Articles | Volume 10, issue 2
https://doi.org/10.5194/gmd-10-1009-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/gmd-10-1009-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Model evaluation paper
| 
03 Mar 2017
Model evaluation paper |
| 03 Mar 2017
Comparing sea ice, hydrography and circulation between NEMO3.6 LIM3 and LIM2
Finnish Meteorological Institute, Helsinki, Finland
Doroteaciro Iovino
Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici (CMCC), Bologna, Italy
Martin Vancoppenolle
Sorbonne Universités (UPMC Paris 6), LOCEAN-IPSL, CNRS/IRD/MNHN, Paris, France
Mikko Lensu
Finnish Meteorological Institute, Helsinki, Finland
Clement Rousset
Sorbonne Universités (UPMC Paris 6), LOCEAN-IPSL, CNRS/IRD/MNHN, Paris, France
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Cited
24 citations as recorded by crossref.
- Optimising assimilation of sea ice concentration in an Earth system model with a multicategory sea ice model M. Kimmritz et al. 10.1080/16000870.2018.1435945
- Challenges and Prospects in Ocean Circulation Models B. Fox-Kemper et al. 10.3389/fmars.2019.00065
- Large-scale Ocean Circulation and Sea Ice Characteristics Derived from Numerical Experiments with the NEMO Model V. Stepanov et al. 10.3103/S1068373919010047
- Simulated Arctic Ocean Response to Doubling of Riverine Carbon and Nutrient Delivery J. Terhaar et al. 10.1029/2019GB006200
- Dependence of Beaufort Sea Low Ice Condition in the Summer of 1998 on Ice Export in the Prior Winter Y. Zhang et al. 10.1175/JCLI-D-19-0943.1
- Presentation and Evaluation of the IPSL‐CM6A‐LR Climate Model O. Boucher et al. 10.1029/2019MS002010
- An evaluation of Antarctic sea-ice thickness from the Global Ice-Ocean Modeling and Assimilation System based on in situ and satellite observations S. Liao et al. 10.5194/tc-16-1807-2022
- Impact of the ice thickness distribution discretization on the sea ice concentration variability in the NEMO3.6–LIM3 global ocean–sea ice model E. Moreno-Chamarro et al. 10.5194/gmd-13-4773-2020
- Evaluation of the CMCC global eddying ocean model for the Ocean Model Intercomparison Project (OMIP2) D. Iovino et al. 10.5194/gmd-16-6127-2023
- Investigation of the Recent Ice Characteristics in the Bohai Sea in the Winters of 2005–2022 Using Multi-Source Data G. Li et al. 10.3390/w16020290
- IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations P. Sepulchre et al. 10.5194/gmd-13-3011-2020
- Mechanisms for the link between onset and duration of open water in the Kara Sea C. Dong et al. 10.1007/s13131-021-1767-5
- Sensitivity of NEMO4.0-SI3 model parameters on sea ice budgets in the Southern Ocean Y. Nie et al. 10.5194/gmd-16-1395-2023
- Limited Lateral Transport Bias During Export of Sea Surface Temperature Proxy Carriers in the Mediterranean Sea A. Rice et al. 10.1029/2021GL096859
- Tuning ice model parameters to improve Arctic sea-ice simulation using the ERA5 atmospheric reanalysis forcing S. MacDermid et al. 10.1080/1755876X.2024.2447155
- The Tuning Strategy of IPSL‐CM6A‐LR J. Mignot et al. 10.1029/2020MS002340
- On the sensitivity of Antarctic sea ice model biases to atmospheric forcing uncertainties A. Barthélemy et al. 10.1007/s00382-017-3972-7
- Effects of Increasing the Category Resolution of the Sea Ice Thickness Distribution in a Coupled Climate Model on Arctic and Antarctic Sea Ice Mean State M. Smith et al. 10.1029/2022JC019044
- Bivariate sea-ice assimilation for global-ocean analysis–reanalysis A. Cipollone et al. 10.5194/os-19-1375-2023
- NEMO-Bohai 1.0: a high-resolution ocean and sea ice modelling system for the Bohai Sea, China Y. Yan et al. 10.5194/gmd-15-1269-2022
- Effect of compressive strength on the performance of the NEMO-LIM model in Arctic Sea ice simulation C. Dong et al. 10.1007/s00343-022-1241-z
- Arctic sea-ice-free season projected to extend into autumn M. Lebrun et al. 10.5194/tc-13-79-2019
- On the discretization of the ice thickness distribution in the NEMO3.6-LIM3 global ocean–sea ice model F. Massonnet et al. 10.5194/gmd-12-3745-2019
- Transport Bias by Ocean Currents in Sedimentary Microplankton Assemblages: Implications for Paleoceanographic Reconstructions P. Nooteboom et al. 10.1029/2019PA003606
24 citations as recorded by crossref.
- Optimising assimilation of sea ice concentration in an Earth system model with a multicategory sea ice model M. Kimmritz et al. 10.1080/16000870.2018.1435945
- Challenges and Prospects in Ocean Circulation Models B. Fox-Kemper et al. 10.3389/fmars.2019.00065
- Large-scale Ocean Circulation and Sea Ice Characteristics Derived from Numerical Experiments with the NEMO Model V. Stepanov et al. 10.3103/S1068373919010047
- Simulated Arctic Ocean Response to Doubling of Riverine Carbon and Nutrient Delivery J. Terhaar et al. 10.1029/2019GB006200
- Dependence of Beaufort Sea Low Ice Condition in the Summer of 1998 on Ice Export in the Prior Winter Y. Zhang et al. 10.1175/JCLI-D-19-0943.1
- Presentation and Evaluation of the IPSL‐CM6A‐LR Climate Model O. Boucher et al. 10.1029/2019MS002010
- An evaluation of Antarctic sea-ice thickness from the Global Ice-Ocean Modeling and Assimilation System based on in situ and satellite observations S. Liao et al. 10.5194/tc-16-1807-2022
- Impact of the ice thickness distribution discretization on the sea ice concentration variability in the NEMO3.6–LIM3 global ocean–sea ice model E. Moreno-Chamarro et al. 10.5194/gmd-13-4773-2020
- Evaluation of the CMCC global eddying ocean model for the Ocean Model Intercomparison Project (OMIP2) D. Iovino et al. 10.5194/gmd-16-6127-2023
- Investigation of the Recent Ice Characteristics in the Bohai Sea in the Winters of 2005–2022 Using Multi-Source Data G. Li et al. 10.3390/w16020290
- IPSL-CM5A2 – an Earth system model designed for multi-millennial climate simulations P. Sepulchre et al. 10.5194/gmd-13-3011-2020
- Mechanisms for the link between onset and duration of open water in the Kara Sea C. Dong et al. 10.1007/s13131-021-1767-5
- Sensitivity of NEMO4.0-SI3 model parameters on sea ice budgets in the Southern Ocean Y. Nie et al. 10.5194/gmd-16-1395-2023
- Limited Lateral Transport Bias During Export of Sea Surface Temperature Proxy Carriers in the Mediterranean Sea A. Rice et al. 10.1029/2021GL096859
- Tuning ice model parameters to improve Arctic sea-ice simulation using the ERA5 atmospheric reanalysis forcing S. MacDermid et al. 10.1080/1755876X.2024.2447155
- The Tuning Strategy of IPSL‐CM6A‐LR J. Mignot et al. 10.1029/2020MS002340
- On the sensitivity of Antarctic sea ice model biases to atmospheric forcing uncertainties A. Barthélemy et al. 10.1007/s00382-017-3972-7
- Effects of Increasing the Category Resolution of the Sea Ice Thickness Distribution in a Coupled Climate Model on Arctic and Antarctic Sea Ice Mean State M. Smith et al. 10.1029/2022JC019044
- Bivariate sea-ice assimilation for global-ocean analysis–reanalysis A. Cipollone et al. 10.5194/os-19-1375-2023
- NEMO-Bohai 1.0: a high-resolution ocean and sea ice modelling system for the Bohai Sea, China Y. Yan et al. 10.5194/gmd-15-1269-2022
- Effect of compressive strength on the performance of the NEMO-LIM model in Arctic Sea ice simulation C. Dong et al. 10.1007/s00343-022-1241-z
- Arctic sea-ice-free season projected to extend into autumn M. Lebrun et al. 10.5194/tc-13-79-2019
- On the discretization of the ice thickness distribution in the NEMO3.6-LIM3 global ocean–sea ice model F. Massonnet et al. 10.5194/gmd-12-3745-2019
- Transport Bias by Ocean Currents in Sedimentary Microplankton Assemblages: Implications for Paleoceanographic Reconstructions P. Nooteboom et al. 10.1029/2019PA003606
Saved (final revised paper)
Latest update: 23 Jun 2025
Short summary
We performed ocean model simulations with new and old sea-ice components. Sea ice improved in the new model compared to the earlier one due to better model physics. In the ocean, the largest differences are confined close to the surface within and near the sea-ice zone. The global ocean circulation slowly deviates between the simulations due to dissimilar sea ice in the deep water formation regions, such as the North Atlantic and Antarctic.
We performed ocean model simulations with new and old sea-ice components. Sea ice improved in...
Special issue