| |
Author |
Title |
Year |
Publication  |
Programme |
Type |
Volume |
Pages |
Links |
|
|
Picard G, Royer A, Arnaud L, Fily M, |
Influence of meter-scale wind-formed features on the variability of the microwave brightness temperature around Dome C in Antarctica
|
2014 |
The Cryosphere |
1110 |
Journal Article |
8 |
1105-1119 |
|
|
|
|
|
2014 |
The Cryosphere |
1053 |
Journal Article |
8 |
2275-2291 |
|
|
|
Barral H, Genthon C, Trouvilliez A, Brun C, Amory C, |
|
2014 |
The Cryosphere |
1013 |
Journal Article |
8 |
1905-1919 |
|
|
|
Domine F, Barrere M, Sarrazin D, Morin S, Arnaud L, |
Automatic monitoring of the effective thermal conductivity of snow in a low-Arctic shrub tundra
|
2015 |
The Cryosphere |
1042 |
Journal Article |
9 |
1265-1276 |
|
|
|
Libois Q, Picard G, Arnaud L, Dumont M, Lafaysse M, Morin S, Lefebvre E, |
Summertime evolution of snow specific surface area close to the surface on the Antarctic Plateau
|
2015 |
The Cryosphere |
1110 |
Journal Article |
9 |
4499-4538 |
|
|
|
|
|
2015 |
The Cryosphere |
1013 |
Journal Article |
9 |
1373-1383 |
|
|
|
Gorodetskaya I V, Kneifel S, Maahn M, Thiery W, Schween J H, Mangold A, Crewell S, Van Lipzig N P M, |
Cloud and precipitation properties from ground-based remote-sensing instruments in East Antarctica
|
2015 |
The Cryosphere |
411 |
Journal Article |
9 |
285-304 |
|
|
|
|
|
2015 |
The Cryosphere |
411 |
Journal Article |
9 |
1373-1383 |
|
|
|
Champollion N, Picard G, Arnaud L, Lefebvre E, Fily M, |
Hoar crystal development and disappearance at Dome C, Antarctica: observation by near-infrared photography and passive microwave satellite |
2013 |
The Cryosphere |
1110 |
Journal Article |
7 |
1247-1262 |
|
|
|
Amory, C., A. Trouvilliez, H. Gallée, F. Naaim-Bouvet, C. Genthon, V. favier, C. Agosta, L. Piard, and H. bellot |
Comparison of aeolian snow transport events and snow mass fluxes between observations and simulations made by the regional climate model MAR in Adélie Land, East Antarctica |
2015 |
The Cryosphere |
1013 |
Journal Article |
9 |
1373-1383 |
|
