Articles | Volume 9, issue 1
https://doi.org/10.5194/tc-9-269-2015
https://doi.org/10.5194/tc-9-269-2015
Research article
 | 
10 Feb 2015
Research article |  | 10 Feb 2015

Arctic sea ice thickness loss determined using subsurface, aircraft, and satellite observations

R. Lindsay and A. Schweiger

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 Ron Lindsay on behalf of the Authors (01 Dec 2014)  Author's response 
ED: Publish subject to minor revisions (Editor review) (24 Dec 2014) by Christian Haas
AR by Ron Lindsay on behalf of the Authors (30 Dec 2014)  Author's response   Manuscript 
ED: Publish as is (11 Jan 2015) by Christian Haas
AR by Ron Lindsay on behalf of the Authors (13 Jan 2015)
Download
Short summary
The sea ice thickness of the Arctic Basin is estimated from sources that include upward-looking sonars, electromagnetic sensors, and lidar or radar altimeters. Good agreement is found between five of the systems while larger systematic differences are found for others. The trend in annual mean ice thickness, 2000--2013, is –0.58–/+0.07m decade–1; for the central Arctic Basin alone the annual mean ice thickness has decreased from 3.45m in 1975 to 1.11m in 2013, a 68% reduction.