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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 8, issue 9
Geosci. Model Dev., 8, 2929–2957, 2015
https://doi.org/10.5194/gmd-8-2929-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The Transport Matrix Method (TMM) for ocean biogeochemical...

Geosci. Model Dev., 8, 2929–2957, 2015
https://doi.org/10.5194/gmd-8-2929-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Development and technical paper 23 Sep 2015

Development and technical paper | 23 Sep 2015

MOPS-1.0: towards a model for the regulation of the global oceanic nitrogen budget by marine biogeochemical processes

I. Kriest and A. Oschlies

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Cited articles

Anderson, L.: On the hydrogen and oxygen content of marine phytoplankton, Deep-Sea Res. Pt. I, 42, 1675–1680, 1995.
Anderson, L. and Sarmiento, J.: Redfield ratios of remineralization determined by nutrient data analysis, Global Biogeochem. Cy., 8, 65–80, 1994.
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Aumont, O., Ethé, C., Tagliabue, A., Bopp, L., and Gehlen, M.: PISCES-v2: an ocean biogeochemical model for carbon and ecosystem studies, Geosci. Model Dev., 8, 2465–2513, https://doi.org/10.5194/gmd-8-2465-2015, 2015.
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We use a global model of oceanic P, N, and O2 cycles to investigate consequences of uncertainties in description of organic matter sinking, remineralization, denitrification, and N2-Fixation. After all biogeochemical and physical processes have been spun-up into a dynamically consistent steady-state, particle sinking and oxidant affinities of aerobic and anaerobic remineralization determine the extent of oxygen minimum zones, global nitrogen fluxes, and the oceanic nitrogen inventory.
We use a global model of oceanic P, N, and O2 cycles to investigate consequences of...
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