Articles | Volume 10, issue 5
https://doi.org/10.5194/gmd-10-2009-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-10-2009-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Model description paper
| 
22 May 2017
Model description paper |
| 22 May 2017
Carbon–nitrogen interactions in idealized simulations with JSBACH (version 3.10)
Le Laboratoire des Sciences du Climat et de l'Environnement, IPSL-LSCE CEA/CNRS/UVSQ Saclay, Gif sur Yvette, France
formerly at: Max Planck Institute for Meteorology, Hamburg, Germany
Alexander J. Winkler
Max Planck Institute for Meteorology, Hamburg, Germany
International Max Planck Research School on Earth System Modeling, Hamburg, Germany
Thomas Raddatz
Max Planck Institute for Meteorology, Hamburg, Germany
Ning Dong
International Max Planck Research School on Earth System Modeling, Hamburg, Germany
Faculty of Agriculture and Environment, Department of Environmental Sciences, University of Sydney, NSW 2006, Australia
Ian Colin Prentice
Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia
AXA Chair in Biosphere and Climate Impacts, Department of Life Sciences, Imperial College London, Silwood Park Campus, Buckhurst Road, Ascot SL5 7PY, UK
Philippe Ciais
Le Laboratoire des Sciences du Climat et de l'Environnement, IPSL-LSCE CEA/CNRS/UVSQ Saclay, Gif sur Yvette, France
Victor Brovkin
Max Planck Institute for Meteorology, Hamburg, Germany
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Short summary
The response of soil organic carbon decomposition to warming and the interactions between nitrogen and carbon cycling affect the feedbacks between the land carbon cycle and the climate. In the model JSBACH carbon–nitrogen interactions have only a small effect on the feedbacks, whereas modifications of soil organic carbon decomposition have a large effect. The carbon cycle in the improved model is more resilient to climatic changes than in previous version of the model.
The response of soil organic carbon decomposition to warming and the interactions between...
