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| Titel |
Comparison between observed and simulated aeolian snow mass fluxes in Adélie Land, East Antarctica |
| VerfasserIn |
C. Amory, A. Trouvilliez, H. Gallée, V. Favier, F. Naaim-Bouvet, C. Genthon, C. Agosta, L. Piard, H. Bellot |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1994-0416
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| Digitales Dokument |
URL |
| Erschienen |
In: The Cryosphere ; 9, no. 4 ; Nr. 9, no. 4 (2015-07-30), S.1373-1383 |
| Datensatznummer |
250116822
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| Publikation (Nr.) |
 copernicus.org/tc-9-1373-2015.pdf |
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| Zusammenfassung |
| Using the original setup described in Gallée et al. (2013), the MAR
regional climate model including a coupled snowpack/aeolian snow transport
parameterization, was run at a fine spatial (5 km horizontal and 2 m
vertical) resolution over 1 summer month in coastal Adélie Land.
Different types of feedback were taken into account in MAR including drag
partitioning caused by surface roughness elements. Model outputs are
compared with observations made at two coastal locations, D17 and D47,
situated respectively 10 and 100 km inland. Wind speed was correctly
simulated with positive values of the Nash test (0.60 for D17 and 0.37 for
D47) but wind velocities above 10 m s−1 were underestimated at both D17
and D47; at D47, the model consistently underestimated wind velocity by
2 m s−1. Aeolian snow transport events were correctly reproduced with the
right timing and a good temporal resolution at both locations except when
the maximum particle height was less than 1 m. The threshold friction
velocity, evaluated only at D17 for a 7-day period without snowfall, was
overestimated. The simulated aeolian snow mass fluxes between 0 and 2 m at
D47 displayed the same variations but were underestimated compared to the
second-generation FlowCaptTM values, as was the simulated relative
humidity at 2 m above the surface. As a result, MAR underestimated the total
aeolian horizontal snow transport for the first 2 m above the ground
by a factor of 10 compared to estimations by the second-generation
FlowCaptTM. The simulation was significantly improved at D47 if a
1-order decrease in the magnitude of z0 was accounted for, but
agreement with observations was reduced at D17. Our results suggest that
z0 may vary regionally depending on snowpack properties, which are
involved in different types of feedback between aeolian transport of snow
and z0. |
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