Articles | Volume 15, issue 2
The Cryosphere, 15, 1005–1014, 2021
The Cryosphere, 15, 1005–1014, 2021

Brief communication 25 Feb 2021

Brief communication | 25 Feb 2021

Brief communication: Glacier run-off estimation using altimetry-derived basin volume change: case study at Humboldt Glacier, northwest Greenland

Laurence Gray


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) (14 Dec 2020) by Kenichi Matsuoka
AR by Laurence Gray on behalf of the Authors (15 Dec 2020)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (21 Dec 2020) by Kenichi Matsuoka
RR by Anonymous Referee #1 (26 Dec 2020)
RR by Anonymous Referee #2 (04 Jan 2021)
ED: Publish subject to technical corrections (14 Jan 2021) by Kenichi Matsuoka
Short summary
A total of 9 years of ice velocity and surface height data obtained from a variety of satellites are used to estimate the water run-off from the northern arm of the Humboldt Glacier in NW Greenland. This represents the first direct measurement of water run-off from a large Greenland glacier, and it complements the iceberg calving flux measurements also based on satellite data. This approach should help improve mass loss estimates for some large Greenland glaciers.