Articles | Volume 9, issue 3
The Cryosphere, 9, 925–944, 2015
https://doi.org/10.5194/tc-9-925-2015
The Cryosphere, 9, 925–944, 2015
https://doi.org/10.5194/tc-9-925-2015

Research article 07 May 2015

Research article | 07 May 2015

Climatic signals from 76 shallow firn cores in Dronning Maud Land, East Antarctica

S. Altnau et al.

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 Sebastian Altnau on behalf of the Authors (11 Mar 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (01 Apr 2015) by Martin Schneebeli
RR by Anonymous Referee #2 (10 Apr 2015)
ED: Publish subject to technical corrections (15 Apr 2015) by Martin Schneebeli
Download
Short summary
The first comprehensive study of a set of 76 firn cores in Dronning Maud Land was carried out. The δ18O of both the plateau and the ice shelf cores exhibit a slight positive trend over the second half of the 20th century. The SMB has a negative trend in the ice shelf cores, but increases on the plateau. Comparison with meteorological data revealed that for the ice shelf regions, atmospheric dynamic effects are more important, while on the plateau, thermodynamic effects predominate.