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Picard G, Domine F, Krinner G, Arnaud L, Lefebvre E,. (2012). Inhibition of the positive snow-albedo feedback by precipitation in interior Antarctica. Bachelor's thesis, Nature Publishing Group, .
Keywords: limate change Cryospheric science
Programme: 1013
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G. Picard, L. Brucker, N. Champollion, L. Arnaud, E. Lefebvre, and M. Fily. (2010). Microwave spectral signature and snow grain size profile in Antarctica. .
Abstract: MicroRAD, Washington USA, 2010.
Programme: 1013
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Champollion N., Arnaud L., Picard G., Gallet J-C., Domine F. and Fily M. (2010). A new device to acquire high-resolution vertical profiles of snow Specific Surface Area (SSA).
Abstract: , EGU Vienna
Programme: 1013
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M. Fily, L. Arnaud, C. Carmagnola, N. Champollion, P. Cliche, F. Domine, F. Dupont, J.C. Gallet, A. Langlois , B. Montpetit, S. Morin, G. Picard, A. Roy, A. Royer, . (2010). A set of devices to acquire vertical profiles of snow specific surface area.
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G. Picard, L. Arnaud, N. Champollion, F. Domine, and M. Fily . (2010). Deep profiles of snow specific surface area at Dome C, Antarctica, and application to passive microwave remote sensing.
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BellotHerve, TrouvilliezAlexandre, Naaim-BouvetFlorence, GenthonChristophe, GalleeHubert, . (2011). Present weather-sensor tests for measuring drifting snow
. ANNALS OF GLACIOLOGY, 52(58), 176–184.
Abstract: In Antarctica, blowing snow accounts for a major component of the surface mass balance near the coast. Measurements of precipitation and blowing snow are scarce, and therefore collected data would allow testing of numerical models of mass flux over this region. A present weather station (PWS), Biral VPF730, was set up on the coast at Cap Prud'homme station, 5 km from Dumont d'Urville (DDU), principally to quantify precipitation. Since we expected to be able to determine blowing-snow fluxes from the PWS data, we tested this device first on our experimental site, the Lac Blanc pass. An empirical calibration was made with a snow particle counter. Although the physics of the phenomenon was not well captured, the flux outputs were better than those from FlowCapts. The first data from Antarctica were reanalyzed. The new calibration seems to be accurate for estimating the high blowing-snow flux with an interrogation of the precipitation effects.
Programme: 1013
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France J L, King M D, Frey M M, Erbland J, Picard G, MacArthur A, Savarino J, . (2011). Snow optical properties at Dome C, Antarctica implications for snow emissions and snow chemistry of reactive nitrogen
. Atmos. Chem. Phys. Discuss., 11(4), 11959–11993.
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Genthon Christophe, Six Delphine, Favier Vincent, Lazzara Matthew, Keller Linda, . (2011). Atmospheric Temperature Measurement Biases on the Antarctic Plateau
. J. Atmos. Oceanic Technol., 28(12), 1598–1605.
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Cyril Palerme. (2011).
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C. Amory. (2011).
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