Articles | Volume 9, issue 8
https://doi.org/10.5194/gmd-9-2589-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-9-2589-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Development and technical paper
| 
02 Aug 2016
Development and technical paper |
| 02 Aug 2016
Evaluation of NorESM-OC (versions 1 and 1.2), the ocean carbon-cycle stand-alone configuration of the Norwegian Earth System Model (NorESM1)
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
Nadine Goris
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
Jerry F. Tjiputra
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
Iris Kriest
GEOMAR Helmholtz-Zentrum für Ozeanforschung, Kiel, Germany
Mats Bentsen
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
Ingo Bethke
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
Mehmet Ilicak
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
Karen M. Assmann
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
now at: Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden
Christoph Heinze
Geophysical Institute, University of Bergen, Bjerknes Centre for Climate Research, Bergen, Norway
Uni Research Climate, Bjerknes Centre for Climate Research, Bergen, Norway
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53 citations as recorded by crossref.
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- Description and evaluation of NorESM1-F: a fast version of the Norwegian Earth System Model (NorESM) C. Guo et al. 10.5194/gmd-12-343-2019
- The Variable Southern Ocean Carbon Sink N. Gruber et al. 10.1146/annurev-marine-121916-063407
- Net primary productivity estimates and environmental variables in the Arctic Ocean: An assessment of coupled physical-biogeochemical models Y. Lee et al. 10.1002/2016JC011993
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- Overview of the Norwegian Earth System Model (NorESM2) and key climate response of CMIP6 DECK, historical, and scenario simulations Ø. Seland et al. 10.5194/gmd-13-6165-2020
- Observed Regional Fluxes to Constrain Modeled Estimates of the Ocean Carbon Sink A. Fay & G. McKinley 10.1029/2021GL095325
- Global Carbon Budget 2018 C. Le Quéré et al. 10.5194/essd-10-2141-2018
- The Southern Ocean Carbon Cycle 1985–2018: Mean, Seasonal Cycle, Trends, and Storage J. Hauck et al. 10.1029/2023GB007848
- Key physical processes and their model representation for projecting climate impacts on subarctic Atlantic net primary production: A synthesis M. Myksvoll et al. 10.1016/j.pocean.2023.103084
- Improved Quantification of Ocean Carbon Uptake by Using Machine Learning to Merge Global Models and pCO2 Data L. Gloege et al. 10.1029/2021MS002620
- Ocean biogeochemistry in the coupled ocean–sea ice–biogeochemistry model FESOM2.1–REcoM3 Ö. Gürses et al. 10.5194/gmd-16-4883-2023
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- Consistency and Challenges in the Ocean Carbon Sink Estimate for the Global Carbon Budget J. Hauck et al. 10.3389/fmars.2020.571720
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- Uncertainty in the global oceanic CO<sub>2</sub> uptake induced by wind forcing: quantification and spatial analysis A. Roobaert et al. 10.5194/bg-15-1701-2018
- Global Carbon Budget 2019 P. Friedlingstein et al. 10.5194/essd-11-1783-2019
- Reviews and syntheses: parameter identification in marine planktonic ecosystem modelling M. Schartau et al. 10.5194/bg-14-1647-2017
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- Ocean carbon sequestration: Particle fragmentation by copepods as a significant unrecognised factor? D. Mayor et al. 10.1002/bies.202000149
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Short summary
We present an evaluation of the ocean carbon cycle stand-alone configuration of the Norwegian Earth System Model. A re-tuning of the ecosystem parameterisation improves surface tracer fields between versions 1 and 1.2 of the model. Focus is placed on the evaluation of newly implemented parameterisations of the biological carbon pump (i.e. the sinking of particular organic carbon). We find that the model previously underestimated the carbon transport into the deep ocean below 2000 m depth.
We present an evaluation of the ocean carbon cycle stand-alone configuration of the Norwegian...
