Articles | Volume 14, issue 1
https://doi.org/10.5194/gmd-14-125-2021
© 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-14-125-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Development and technical paper
| 
11 Jan 2021
Development and technical paper |
| 11 Jan 2021
| 11 Jan 2021
Calibration of temperature-dependent ocean microbial processes in the cGENIE.muffin (v0.9.13) Earth system model
Katherine A. Crichton
CORRESPONDING AUTHOR
School of Earth and Ocean Sciences, Cardiff University, Cardiff, CF10 3AT, UK
now at: School of Geography, University of Exeter, Exeter, EX4 4RJ, UK
Jamie D. Wilson
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, BS8 1QU, UK
Andy Ridgwell
Department of Earth and Planetary Sciences, University of California, Riverside, CA 92521, USA
Paul N. Pearson
School of Earth and Ocean Sciences, Cardiff University, Cardiff, CF10 3AT, UK
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Cited
25 citations as recorded by crossref.
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- Plio‐Pleistocene Ocean Circulation Changes in the Gulf of Alaska and Its Impacts on the Carbon and Nitrogen Cycles and the Cordilleran Ice Sheet Development M. Sánchez Montes et al. 10.1029/2021PA004341
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- A diatom extension to the cGEnIE Earth system model – EcoGEnIE 1.1 A. Naidoo-Bagwell et al. 10.5194/gmd-17-1729-2024
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- Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points R. Wood et al. 10.1007/s10712-024-09859-3
- Data-constrained assessment of ocean circulation changes since the middle Miocene in an Earth system model K. Crichton et al. 10.5194/cp-17-2223-2021
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- Characterizing the marine iodine cycle and its relationship to ocean deoxygenation in an Earth system model K. Cheng et al. 10.5194/bg-21-4927-2024
- 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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- Continental configuration controls ocean oxygenation during the Phanerozoic A. Pohl et al. 10.1038/s41586-022-05018-z
- End-Permian marine extinction due to temperature-driven nutrient recycling and euxinia D. Hülse et al. 10.1038/s41561-021-00829-7
24 citations as recorded by crossref.
- Temperature controls carbon cycling and biological evolution in the ocean twilight zone F. Boscolo-Galazzo et al. 10.1126/science.abb6643
- What the geological past can tell us about the future of the ocean’s twilight zone K. Crichton et al. 10.1038/s41467-023-37781-6
- Depth-resolved photochemical production of hydrogen peroxide in the global ocean using remotely sensed ocean color Y. Zhu et al. 10.3389/frsen.2022.1009398
- The dynamic ocean redox evolution during the late Cambrian SPICE: Evidence from the I/Ca proxy R. He et al. 10.1016/j.gloplacha.2024.104354
- Recurrent marine anoxia in the Paleo-Tethys linked to constriction of seaways during the Early Triassic Y. Wu et al. 10.1016/j.epsl.2024.118882
- Plio‐Pleistocene Ocean Circulation Changes in the Gulf of Alaska and Its Impacts on the Carbon and Nitrogen Cycles and the Cordilleran Ice Sheet Development M. Sánchez Montes et al. 10.1029/2021PA004341
- A seasonal transition in biological carbon pump efficiency in the northern Scotia Sea, Southern Ocean S. Henson et al. 10.1016/j.dsr2.2023.105274
- CANOPS-GRB v1.0: a new Earth system model for simulating the evolution of ocean–atmosphere chemistry over geologic timescales K. Ozaki et al. 10.5194/gmd-15-7593-2022
- The Earth system model CLIMBER-X v1.0 – Part 2: The global carbon cycle M. Willeit et al. 10.5194/gmd-16-3501-2023
- A diatom extension to the cGEnIE Earth system model – EcoGEnIE 1.1 A. Naidoo-Bagwell et al. 10.5194/gmd-17-1729-2024
- Why the Early Paleozoic was intrinsically prone to marine extinction A. Pohl et al. 10.1126/sciadv.adg7679
- Climate pathways behind phytoplankton-induced atmospheric warming R. Asselot et al. 10.5194/bg-19-223-2022
- Late Neogene evolution of modern deep-dwelling plankton F. Boscolo-Galazzo et al. 10.5194/bg-19-743-2022
- Post-extinction recovery of the Phanerozoic oceans and biodiversity hotspots P. Cermeño et al. 10.1038/s41586-022-04932-6
- Diagnosing the causes of AMOC slowdown in a coupled model: a cautionary tale J. Gérard & M. Crucifix 10.5194/esd-15-293-2024
- Assessment of Arctic sea ice simulations in cGENIE model and projections under RCP scenarios D. Chen et al. 10.1038/s41598-024-67391-1
- Partitioning the Apparent Temperature Sensitivity into Within- and Across-Taxa Responses: Revisiting the Difference between Autotrophic and Heterotrophic Protists B. Chen (陈炳章) et al. 10.1086/723243
- Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points R. Wood et al. 10.1007/s10712-024-09859-3
- Data-constrained assessment of ocean circulation changes since the middle Miocene in an Earth system model K. Crichton et al. 10.5194/cp-17-2223-2021
- Vertical decoupling in Late Ordovician anoxia due to reorganization of ocean circulation A. Pohl et al. 10.1038/s41561-021-00843-9
- Characterizing the marine iodine cycle and its relationship to ocean deoxygenation in an Earth system model K. Cheng et al. 10.5194/bg-21-4927-2024
- Resolving ecological feedbacks on the ocean carbon sink in Earth system models D. Armstrong McKay et al. 10.5194/esd-12-797-2021
- Iron and sulfur cycling in the cGENIE.muffin Earth system model (v0.9.21) S. van de Velde et al. 10.5194/gmd-14-2713-2021
- Continental configuration controls ocean oxygenation during the Phanerozoic A. Pohl et al. 10.1038/s41586-022-05018-z
1 citations as recorded by crossref.
Latest update: 20 Nov 2024
Short summary
Temperature is a controller of metabolic processes and therefore also a controller of the ocean's biological carbon pump (BCP). We calibrate a temperature-dependent version of the BCP in the cGENIE Earth system model. Since the pre-industrial period, warming has intensified near-surface nutrient recycling, supporting production and largely offsetting stratification-induced surface nutrient limitation. But at the same time less carbon that sinks out of the surface then reaches the deep ocean.
Temperature is a controller of metabolic processes and therefore also a controller of the...
