Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica
[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience The surface of windy Antarctic snowfields is subject to drifting snow, which leads to the formation of sastrugi. In turn, sastrugi contribute to...
Published in: | Boundary-Layer Meteorology |
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Online Access: | https://hal.inrae.fr/hal-02607299 https://doi.org/10.1007/s10546-017-0242-5 |
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ftinsu:oai:HAL:hal-02607299v1 2024-04-21T07:43:42+00:00 Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica Amory, C. Gallee, H. Naaim-Bouvet, F. Favier, V. Vignon, E. Picard, G. Trouvilliez, A. Piard, L. Genthon, C. Bellot, H. Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) 2017 https://hal.inrae.fr/hal-02607299 https://doi.org/10.1007/s10546-017-0242-5 en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s10546-017-0242-5 hal-02607299 https://hal.inrae.fr/hal-02607299 doi:10.1007/s10546-017-0242-5 IRSTEA: PUB00057155 ISSN: 0006-8314 EISSN: 1573-1472 Boundary-Layer Meteorology https://hal.inrae.fr/hal-02607299 Boundary-Layer Meteorology, 2017, 164 (1), pp.107-133. ⟨10.1007/s10546-017-0242-5⟩ ANTARCTIQUE [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2017 ftinsu https://doi.org/10.1007/s10546-017-0242-5 2024-04-05T00:42:49Z [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience The surface of windy Antarctic snowfields is subject to drifting snow, which leads to the formation of sastrugi. In turn, sastrugi contribute to the drag exerted by the snowsurface on the atmosphere and hence influence drifting snow. Although the surface drag over rough sastrugi fields has been estimated for individual locations in Antarctica, its variation over time and with respect to drifting snow has received little attention. Using year-round data from a meteorological mast, seasonal variations in the neutral drag coefficient at a height of 10m (C-DN10) in coastal Adelie Land are presented and discussed in light of the formation and behaviour of sastrugi based on observed aeolian erosion patterns. The measurements revealed high C-DN10 values (>= 2 x 10(-3)) and limited drifting snow (35% of the time) in summer (December-February) versus lower C-DN10 values (approximate to 1.5 x 10(-3)) associated with more frequent drifting snow (70% of the time) in winter (March-November). Without the seasonal distinction, there was no clear dependence of C-DN10 on friction velocity or wind direction, but observations revealed a general increase in C-DN10 with rising air temperature. Themain hypothesis defended here is that higher temperatures increase snowcohesion and the development of sastrugi just after snow deposition while inhibiting the sastrugi streamlining process by raising the erosion threshold. This increases the contribution of the sastrugi form drag to the total surface drag in summer when winds are lighter and more variable. The analysis also showed that, in the absence of erosion, single snowfall events can reduce C-DN10 to 1 x 10(-3) due to the burying of pre-existing microrelief under newly deposited snow. The results suggest that polar atmospheric models should account for spatial and temporal variations in snow surface roughness through a ... Article in Journal/Newspaper Adelie Land Antarc* Antarctic Antarctica Antarctique* East Antarctica Institut national des sciences de l'Univers: HAL-INSU Boundary-Layer Meteorology 164 1 107 133 |
institution |
Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
ANTARCTIQUE [SDE]Environmental Sciences |
spellingShingle |
ANTARCTIQUE [SDE]Environmental Sciences Amory, C. Gallee, H. Naaim-Bouvet, F. Favier, V. Vignon, E. Picard, G. Trouvilliez, A. Piard, L. Genthon, C. Bellot, H. Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica |
topic_facet |
ANTARCTIQUE [SDE]Environmental Sciences |
description |
[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE International audience The surface of windy Antarctic snowfields is subject to drifting snow, which leads to the formation of sastrugi. In turn, sastrugi contribute to the drag exerted by the snowsurface on the atmosphere and hence influence drifting snow. Although the surface drag over rough sastrugi fields has been estimated for individual locations in Antarctica, its variation over time and with respect to drifting snow has received little attention. Using year-round data from a meteorological mast, seasonal variations in the neutral drag coefficient at a height of 10m (C-DN10) in coastal Adelie Land are presented and discussed in light of the formation and behaviour of sastrugi based on observed aeolian erosion patterns. The measurements revealed high C-DN10 values (>= 2 x 10(-3)) and limited drifting snow (35% of the time) in summer (December-February) versus lower C-DN10 values (approximate to 1.5 x 10(-3)) associated with more frequent drifting snow (70% of the time) in winter (March-November). Without the seasonal distinction, there was no clear dependence of C-DN10 on friction velocity or wind direction, but observations revealed a general increase in C-DN10 with rising air temperature. Themain hypothesis defended here is that higher temperatures increase snowcohesion and the development of sastrugi just after snow deposition while inhibiting the sastrugi streamlining process by raising the erosion threshold. This increases the contribution of the sastrugi form drag to the total surface drag in summer when winds are lighter and more variable. The analysis also showed that, in the absence of erosion, single snowfall events can reduce C-DN10 to 1 x 10(-3) due to the burying of pre-existing microrelief under newly deposited snow. The results suggest that polar atmospheric models should account for spatial and temporal variations in snow surface roughness through a ... |
author2 |
Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Erosion torrentielle neige et avalanches (UR ETGR (ETNA)) Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) |
format |
Article in Journal/Newspaper |
author |
Amory, C. Gallee, H. Naaim-Bouvet, F. Favier, V. Vignon, E. Picard, G. Trouvilliez, A. Piard, L. Genthon, C. Bellot, H. |
author_facet |
Amory, C. Gallee, H. Naaim-Bouvet, F. Favier, V. Vignon, E. Picard, G. Trouvilliez, A. Piard, L. Genthon, C. Bellot, H. |
author_sort |
Amory, C. |
title |
Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica |
title_short |
Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica |
title_full |
Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica |
title_fullStr |
Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica |
title_full_unstemmed |
Seasonal variations in drag coefficient over a Sastrugi-covered snowfield in coastal East Antarctica |
title_sort |
seasonal variations in drag coefficient over a sastrugi-covered snowfield in coastal east antarctica |
publisher |
HAL CCSD |
publishDate |
2017 |
url |
https://hal.inrae.fr/hal-02607299 https://doi.org/10.1007/s10546-017-0242-5 |
genre |
Adelie Land Antarc* Antarctic Antarctica Antarctique* East Antarctica |
genre_facet |
Adelie Land Antarc* Antarctic Antarctica Antarctique* East Antarctica |
op_source |
ISSN: 0006-8314 EISSN: 1573-1472 Boundary-Layer Meteorology https://hal.inrae.fr/hal-02607299 Boundary-Layer Meteorology, 2017, 164 (1), pp.107-133. ⟨10.1007/s10546-017-0242-5⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s10546-017-0242-5 hal-02607299 https://hal.inrae.fr/hal-02607299 doi:10.1007/s10546-017-0242-5 IRSTEA: PUB00057155 |
op_doi |
https://doi.org/10.1007/s10546-017-0242-5 |
container_title |
Boundary-Layer Meteorology |
container_volume |
164 |
container_issue |
1 |
container_start_page |
107 |
op_container_end_page |
133 |
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1796952023997874176 |