Articles | Volume 12, issue 1
https://doi.org/10.5194/cp-12-103-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-103-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
20 Jan 2016
Research article |
| 20 Jan 2016
Variability of sulfate signal in ice core records based on five replicate cores
E. Gautier
CORRESPONDING AUTHOR
Université Grenoble Alpes, LGGE, 38000 Grenoble, France
CNRS, LGGE, 38000 Grenoble, France
J. Savarino
Université Grenoble Alpes, LGGE, 38000 Grenoble, France
CNRS, LGGE, 38000 Grenoble, France
J. Erbland
Université Grenoble Alpes, LGGE, 38000 Grenoble, France
CNRS, LGGE, 38000 Grenoble, France
A. Lanciki
Université Grenoble Alpes, LGGE, 38000 Grenoble, France
CNRS, LGGE, 38000 Grenoble, France
P. Possenti
Université Grenoble Alpes, LGGE, 38000 Grenoble, France
CNRS, LGGE, 38000 Grenoble, France
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Short summary
We evaluate the local-scale variability of a sulfate profile at a low-accumulation site (Dome C, Antarctica) to assess the representativeness of one ice core for volcanic reconstructions. Peak statistical occurrence, depth and flux variability are evaluated from five cores. Due to local-scale variability, 64 volcanic peaks can be identified by a five-cores analysis, while only half of them can be assessed from two cores. Using five cores, the uncertainty of the mean flux is reduced to 29 %.
We evaluate the local-scale variability of a sulfate profile at a low-accumulation site (Dome C,...
