Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land

[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience The Surface Mass Balance (SMB) of the Antarctic ice sheet is probably the only important negative contribution to the sea-level rise. Net erosion of snow by the wind may contribute significantly to the SMB of the Antarctic costal zon...

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Bibliographic Details
Main Authors: Trouvilliez, A., Naaim-Bouvet, F., Genthon, C., Favier, V., Piard, L., Bellot, H., Agosta, C., Palerme, C., Amory, C.
Other Authors: Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Erosion torrentielle neige et avalanches (UR ETGR (ETNA)), Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Université de Liège
Format: Conference Object
Language:English
Published: HAL CCSD 2013
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Online Access:https://hal.science/hal-00951148
https://hal.science/hal-00951148/document
https://hal.science/hal-00951148/file/gr2013-pub00040266.pdf
Description
Summary:[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience The Surface Mass Balance (SMB) of the Antarctic ice sheet is probably the only important negative contribution to the sea-level rise. Net erosion of snow by the wind may contribute significantly to the SMB of the Antarctic costal zone. However, there are very few field observations to confirm this hypothesis and to evaluate numerical models developed for this purpose. Adélie Land, located in East Antarctica, is one of the windiest places in the world in term of mean wind speed at the coast. Furthermore, the frequency of the blowing snow events, determined by visual observations, is very high. That is why a field campaign was launched in January 2009 to acquire new modelevaluation- oriented observations in the framework of the European project ICE2SEA and with the logistical support of the French polar Institute (IPEV). Three automatic weather and snow stations, including acoustic sensors for the aeolian transport of snow named FlowCapt, have been deployed in Adélie Land. The stations locations are distinct ranging from 1 to 100 km inland. One of them is a 7 mmast with 6 levels of anemometers and thermo-hygrometers. Thus, the campaign can assess, inter alias, transport events periods, transport frequencies, snow quantities transported, threshold friction velocities and the ratio between small and large fluxes events. Those results can be use in the evaluations of the regional climate models.