Articles | Volume 10, issue 5
https://doi.org/10.5194/tc-10-2465-2016
https://doi.org/10.5194/tc-10-2465-2016
Research article
 | 
24 Oct 2016
Research article |  | 24 Oct 2016

Reconstructing the mass balance of Brewster Glacier, New Zealand, using MODIS-derived glacier-wide albedo

Pascal Sirguey, Holly Still, Nicolas J. Cullen, Marie Dumont, Yves Arnaud, and Jonathan P. Conway

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 P. Sirguey on behalf of the Authors (14 Sep 2016)
ED: Publish as is (16 Sep 2016) by Chris R. Stokes
AR by P. Sirguey on behalf of the Authors (23 Sep 2016)  Manuscript 
Download
Short summary
Fourteen years of satellite observations are used to monitor the albedo of Brewster Glacier, New Zealand and estimate annual and seasonal balances. This confirms the governing role of the summer balance in the annual balance and allows the reconstruction of the annual balance to 1977 using a photographic record of the snowline. The longest mass balance record for a New Zealand glacier shows negative balances after 2008, yielding a loss of 35 % of the gain accumulated over the previous 30 years.