Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Neige Calonne"'
Autor:
Maurine Montagnat, Henning Löwe, Neige Calonne, Martin Schneebeli, Margret Matzl, Matthias Jaggi
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
The role of near-surface snow processes for the formation of climate signals through densification into deep polar firn is still barely understood. To this end we have analyzed a shallow snow pit (0-3 meters) from EastGRIP (Greenland) and derived hig
Externí odkaz:
https://doaj.org/article/9b885a6ea2054b65b5fa653e217b9c6a
Publikováno v:
The Cryosphere. 16:967-980
Modeling air transport through the entire firn column of polar ice sheets is needed to interpret climate archives. To this end, different regressions have been proposed in the past to estimate the effective coefficient of diffusion and permeability o
Heterogeneous grain growth and vertical mass transfer within a snow layer under temperature gradient
Inside a snow cover, metamorphism plays a key role in snow evolution at different scales. This study focuses on the impact of temperature gradient metamorphism on a snow layer in its vertical extent. To this end, two cold-laboratory experiments were
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f03b38231ce7abfbc7d006e0f236845c
https://doi.org/10.5194/tc-2022-255
https://doi.org/10.5194/tc-2022-255
Autor:
Pascal Hagenmuller, Neige Calonne, Marie Dumont, Julien Brondex, Francois Tuzet, Jacques Roulle
Due to very active metamorphism, snow on the ground exhibits a wide range of microstructural patterns. Indeed, snow is a very porous material and it exists on Earth close to its melting point, which promotes its structural evolution through vapor tra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a5e821a06020b1c209691990fa03129
https://doi.org/10.5194/egusphere-egu22-8516
https://doi.org/10.5194/egusphere-egu22-8516
A new experiment has been conducted to characterize experimentally heat and mass transport as well as metamorphism evolution during temperature gradient conditions. To be able to appreciate fine scale as well as larger scale processes, the experiment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d13677dc5c873ec0033173cd0542fca
https://doi.org/10.5194/egusphere-egu22-4509
https://doi.org/10.5194/egusphere-egu22-4509
Modeling air transport through the entire ice sheet column is needed to interpret climate archives. To this end, different regressions were proposed to estimate the effective coefficient of diffusion and permeability of firn. Such regressions are oft
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c94e4b3b94ed8d6e9b85c5675cd9bd4e
https://doi.org/10.5194/tc-2021-196
https://doi.org/10.5194/tc-2021-196
Representing snow isothermal metamorphism is key to model the evolution and properties of the snow cover. Recently, a new phase-field model allowing to describe 3D microstructure induced by curvature effects has been proposed (Bretin et al, Esiam: M2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbdd934f3ced24ad8ec2fce5fbe661d8
https://doi.org/10.5194/egusphere-egu21-5410
https://doi.org/10.5194/egusphere-egu21-5410
Autor:
Marie Dumont, Frederic Flin, Aleksey Malinka, Olivier Brissaud, Pascal Hagenmuller, Philippe Lapalus, Bernard Lesaffre, Anne Dufour, Neige Calonne, Sabine Rolland du Roscoat, Edward Ando
Snow stands out from materials at the Earth's surface owing to its unique optical properties. Snow optical properties are sensitive to the snow microstructure, triggering potent climate feedbacks. The impacts of snow microstructure on its optical pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f8b79115cf3d7291af823773cfbe9e1
https://doi.org/10.5194/tc-2021-53
https://doi.org/10.5194/tc-2021-53