Zobrazeno 1 - 10
of 167
pro vyhledávání: '"F. Larue"'
Publikováno v:
The Cryosphere, Vol 16, Pp 559-579 (2022)
The surface temperature controls the temporal evolution of the snowpack, playing a key role in metamorphism and snowmelt. It shows large spatial variations in mountainous areas because the surface energy budget is affected by the topography, for inst
Externí odkaz:
https://doaj.org/article/3a9a5176378046c3940199cc8194f671
Autor:
G. Picard, H. Löwe, F. Domine, L. Arnaud, F. Larue, V. Favier, E. Le Meur, E. Lefebvre, J. Savarino, A. Royer
Publikováno v:
AGU Advances, Vol 3, Iss 4, Pp n/a-n/a (2022)
Abstract Satellite observations of snow‐covered regions in the microwave range have the potential to retrieve essential climate variables such as snow height. This requires a precise understanding of how microwave scattering is linked to snow micro
Externí odkaz:
https://doaj.org/article/853d64dd45d9468d8e209c249b475eeb
Autor:
F. Tuzet, M. Dumont, G. Picard, M. Lamare, D. Voisin, P. Nabat, M. Lafaysse, F. Larue, J. Revuelto, L. Arnaud
Publikováno v:
The Cryosphere, Vol 14, Pp 4553-4579 (2020)
The presence of light-absorbing particles (LAPs) in snow leads to a decrease in short-wave albedo affecting the surface energy budget. However, the understanding of the impacts of LAPs is hampered by the lack of dedicated datasets, as well as the sca
Externí odkaz:
https://doaj.org/article/54ab259ae30c4b07a23102191415689c
Publikováno v:
The Cryosphere, Vol 14, Pp 3995-4020 (2020)
The monitoring of snow-covered surfaces on Earth is largely facilitated by the wealth of satellite data available, with increasing spatial resolution and temporal coverage over the last few years. Yet to date, retrievals of snow physical properties s
Externí odkaz:
https://doaj.org/article/a1a4cb1adb08457d95ad99391e843b73
Publikováno v:
The Cryosphere, Vol 14, Pp 1497-1517 (2020)
Surface albedo is an essential variable to determine the Earth's surface energy budget, in particular for snow-covered areas where it is involved in one of the most powerful positive feedback loops of the climate system. In situ measurements of broad
Externí odkaz:
https://doaj.org/article/62df1a334757442aad19e6234fbd4ce5
Autor:
F. Larue, G. Picard, L. Arnaud, I. Ollivier, C. Delcourt, M. Lamare, F. Tuzet, J. Revuelto, M. Dumont
Publikováno v:
The Cryosphere, Vol 14, Pp 1651-1672 (2020)
Most models simulating snow albedo assume a flat and smooth surface, neglecting surface roughness. However, the presence of macroscopic roughness leads to a systematic decrease in albedo due to two effects: (1) photons are trapped in concavities (mul
Externí odkaz:
https://doaj.org/article/e79595d6861f4141a353988378b1ba65
Publikováno v:
The Cryosphere, Vol 13, Pp 2169-2187 (2019)
Light-absorbing particles (LAPs) such as black carbon or mineral dust are some of the main drivers of snow radiative transfer. Small amounts of LAPs significantly increase snowpack absorption in the visible wavelengths where ice absorption is particu
Externí odkaz:
https://doaj.org/article/8a5775a2d1d542b69e73227d93bed56a
Publikováno v:
Hydrology and Earth System Sciences, Vol 22, Pp 5711-5734 (2018)
Over northeastern Canada, the amount of water stored in a snowpack, estimated by its snow water equivalent (SWE) amount, is a key variable for hydrological applications. The limited number of weather stations driving snowpack models over large and
Externí odkaz:
https://doaj.org/article/ff7848b12c78439a81e24fd0a31f3a17
Autor:
Patrick F. Larue, Orlandrew E. Danzell
Publikováno v:
Terrorism and Political Violence. 34:1241-1258
The civil conflict literature often relies on state capacity having significant impacts on the risk of, and duration of, civil war and other civil conflicts. Many characteristics of civil conflict ...
Publikováno v:
The Cryosphere
The Cryosphere, 2022, 16, pp.559-579. ⟨10.5194/tc-16-559-2022⟩
The Cryosphere, Vol 16, Pp 559-579 (2022)
The Cryosphere, 2022, 16, pp.559-579. ⟨10.5194/tc-16-559-2022⟩
The Cryosphere, Vol 16, Pp 559-579 (2022)
The surface temperature controls the temporal evolution of the snowpack, playing a key role in metamorphism and snowmelt. It shows large spatial variations in mountainous areas because the surface energy budget is affected by the topography, for inst
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::96fceb24e3abb56daebeb6b86689d498
https://tc.copernicus.org/preprints/tc-2021-180/
https://tc.copernicus.org/preprints/tc-2021-180/