Articles | Volume 14, issue 6
https://doi.org/10.5194/gmd-14-3697-2021
© Author(s) 2021. 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-14-3697-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model description paper
| 
22 Jun 2021
Model description paper |
| 22 Jun 2021
| 22 Jun 2021
Coupling framework (1.0) for the PISM (1.1.4) ice sheet model and the MOM5 (5.1.0) ocean model via the PICO ice shelf cavity model in an Antarctic domain
Earth System Analysis, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, 14412 Potsdam, Germany
Institute of Physics and Astronomy, University of Potsdam, 14476 Potsdam, Germany
Ronja Reese
Earth System Analysis, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, 14412 Potsdam, Germany
Willem Nicholas Huiskamp
Earth System Analysis, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, 14412 Potsdam, Germany
Stefan Petri
Earth System Analysis, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, 14412 Potsdam, Germany
Torsten Albrecht
Earth System Analysis, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, 14412 Potsdam, Germany
Georg Feulner
Earth System Analysis, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, 14412 Potsdam, Germany
Ricarda Winkelmann
CORRESPONDING AUTHOR
Earth System Analysis, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, 14412 Potsdam, Germany
Institute of Physics and Astronomy, University of Potsdam, 14476 Potsdam, Germany
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11 citations as recorded by crossref.
- Predicting ocean-induced ice-shelf melt rates using deep learning S. Rosier et al. 10.5194/tc-17-499-2023
- 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
- An assessment of basal melt parameterisations for Antarctic ice shelves C. Burgard et al. 10.5194/tc-16-4931-2022
- What do we mean, ‘tipping cascade’? A. Klose et al. 10.1088/1748-9326/ac3955
- East Antarctic warming forced by ice loss during the Last Interglacial D. Hutchinson et al. 10.1038/s41467-024-45501-x
- Unsupervised Machine Learning for Improved Delaunay Triangulation T. Song et al. 10.3390/jmse9121398
- 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
- 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
- Ice shelf basal channel shape determines channelized ice-ocean interactions C. Cheng et al. 10.1038/s41467-024-47351-z
- Nunataks as barriers to ice flow: implications for palaeo ice sheet reconstructions M. Mas e Braga et al. 10.5194/tc-15-4929-2021
- Climate tipping point interactions and cascades: a review N. Wunderling et al. 10.5194/esd-15-41-2024
1 citations as recorded by crossref.
Latest update: 26 Apr 2024
Short summary
We present the technical implementation of a coarse-resolution coupling between an ice sheet model and an ocean model that allows one to simulate ice–ocean interactions at timescales from centuries to millennia. As ice shelf cavities cannot be resolved in the ocean model at coarse resolution, we bridge the gap using an sub-shelf cavity module. It is shown that the framework is computationally efficient, conserves mass and energy, and can produce a stable coupled state under present-day forcing.
We present the technical implementation of a coarse-resolution coupling between an ice sheet...
