Articles | Volume 12, issue 6
https://doi.org/10.5194/gmd-12-2255-2019
© Author(s) 2019. 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-12-2255-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model experiment description paper
| 
12 Jun 2019
Model experiment description paper |
| 12 Jun 2019
| 12 Jun 2019
Assessment of sub-shelf melting parameterisations using the ocean–ice-sheet coupled model NEMO(v3.6)–Elmer/Ice(v8.3)
Lionel Favier
CORRESPONDING AUTHOR
Univ. Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Nicolas C. Jourdain
Univ. Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Adrian Jenkins
British Antarctic Survey, Cambridge, CB3 0ET, UK
Nacho Merino
Univ. Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Gaël Durand
Univ. Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Olivier Gagliardini
Univ. Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Fabien Gillet-Chaulet
Univ. Grenoble Alpes, CNRS, IRD, IGE, 38000 Grenoble, France
Pierre Mathiot
Met Office, Exeter, UK
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- Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP) S. Sun et al. 10.1017/jog.2020.67
- The Framework For Ice Sheet–Ocean Coupling (FISOC) V1.1 R. Gladstone et al. 10.5194/gmd-14-889-2021
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- Aurora Basin, the Weak Underbelly of East Antarctica T. Pelle et al. 10.1029/2019GL086821
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- 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 C. Pelletier et al. 10.5194/gmd-15-553-2022
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- Evaluation of an emergent feature of sub-shelf melt oscillations from an idealized coupled ice sheet–ocean model using FISOC (v1.1) – ROMSIceShelf (v1.0) – Elmer/Ice (v9.0) C. Zhao et al. 10.5194/gmd-15-5421-2022
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- The tipping points and early warning indicators for Pine Island Glacier, West Antarctica S. Rosier et al. 10.5194/tc-15-1501-2021
- A protocol for calculating basal melt rates in the ISMIP6 Antarctic ice sheet projections N. Jourdain et al. 10.5194/tc-14-3111-2020
- An assessment of basal melt parameterisations for Antarctic ice shelves C. Burgard et al. 10.5194/tc-16-4931-2022
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- Towards a fully unstructured ocean model for ice shelf cavity environments: Model development and verification using the Firedrake finite element framework W. Scott et al. 10.1016/j.ocemod.2023.102178
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- Assessing Uncertainty in the Dynamical Ice Response to Ocean Warming in the Amundsen Sea Embayment, West Antarctica I. Nias et al. 10.1029/2019GL084941
- Quantifying the Impact of Bedrock Topography Uncertainty in Pine Island Glacier Projections for This Century A. Wernecke et al. 10.1029/2021GL096589
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- Ice Shelf Basal Melt Sensitivity to Tide‐Induced Mixing Based on the Theory of Subglacial Plumes J. Anselin et al. 10.1029/2022JC019156
- Antarctic tipping points triggered by the mid-Pliocene warm climate J. Blasco et al. 10.5194/cp-20-1919-2024
- Remote Control of Filchner‐Ronne Ice Shelf Melt Rates by the Antarctic Slope Current C. Bull et al. 10.1029/2020JC016550
- The role of history and strength of the oceanic forcing in sea level projections from Antarctica with the Parallel Ice Sheet Model R. Reese et al. 10.5194/tc-14-3097-2020
- Ice Shelf Basal Melt Rates in the Amundsen Sea at the End of the 21st Century N. Jourdain et al. 10.1029/2022GL100629
- A thicker Antarctic ice stream during the mid-Pliocene warm period M. Mas e Braga et al. 10.1038/s43247-023-00983-3
- AMOC Stabilization Under the Interaction With Tipping Polar Ice Sheets S. Sinet et al. 10.1029/2022GL100305
- Unveiling spatial variability within the Dotson Melt Channel through high-resolution basal melt rates from the Reference Elevation Model of Antarctica A. Zinck et al. 10.5194/tc-17-3785-2023
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- Strong impact of sub-shelf melt parameterisation on ice-sheet retreat in idealised and realistic Antarctic topography C. Berends et al. 10.1017/jog.2023.33
- Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100 A. Alevropoulos-Borrill et al. 10.5194/tc-14-1245-2020
- A framework for estimating the anthropogenic part of Antarctica’s sea level contribution in a synthetic setting A. Bradley et al. 10.1038/s43247-024-01287-w
- The GRISLI-LSCE contribution to the Ice Sheet Model Intercomparison Project for phase 6 of the Coupled Model Intercomparison Project (ISMIP6) – Part 2: Projections of the Antarctic ice sheet evolution by the end of the 21st century A. Quiquet & C. Dumas 10.5194/tc-15-1031-2021
- A Semi-Empirical Framework for ice sheet response analysis under Oceanic forcing in Antarctica and Greenland X. Luo & T. Lin 10.1007/s00382-022-06317-x
- 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
- Responses of the Pine Island and Thwaites glaciers to melt and sliding parameterizations I. Joughin et al. 10.5194/tc-18-2583-2024
- Modelling landfast sea ice and its influence on ocean–ice interactions in the area of the Totten Glacier, East Antarctica G. Van Achter et al. 10.1016/j.ocemod.2021.101920
- The stability of present-day Antarctic grounding lines – Part 2: Onset of irreversible retreat of Amundsen Sea glaciers under current climate on centennial timescales cannot be excluded R. Reese et al. 10.5194/tc-17-3761-2023
- FAMOUS version xotzt (FAMOUS-ice): a general circulation model (GCM) capable of energy- and water-conserving coupling to an ice sheet model R. Smith et al. 10.5194/gmd-14-5769-2021
- Predicting ocean-induced ice-shelf melt rates using deep learning S. Rosier et al. 10.5194/tc-17-499-2023
Latest update: 20 Nov 2024
Short summary
The melting at the base of floating ice shelves is the main driver of the Antarctic ice sheet current retreat. Here, we use an ideal set-up to assess a wide range of melting parameterisations depending on oceanic properties with regard to a new ocean–ice-sheet coupled model, published here for the first time. A parameterisation that depends quadratically on thermal forcing in both a local and a non-local way yields the best results and needs to be further assessed with more realistic set-ups.
The melting at the base of floating ice shelves is the main driver of the Antarctic ice sheet...
