Articles | Volume 15, issue 2
https://doi.org/10.5194/gmd-15-553-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-15-553-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model description paper
| 
25 Jan 2022
Model description paper |
| 25 Jan 2022
| 25 Jan 2022
PARASO, a circum-Antarctic fully coupled ice-sheet–ocean–sea-ice–atmosphere–land model involving f.ETISh1.7, NEMO3.6, LIM3.6, COSMO5.0 and CLM4.5
Charles Pelletier
CORRESPONDING AUTHOR
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Thierry Fichefet
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Hugues Goosse
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Konstanze Haubner
Laboratoire de Glaciologie, Université Libre de Bruxelles, Brussels, Belgium
Samuel Helsen
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Pierre-Vincent Huot
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Christoph Kittel
Laboratory of Climatology, Department of Geography, SPHERES, University of Liège, Liège, Belgium
François Klein
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Sébastien Le clec'h
Earth System Science and Departement Geografie, Vrije Universiteit Brussel, Brussels, Belgium
Nicole P. M. van Lipzig
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Sylvain Marchi
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
François Massonnet
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Pierre Mathiot
Met Office, Exeter, United Kingdom
Université Grenoble Alpes/CNRS/IRD/G-INP, IGE, Grenoble, France
Ehsan Moravveji
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
ICTS, KU Leuven, Leuven, Belgium
Eduardo Moreno-Chamarro
Barcelona Supercomputing Center (BSC), Barcelona, Spain
Pablo Ortega
Barcelona Supercomputing Center (BSC), Barcelona, Spain
Frank Pattyn
Laboratoire de Glaciologie, Université Libre de Bruxelles, Brussels, Belgium
Niels Souverijns
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Environmental Modelling Unit, Flemish Institute for Technological Research (VITO), Mol, Belgium
Guillian Van Achter
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Sam Vanden Broucke
Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Alexander Vanhulle
Earth System Science and Departement Geografie, Vrije Universiteit Brussel, Brussels, Belgium
Deborah Verfaillie
Earth and Life Institute (ELI), UCLouvain, Louvain-la-Neuve, Belgium
Lars Zipf
Laboratoire de Glaciologie, Université Libre de Bruxelles, Brussels, Belgium
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Cited
15 citations as recorded by crossref.
- Contributions of atmospheric forcing and ocean preconditioning in the 2016 Antarctic sea ice extent drop B. Mezzina et al. 10.1088/2752-5295/ad3a0b
- Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing E. Kazmierczak et al. 10.5194/tc-16-4537-2022
- Simulation of a fully coupled 3D glacial isostatic adjustment – ice sheet model for the Antarctic ice sheet over a glacial cycle C. van Calcar et al. 10.5194/gmd-16-5473-2023
- Future Response of Antarctic Continental Shelf Temperatures to Ice Shelf Basal Melting and Calving M. Thomas et al. 10.1029/2022GL102101
- Ice shelf basal channel shape determines channelized ice-ocean interactions C. Cheng et al. 10.1038/s41467-024-47351-z
- Disentangling the drivers of future Antarctic ice loss with a historically calibrated ice-sheet model V. Coulon et al. 10.5194/tc-18-653-2024
- Conservation of heat and mass in P-SKRIPS version 1: the coupled atmosphere–ice–ocean model of the Ross Sea A. Malyarenko et al. 10.5194/gmd-16-3355-2023
- Southern Ocean warming and Antarctic ice shelf melting in conditions plausible by late 23rd century in a high-end scenario P. Mathiot & N. Jourdain 10.5194/os-19-1595-2023
- Influence of fast ice on future ice shelf melting in the Totten Glacier area, East Antarctica G. Van Achter et al. 10.5194/tc-16-4745-2022
- Modulation of the seasonal cycle of the Antarctic sea ice extent by sea ice processes and feedbacks with the ocean and the atmosphere H. Goosse et al. 10.5194/tc-17-407-2023
- Modelling Antarctic ice shelf basal melt patterns using the one-layer Antarctic model for dynamical downscaling of ice–ocean exchanges (LADDIE v1.0) E. Lambert et al. 10.5194/tc-17-3203-2023
- Is It the Same Every Summer for the Euphausiids of the Ross Sea? A. De Felice et al. 10.3390/d14060433
- The circum-Antarctic ice-shelves respond to a more positive Southern Annular Mode with regionally varied melting D. Verfaillie et al. 10.1038/s43247-022-00458-x
- Data initiatives for ocean-driven melt of Antarctic ice shelves S. Cook et al. 10.1017/aog.2023.6
- Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming G. Van Achter et al. 10.3390/geosciences13040106
15 citations as recorded by crossref.
- Contributions of atmospheric forcing and ocean preconditioning in the 2016 Antarctic sea ice extent drop B. Mezzina et al. 10.1088/2752-5295/ad3a0b
- Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing E. Kazmierczak et al. 10.5194/tc-16-4537-2022
- Simulation of a fully coupled 3D glacial isostatic adjustment – ice sheet model for the Antarctic ice sheet over a glacial cycle C. van Calcar et al. 10.5194/gmd-16-5473-2023
- Future Response of Antarctic Continental Shelf Temperatures to Ice Shelf Basal Melting and Calving M. Thomas et al. 10.1029/2022GL102101
- Ice shelf basal channel shape determines channelized ice-ocean interactions C. Cheng et al. 10.1038/s41467-024-47351-z
- Disentangling the drivers of future Antarctic ice loss with a historically calibrated ice-sheet model V. Coulon et al. 10.5194/tc-18-653-2024
- Conservation of heat and mass in P-SKRIPS version 1: the coupled atmosphere–ice–ocean model of the Ross Sea A. Malyarenko et al. 10.5194/gmd-16-3355-2023
- Southern Ocean warming and Antarctic ice shelf melting in conditions plausible by late 23rd century in a high-end scenario P. Mathiot & N. Jourdain 10.5194/os-19-1595-2023
- Influence of fast ice on future ice shelf melting in the Totten Glacier area, East Antarctica G. Van Achter et al. 10.5194/tc-16-4745-2022
- Modulation of the seasonal cycle of the Antarctic sea ice extent by sea ice processes and feedbacks with the ocean and the atmosphere H. Goosse et al. 10.5194/tc-17-407-2023
- Modelling Antarctic ice shelf basal melt patterns using the one-layer Antarctic model for dynamical downscaling of ice–ocean exchanges (LADDIE v1.0) E. Lambert et al. 10.5194/tc-17-3203-2023
- Is It the Same Every Summer for the Euphausiids of the Ross Sea? A. De Felice et al. 10.3390/d14060433
- The circum-Antarctic ice-shelves respond to a more positive Southern Annular Mode with regionally varied melting D. Verfaillie et al. 10.1038/s43247-022-00458-x
- Data initiatives for ocean-driven melt of Antarctic ice shelves S. Cook et al. 10.1017/aog.2023.6
- Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming G. Van Achter et al. 10.3390/geosciences13040106
Latest update: 24 Apr 2024
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Short summary
We present PARASO, a circumpolar model for simulating the Antarctic climate. PARASO features five distinct models, each covering different Earth system subcomponents (ice sheet, atmosphere, land, sea ice, ocean). In this technical article, we describe how this tool has been developed, with a focus on the
coupling interfacesrepresenting the feedbacks between the distinct models used for contribution. PARASO is stable and ready to use but is still characterized by significant biases.
We present PARASO, a circumpolar model for simulating the Antarctic climate. PARASO features...
