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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 2
The Cryosphere, 10, 743–750, 2016
https://doi.org/10.5194/tc-10-743-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 743–750, 2016
https://doi.org/10.5194/tc-10-743-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Brief communication 01 Apr 2016

Brief communication | 01 Apr 2016

Brief communication: Two well-marked cases of aerodynamic adjustment of sastrugi

C. Amory et al.

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Cited articles

Agosta, C., Favier, V., Genthon, C., Gallée, H., Krinner, G., Lenaerts, J. T. M., and van den Broeke, M. R.: A 40-year accumulation dataset for Adélie Land, Antarctica and its application for model validation, Clim. Dynam., 38, 75–86, 2012.
Amory, C., Trouvilliez, A., Gallée, H., Favier, V., Naaim-Bouvet, F., Genthon, C., Agosta, C., Piard, L., and Bellot, H.: Comparison between observed and simulated aeolian snow mass fluxes in Adélie Land, East Antarctica, The Cryosphere, 9, 1373–1383, https://doi.org/10.5194/tc-9-1373-2015, 2015.
Andreas, E. L.: Air-ice drag coefficients in the western weddell sea. 2. A model based on form drag and drifting snow, J. Geophys. Res., 100, 4833–4843, 1995.
Andreas, E. L. and Claffey, K. J.: Air-ice drag coefficients in the western weddell sea. 1. Values deduced from profile measurements, J. Geophys. Res., 100, 4821–4831, 1995.
Budd, W. F.: The drifting of non-uniform snow particles, in: Studies in Antarctic Meteorology, edited by: Rubin, M. J., Antarctic Research Series, Vol. 9, American Geophysical Union, 59–70, 1966.
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This study presents observational characterization of interactions between wind-induced surface roughness and aeolian erosion over a rough surface in coastal East Antarctica. It is shown that the drag caused by small-scale roughness elements can significantly affects the aeolian snow mass flux during an erosion event, depending on the ability of the surface to adjust according to the main wind. Such measurements are essential to improve parameterization schemes for aeolian snow transport models.
This study presents observational characterization of interactions between wind-induced surface...
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