Articles | Volume 12, issue 10
https://doi.org/10.5194/cp-12-1949-2016
© 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/cp-12-1949-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
12 Oct 2016
Research article |
| 12 Oct 2016
Ocean carbon cycling during the past 130 000 years – a pilot study on inverse palaeoclimate record modelling
Geophysical Institute, University of Bergen, Allégaten 70, 5007 Bergen, Norway
Uni Research Climate, Nygårdsgaten 112, 5008 Bergen, Norway
Bjerknes Centre for Climate Research, Bergen, Norway
Babette A. A. Hoogakker
Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK
Arne Winguth
Department of Earth and Environmental Sciences, University of Texas Arlington, P.O. Box 19049, Arlington, TX 76019, USA
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- What was the source of the atmospheric CO<sub>2</sub> increase during the Holocene? V. Brovkin et al. 10.5194/bg-16-2543-2019
- Calibration of temperature-dependent ocean microbial processes in the cGENIE.muffin (v0.9.13) Earth system model K. Crichton et al. 10.5194/gmd-14-125-2021
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Latest update: 29 Jun 2024
Short summary
Sensitivities of sediment tracers to changes in carbon cycle parameters were determined with a global ocean model. The sensitivities were combined with sediment and ice core data. The results suggest a drawdown of the sea surface temperature by 5 °C, an outgassing of the land biosphere by 430 Pg C, and a strengthening of the vertical carbon transfer by biological processes at the Last Glacial Maximum. A glacial change in marine calcium carbonate production can neither be proven nor rejected.
Sensitivities of sediment tracers to changes in carbon cycle parameters were determined with a...
