The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2

Detailed studies of snow cover processes require models that offer a fine description of the snow cover properties. The detailed snowpack model Crocus is such a scheme, and has been run operationally for avalanche forecasting over the French mountains for 20 yr. It is also used for climate or hydrol...

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Published in:Geoscientific Model Development
Main Authors: Vionnet, V., Brun, E., Morin, S., Boone, A., Faroux, S., Moigne, P., Martin, E., Willemet, J.-M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/gmd-5-773-2012
https://gmd.copernicus.org/articles/5/773/2012/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd12737 2023-05-15T13:36:36+02:00 The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2 Vionnet, V. Brun, E. Morin, S. Boone, A. Faroux, S. Moigne, P. Martin, E. Willemet, J.-M. 2018-09-27 application/pdf https://doi.org/10.5194/gmd-5-773-2012 https://gmd.copernicus.org/articles/5/773/2012/ eng eng doi:10.5194/gmd-5-773-2012 https://gmd.copernicus.org/articles/5/773/2012/ eISSN: 1991-9603 Text 2018 ftcopernicus https://doi.org/10.5194/gmd-5-773-2012 2020-07-20T16:25:49Z Detailed studies of snow cover processes require models that offer a fine description of the snow cover properties. The detailed snowpack model Crocus is such a scheme, and has been run operationally for avalanche forecasting over the French mountains for 20 yr. It is also used for climate or hydrological studies. To extend its potential applications, Crocus has been recently integrated within the framework of the externalized surface module SURFEX. SURFEX computes the exchanges of energy and mass between different types of surface and the atmosphere. It includes in particular the land surface scheme ISBA (Interactions between Soil, Biosphere, and Atmosphere). It allows Crocus to be run either in stand-alone mode, using a time series of forcing meteorological data or in fully coupled mode (explicit or fully implicit numerics) with atmospheric models ranging from meso-scale models to general circulation models. This approach also ensures a full coupling between the snow cover and the soil beneath. Several applications of this new simulation platform are presented. They range from a 1-D stand-alone simulation (Col de Porte, France) to fully-distributed simulations in complex terrain over a whole mountain range (Massif des Grandes Rousses, France), or in coupled mode such as a surface energy balance and boundary layer simulation over the East Antarctic Ice Sheet (Dome C). Text Antarc* Antarctic Ice Sheet Copernicus Publications: E-Journals Antarctic East Antarctic Ice Sheet Geoscientific Model Development 5 3 773 791
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description Detailed studies of snow cover processes require models that offer a fine description of the snow cover properties. The detailed snowpack model Crocus is such a scheme, and has been run operationally for avalanche forecasting over the French mountains for 20 yr. It is also used for climate or hydrological studies. To extend its potential applications, Crocus has been recently integrated within the framework of the externalized surface module SURFEX. SURFEX computes the exchanges of energy and mass between different types of surface and the atmosphere. It includes in particular the land surface scheme ISBA (Interactions between Soil, Biosphere, and Atmosphere). It allows Crocus to be run either in stand-alone mode, using a time series of forcing meteorological data or in fully coupled mode (explicit or fully implicit numerics) with atmospheric models ranging from meso-scale models to general circulation models. This approach also ensures a full coupling between the snow cover and the soil beneath. Several applications of this new simulation platform are presented. They range from a 1-D stand-alone simulation (Col de Porte, France) to fully-distributed simulations in complex terrain over a whole mountain range (Massif des Grandes Rousses, France), or in coupled mode such as a surface energy balance and boundary layer simulation over the East Antarctic Ice Sheet (Dome C).
format Text
author Vionnet, V.
Brun, E.
Morin, S.
Boone, A.
Faroux, S.
Moigne, P.
Martin, E.
Willemet, J.-M.
spellingShingle Vionnet, V.
Brun, E.
Morin, S.
Boone, A.
Faroux, S.
Moigne, P.
Martin, E.
Willemet, J.-M.
The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2
author_facet Vionnet, V.
Brun, E.
Morin, S.
Boone, A.
Faroux, S.
Moigne, P.
Martin, E.
Willemet, J.-M.
author_sort Vionnet, V.
title The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2
title_short The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2
title_full The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2
title_fullStr The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2
title_full_unstemmed The detailed snowpack scheme Crocus and its implementation in SURFEX v7.2
title_sort detailed snowpack scheme crocus and its implementation in surfex v7.2
publishDate 2018
url https://doi.org/10.5194/gmd-5-773-2012
https://gmd.copernicus.org/articles/5/773/2012/
geographic Antarctic
East Antarctic Ice Sheet
geographic_facet Antarctic
East Antarctic Ice Sheet
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-5-773-2012
https://gmd.copernicus.org/articles/5/773/2012/
op_doi https://doi.org/10.5194/gmd-5-773-2012
container_title Geoscientific Model Development
container_volume 5
container_issue 3
container_start_page 773
op_container_end_page 791
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