Articles | Volume 9, issue 3
https://doi.org/10.5194/tc-9-925-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-925-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
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
CORRESPONDING AUTHOR
Deutscher Wetterdienst (DWD), 63067 Offenbach, Germany
Institute of Meteorology and Geophysics, Centre for Climate and Cryosphere, University of Innsbruck, 6020 Innsbruck, Austria
E. Schlosser
Austrian Polar Research Institute, Vienna, Austria
Institute of Meteorology and Geophysics, Centre for Climate and Cryosphere, University of Innsbruck, 6020 Innsbruck, Austria
E. Isaksson
Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway
D. Divine
Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway
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Latest update: 18 Nov 2024
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.
The first comprehensive study of a set of 76 firn cores in Dronning Maud Land was carried out....
