Articles | Volume 15, issue 14
https://doi.org/10.5194/bg-15-4459-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-15-4459-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Global soil organic carbon removal by water erosion under climate change and land use change during AD 1850–2005
Victoria Naipal
CORRESPONDING AUTHOR
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS
UVSQ, Gif-sur-Yvette 91191, France
Philippe Ciais
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS
UVSQ, Gif-sur-Yvette 91191, France
Yilong Wang
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS
UVSQ, Gif-sur-Yvette 91191, France
Ronny Lauerwald
Department of Geoscience,
Environment and Society, Université Libre de Bruxelles, Brussels,
Belgium
Department of Mathematics, College of Engineering, Mathematics and
Physical Sciences, University of Exeter, Exeter, UK
Bertrand Guenet
Laboratoire des Sciences du Climat et de l'Environnement, CEA CNRS
UVSQ, Gif-sur-Yvette 91191, France
Kristof Van Oost
Université catholique de Louvain, TECLIM – Georges Lemaître
Centre for Earth and Climate Research, Louvain-la-Neuve, Belgium
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Latest update: 06 Dec 2024
Short summary
We seek to better understand the links between soil erosion by rainfall and the global carbon (C) cycle by coupling a soil erosion model to the C cycle of a land surface model. With this modeling approach we evaluate the effects of soil removal on soil C stocks in the presence of climate change and land use change. We find that accelerated soil erosion leads to a potential SOC removal flux of 74 ±18 Pg of C globally over the period AD 1850–2005, with significant impacts on the land C balance.
We seek to better understand the links between soil erosion by rainfall and the global carbon...
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