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GMD | Articles | Volume 13, issue 8
Geosci. Model Dev., 13, 3529–3552, 2020
https://doi.org/10.5194/gmd-13-3529-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: The FAMOUS climate model

Geosci. Model Dev., 13, 3529–3552, 2020
https://doi.org/10.5194/gmd-13-3529-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Development and technical paper 07 Aug 2020

Development and technical paper | 07 Aug 2020

Simulating stable carbon isotopes in the ocean component of the FAMOUS general circulation model with MOSES1 (XOAVI)

Jennifer E. Dentith et al.

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Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-365,https://doi.org/10.5194/bg-2019-365, 2019
Revised manuscript has not been submitted
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Cited articles

Andres, R., Boden, T., and Marland, G.: Annual Fossil-Fuel CO2 Emissions: Global Stable Carbon Isotopic Signature, CDIAC, https://doi.org/10.3334/CDIAC/FFE.DB1013.2017, 1996. 
Andres, R. J., Marland, G., Boden, T., and Bischof, S.: Carbon dioxide emissions from fossil fuel consumption and cement manufacture, 1751–1991; and an estimate of their isotopic composition and latitudinal distribution, Oak Ridge National Lab., TN (United States), Oak Ridge Inst. for Science and Education, TN (United States), available at: https://www.osti.gov/biblio/10185357 (last access:29 October 2018), 1994. 
Bardin, A., Primeau, F., and Lindsay, K.: An offline implicit solver for simulating prebomb radiocarbon, Ocean Model., 73, 45–58, https://doi.org/10.1016/j.ocemod.2013.09.008, 2014. 
Behrenfeld, M. J. and Falkowski, P. G.: Photosynthetic rates derived from satellite-based chlorophyll concentration, Limnol. Oceanogr., 42, 1–20, https://doi.org/10.4319/lo.1997.42.1.0001, 1997. 
Bouttes, N., Roche, D. M., Mariotti, V., and Bopp, L.: Including an ocean carbon cycle model into iLOVECLIM (v1.0), Geosci. Model Dev., 8, 1563–1576, https://doi.org/10.5194/gmd-8-1563-2015, 2015. 
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We have added a new tracer (13C) into the ocean of the FAMOUS climate model to study large-scale circulation and the marine carbon cycle. The model captures the large-scale spatial pattern of observations but the simulated values are consistently higher than observed. In the first instance, our new tracer is therefore useful for recalibrating the physical and biogeochemical components of the model.
We have added a new tracer (13C) into the ocean of the FAMOUS climate model to study large-scale...
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