Articles | Volume 18, issue 7
https://doi.org/10.5194/gmd-18-2193-2025
https://doi.org/10.5194/gmd-18-2193-2025
Methods for assessment of models
 | 
08 Apr 2025
Methods for assessment of models |  | 08 Apr 2025

Synthesizing global carbon–nitrogen coupling effects – the MAGICC coupled carbon–nitrogen cycle model v1.0

Gang Tang, Zebedee Nicholls, Alexander Norton, Sönke Zaehle, and Malte Meinshausen

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This preprint is open for discussion and under review for Geoscientific Model Development (GMD).
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Cited articles

Alvarez-Clare, S., Mack, M. C., and Brooks, M.: A direct test of nitrogen and phosphorus limitation to net primary productivity in a lowland tropical wet forest, Ecology, 94, 1540–1551, https://doi.org/10.1890/12-2128.1, 2013. 
Anav, A., Friedlingstein, P., Kidston, M., Bopp, L., Ciais, P., Cox, P., Jones, C., Jung, M., Myneni, R., and Zhu, Z.: Evaluating the Land and Ocean Components of the Global Carbon Cycle in the CMIP5 Earth System Models, J. Climate, 26, 6801–6843, https://doi.org/10.1175/JCLI-D-12-00417.1, 2013. 
Averill, C. and Waring, B.: Nitrogen limitation of decomposition and decay: How can it occur?, Global Change Biol., 24, 1417–1427, https://doi.org/10.1111/gcb.13980, 2018. 
Bacastow, R. and Keeling, C. D.: Atmospheric carbon dioxide and radiocarbon in the natural carbon cycle: II. Changes from AD 1700 to 2070 as deduced from a geochemical model, in: Carbon and the biosphere; proceedings of the 24th Brookhaven symposium in biology, edited by: Woodwell, G. M. and Pecan, E. V., Technical Information Center, Office of Information Services, US Atomic Energy Commission, Springfield, Virginia, USA, 86–135, https://doi.org/10.5962/bhl.title.4036, 1973. 
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Short summary
We studied carbon–nitrogen coupling in Earth system models by developing a global carbon–nitrogen cycle model (CNit v1.0) within the widely used emulator MAGICC. CNit effectively reproduced the global carbon–nitrogen cycle dynamics observed in complex models. Our results show persistent nitrogen limitations on plant growth (net primary production) from 1850 to 2100, suggesting that nitrogen deficiency may constrain future land carbon sequestration.
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