Articles | Volume 9, issue 6
https://doi.org/10.5194/tc-9-2383-2015
© 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-9-2383-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
15 Dec 2015
Research article |
| 15 Dec 2015
Summertime evolution of snow specific surface area close to the surface on the Antarctic Plateau
Univ. Grenoble Alpes, LGGE (UMR5183), 38041 Grenoble, France
CNRS, LGGE (UMR5183), 38041 Grenoble, France
now at: ESCER Centre, Department of Earth and Atmospheric Sciences, Université du Québec à Montréal, 201 Av. du Président-Kennedy, Montréal, H3C3P8, Canada
G. Picard
Univ. Grenoble Alpes, LGGE (UMR5183), 38041 Grenoble, France
CNRS, LGGE (UMR5183), 38041 Grenoble, France
L. Arnaud
Univ. Grenoble Alpes, LGGE (UMR5183), 38041 Grenoble, France
CNRS, LGGE (UMR5183), 38041 Grenoble, France
M. Dumont
Météo-France – CNRS, CNRM – GAME (UMR 3589), Centre d'Études de la Neige, Grenoble, France
M. Lafaysse
Météo-France – CNRS, CNRM – GAME (UMR 3589), Centre d'Études de la Neige, Grenoble, France
Météo-France – CNRS, CNRM – GAME (UMR 3589), Centre d'Études de la Neige, Grenoble, France
E. Lefebvre
Univ. Grenoble Alpes, LGGE (UMR5183), 38041 Grenoble, France
CNRS, LGGE (UMR5183), 38041 Grenoble, France
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- The determination of snow parameters using SGLI/GCOM-C spaceborne top-of-atmosphere spectral reflectance measurements over Antarctica A. Kokhanovsky et al. 10.1016/j.jqsrt.2022.108226
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- Spectral measurements of surface hoar crystals S. HORTON & B. JAMIESON 10.1017/jog.2017.6
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- Spectral albedo measurements over snow-covered slopes: theory and slope effect corrections G. Picard et al. 10.5194/tc-14-1497-2020
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Latest update: 13 Dec 2024
Short summary
The albedo and surface energy budget of the Antarctic Plateau are largely determined by snow specific surface area. The latter experiences substantial daily-to-seasonal variations in response to meteorological conditions. In particular, it decreases by a factor three in summer, causing a drop in albedo. These variations are monitored from in situ and remote sensing observations at Dome C. For the first time, they are also simulated with a snowpack evolution model adapted to Antarctic conditions.
The albedo and surface energy budget of the Antarctic Plateau are largely determined by snow...
