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.
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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- Global Carbon Budget 2018 C. Le Quéré et al. 10.5194/essd-10-2141-2018
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- Improved Quantification of Ocean Carbon Uptake by Using Machine Learning to Merge Global Models and pCO2 Data L. Gloege et al. 10.1029/2021MS002620
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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...