Articles | Volume 17, issue 12
https://doi.org/10.5194/bg-17-3057-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-3057-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
One size fits all? Calibrating an ocean biogeochemistry model for different circulations
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel,
Düsternbrooker Weg 20, 24105 Kiel, Germany
Paul Kähler
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel,
Düsternbrooker Weg 20, 24105 Kiel, Germany
Wolfgang Koeve
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel,
Düsternbrooker Weg 20, 24105 Kiel, Germany
Karin Kvale
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel,
Düsternbrooker Weg 20, 24105 Kiel, Germany
Volkmar Sauerland
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel,
Düsternbrooker Weg 20, 24105 Kiel, Germany
Department of Mathematics, Kiel University, Christian-Albrechts-Platz 4, 24118 Kiel, Germany
Andreas Oschlies
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel,
Düsternbrooker Weg 20, 24105 Kiel, Germany
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- Use of genetic algorithms for ocean model parameter optimisation: a case study using PISCES-v2_RC for North Atlantic particulate organic carbon M. Falls et al. 10.5194/gmd-15-5713-2022
- Resolving ecological feedbacks on the ocean carbon sink in Earth system models D. Armstrong McKay et al. 10.5194/esd-12-797-2021
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- A derivative-free optimisation method for global ocean biogeochemical models S. Oliver et al. 10.5194/gmd-15-3537-2022
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- The role of biota in the Southern Ocean carbon cycle P. Boyd et al. 10.1038/s43017-024-00531-3
- When to add a new process to a model – and when not: A marine biogeochemical perspective A. Martin et al. 10.1016/j.ecolmodel.2024.110870
- Sensitivity of 21st-century projected ocean new production changes to idealized biogeochemical model structure G. Brett et al. 10.5194/bg-18-3123-2021
- Bridging the gaps between particulate backscattering measurements and modeled particulate organic carbon in the ocean M. Galí et al. 10.5194/bg-19-1245-2022
- Competing effects of wind and buoyancy forcing on ocean oxygen trends in recent decades H. Hollitzer et al. 10.1038/s41467-024-53557-y
- A structure-preserving model for the dynamics of estuarine ecosystems and its application in western Patagonia fjords P. Mata Almonacid & C. Medel 10.1016/j.ecolmodel.2021.109871
- Influence of GEOTRACES data distribution and misfit function choice on objective parameter retrieval in a marine zinc cycle model C. Eisenring et al. 10.5194/bg-19-5079-2022
- Sensitivity of Steady State, Deep Ocean Dissolved Organic Carbon to Surface Boundary Conditions K. Matsumoto et al. 10.1029/2021GB007102
- FOCI-MOPS v1 – integration of marine biogeochemistry within the Flexible Ocean and Climate Infrastructure version 1 (FOCI 1) Earth system model C. Chien et al. 10.5194/gmd-15-5987-2022
- The biological and preformed carbon pumps in perpetually slower and warmer oceans B. Pasquier et al. 10.5194/bg-21-3373-2024
Latest update: 23 Dec 2024
Short summary
Constants of global biogeochemical ocean models are often tuned
by handto match observations of nutrients or oxygen. We investigate the effect of this tuning by optimising six constants of a global biogeochemical model, simulated in five different offline circulations. Optimal values for three constants adjust to distinct features of the circulation applied and can afterwards be swapped among the circulations, without losing too much of the model's fit to observed quantities.
Constants of global biogeochemical ocean models are often tuned
by handto match observations of...
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