  Manuscript 
Download
Short summary
Getz Ice Shelf is the largest meltwater source from Antarctica of the Southern Ocean. This study compares the relative importance of the meltwater production of Getz from both ocean and subglacial sources. We show that basal melt rates are elevated where bathymetric troughs provide pathways for warm Circumpolar Deep Water to enter the Getz Ice Shelf cavity. In particular, we find that subshelf melting is enhanced where subglacially discharged fresh water flows across the grounding line.