Articles | Volume 16, issue 19
https://doi.org/10.5194/bg-16-3883-2019
© Author(s) 2019. 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-16-3883-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Oct 2019
Research article |
| 09 Oct 2019
| 09 Oct 2019
Response of simulated burned area to historical changes in environmental and anthropogenic factors: a comparison of seven fire models
Lina Teckentrup
Max Planck Institute for Meteorology, Land in the Earth System, Bundesstraße 53, Hamburg, Germany
Sandy P. Harrison
School of Archaeology, Geography and Environmental Sciences (SAGES), University of Reading, Whiteknights, Reading, UK
Stijn Hantson
Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research, Atmospheric Environmental Research, 82467 Garmisch-Partenkirchen, Germany
Angelika Heil
Max Planck Institute for Meteorology, Land in the Earth System, Bundesstraße 53, Hamburg, Germany
Joe R. Melton
Climate Research Division, Environment Canada, Victoria, BC, V8W 2Y2, Canada
Matthew Forrest
Senckenberg Biodiversity and Climate Research Institute (BiK-F), 60325 Frankfurt am Main, Germany
International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
Chao Yue
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL,CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
Almut Arneth
Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research, Atmospheric Environmental Research, 82467 Garmisch-Partenkirchen, Germany
Thomas Hickler
Senckenberg Biodiversity and Climate Research Institute (BiK-F), 60325 Frankfurt am Main, Germany
Stephen Sitch
College of Life and Environmental Sciences, University of Exeter, Exeter, UK
Gitta Lasslop
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Land in the Earth System, Bundesstraße 53, Hamburg, Germany
Senckenberg Biodiversity and Climate Research Institute (BiK-F), 60325 Frankfurt am Main, Germany
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- Increased burning in a warming climate reduces carbon uptake in the Greater Yellowstone Ecosystem despite productivity gains P. Henne et al. 10.1111/1365-2745.13559
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Latest update: 19 Nov 2024
Short summary
This study compares simulated burned area of seven global vegetation models provided by the Fire Model Intercomparison Project (FireMIP) since 1900. We investigate the influence of five forcing factors: atmospheric CO2, population density, land–use change, lightning and climate.
We find that the anthropogenic factors lead to the largest spread between models. Trends due to climate are mostly not significant but climate strongly influences the inter-annual variability of burned area.
This study compares simulated burned area of seven global vegetation models provided by the Fire...
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