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...

Full description

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
Subjects:
Online Access:https://hal.science/hal-00951148
https://hal.science/hal-00951148/document
https://hal.science/hal-00951148/file/gr2013-pub00040266.pdf
id ftunivsavoie:oai:HAL:hal-00951148v1
record_format openpolar
institution Open Polar
collection Université Savoie Mont Blanc: HAL
op_collection_id ftunivsavoie
language English
topic TRANSPORT DE NEIGE PAR LE VENT
CONGERE
ACCUMULATION EOLIENNE
ANTARCTIQUE
AEOLIAN TRANSPORT
BLOWING SNOW
DRIFTING SNOW
[SDE]Environmental Sciences
spellingShingle TRANSPORT DE NEIGE PAR LE VENT
CONGERE
ACCUMULATION EOLIENNE
ANTARCTIQUE
AEOLIAN TRANSPORT
BLOWING SNOW
DRIFTING SNOW
[SDE]Environmental Sciences
Trouvilliez, A.
Naaim-Bouvet, F.
Genthon, C.
Favier, V.
Piard, L.
Bellot, H.
Agosta, C.
Palerme, C.
Amory, C.
Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land
topic_facet TRANSPORT DE NEIGE PAR LE VENT
CONGERE
ACCUMULATION EOLIENNE
ANTARCTIQUE
AEOLIAN TRANSPORT
BLOWING SNOW
DRIFTING SNOW
[SDE]Environmental Sciences
description [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.
author2 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
author Trouvilliez, A.
Naaim-Bouvet, F.
Genthon, C.
Favier, V.
Piard, L.
Bellot, H.
Agosta, C.
Palerme, C.
Amory, C.
author_facet Trouvilliez, A.
Naaim-Bouvet, F.
Genthon, C.
Favier, V.
Piard, L.
Bellot, H.
Agosta, C.
Palerme, C.
Amory, C.
author_sort Trouvilliez, A.
title Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land
title_short Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land
title_full Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land
title_fullStr Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land
title_full_unstemmed Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land
title_sort blowing snow in antarctica: 3 years of continuous observations in adélie land
publisher HAL CCSD
publishDate 2013
url https://hal.science/hal-00951148
https://hal.science/hal-00951148/document
https://hal.science/hal-00951148/file/gr2013-pub00040266.pdf
op_coverage Grenoble - Chamonix Mont-Blanc, France
genre Antarc*
Antarctic
Antarctica
Antarctique*
East Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Antarctique*
East Antarctica
Ice Sheet
op_source International Snow Science Workshop (ISSW 2013), Grenoble Chamonix-Mont-Blanc, France, October 7-11, 2013 : a merging of theory and practice. Florence Naaim-Bouvet, Yves Durand, Richard Lambert (ed.)
International Snow Science Workshop (ISSW)
https://hal.science/hal-00951148
International Snow Science Workshop (ISSW), Oct 2013, Grenoble - Chamonix Mont-Blanc, France. p. 1327 - p. 1331
op_relation hal-00951148
https://hal.science/hal-00951148
https://hal.science/hal-00951148/document
https://hal.science/hal-00951148/file/gr2013-pub00040266.pdf
IRSTEA: PUB00040266
op_rights info:eu-repo/semantics/OpenAccess
_version_ 1796952803890954240
spelling ftunivsavoie:oai:HAL:hal-00951148v1 2024-04-21T07:49:02+00:00 Blowing snow in Antarctica: 3 years of continuous observations in Adélie Land Trouvilliez, A. Naaim-Bouvet, F. Genthon, C. Favier, V. Piard, L. Bellot, H. Agosta, C. Palerme, C. Amory, C. 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 Grenoble - Chamonix Mont-Blanc, France 2013-10-07 https://hal.science/hal-00951148 https://hal.science/hal-00951148/document https://hal.science/hal-00951148/file/gr2013-pub00040266.pdf en eng HAL CCSD Irstea, ANENA, Meteo France hal-00951148 https://hal.science/hal-00951148 https://hal.science/hal-00951148/document https://hal.science/hal-00951148/file/gr2013-pub00040266.pdf IRSTEA: PUB00040266 info:eu-repo/semantics/OpenAccess International Snow Science Workshop (ISSW 2013), Grenoble Chamonix-Mont-Blanc, France, October 7-11, 2013 : a merging of theory and practice. Florence Naaim-Bouvet, Yves Durand, Richard Lambert (ed.) International Snow Science Workshop (ISSW) https://hal.science/hal-00951148 International Snow Science Workshop (ISSW), Oct 2013, Grenoble - Chamonix Mont-Blanc, France. p. 1327 - p. 1331 TRANSPORT DE NEIGE PAR LE VENT CONGERE ACCUMULATION EOLIENNE ANTARCTIQUE AEOLIAN TRANSPORT BLOWING SNOW DRIFTING SNOW [SDE]Environmental Sciences info:eu-repo/semantics/conferenceObject Conference papers 2013 ftunivsavoie 2024-04-11T00:10:42Z [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. Conference Object Antarc* Antarctic Antarctica Antarctique* East Antarctica Ice Sheet Université Savoie Mont Blanc: HAL