Articles | Volume 8, issue 5
The Cryosphere, 8, 1825–1838, 2014
The Cryosphere, 8, 1825–1838, 2014
Research article
09 Oct 2014
Research article | 09 Oct 2014

Influence of stress, temperature and crystal morphology on isothermal densification and specific surface area decrease of new snow

S. Schleef et al.

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Cited articles

Arnaud, L., Barnola, J. M., and Duval, P.: Physical modeling of the densification of snow / firn and ice upper part of polar ice sheets, in: Physics of Ice Core Records, edited by Hondoh, T., vol. 159, pp. 285–305, Hokkaido University Press, Sapporo, Japan, 2000.
Arnaud, L., Picard, G., Champollion, N., Domine, F., Gallet, J., Lefebvre, E., Fily, M., and Barnola, J.: Measurement of vertical profiles of snow specific surface area with a 1 cm resolution using infrared reflectance: instrument description and validation, J. Glaciol., 57, 17–29, 2011.
Bader, H.: Theory of densification of dry snow on high polar glaciers, US Army SIPRE Res. Rep., 69, 1960.
Bartelt, P. and Lehning, M.: A physical SNOWPACK model for the Swiss avalanche warning Part I: numerical model, Cold Reg. Sci. Technol., 35, 123–145, 2002.
Cabanes, A., Legagneux, L., and Domine, F.: Evolution of the specific surface area and of crystal morphology of Arctic fresh snow during the ALERT 2000 campaign, Atmos. Environ., 36, 2767–2777, 2002.