Articles | Volume 9, issue 2
https://doi.org/10.5194/esd-9-663-2018
© 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/esd-9-663-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
28 May 2018
Research article |
| 28 May 2018
| 28 May 2018
The biomass burning contribution to climate–carbon-cycle feedback
Sandy P. Harrison
CORRESPONDING AUTHOR
Department of Geography and Environmental Science, University of
Reading, Whiteknights, Reading, RG6 6AB, UK
Patrick J. Bartlein
Department of Geography, University of Oregon, Eugene, Oregon
97403–1251, USA
Victor Brovkin
Max Planck Institute for Meteorology, Bundesstraße 53, 20146
Hamburg, Germany
Sander Houweling
Department of Earth Sciences, Vrije Universiteit Amsterdam, De
Boelelaan 1085, 1081 HV Amsterdam, The Netherlands
Silvia Kloster
Max Planck Institute for Meteorology, Bundesstraße 53, 20146
Hamburg, Germany
I. Colin Prentice
AXA Chair of Biosphere and Climate Impacts, Department of Life
Sciences, Imperial College London, Ascot, SL5 7PY, UK
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Cited
23 citations as recorded by crossref.
- Scientists’ warning on wildfire — a Canadian perspective S. Coogan et al. 10.1139/cjfr-2019-0094
- Mid-Holocene European climate revisited: New high-resolution regional climate model simulations using pollen-based land-cover G. Strandberg et al. 10.1016/j.quascirev.2022.107431
- Impacts of different biomass burning emission inventories: Simulations of atmospheric CO2 concentrations based on GEOS-Chem M. Su et al. 10.1016/j.scitotenv.2023.162825
- Evidence for fire in the Pliocene Arctic in response to amplified temperature T. Fletcher et al. 10.5194/cp-15-1063-2019
- Fire air pollution reduces global terrestrial productivity X. Yue & N. Unger 10.1038/s41467-018-07921-4
- The Reading Palaeofire Database: an expanded global resource to document changes in fire regimes from sedimentary charcoal records S. Harrison et al. 10.5194/essd-14-1109-2022
- The black carbon cycle and its role in the Earth system A. Coppola et al. 10.1038/s43017-022-00316-6
- Modelling Human-Fire Interactions: Combining Alternative Perspectives and Approaches A. Ford et al. 10.3389/fenvs.2021.649835
- Reduced global fire activity due to human demography slows global warming by enhanced land carbon uptake C. Wu et al. 10.1073/pnas.2101186119
- Global and Regional Trends and Drivers of Fire Under Climate Change M. Jones et al. 10.1029/2020RG000726
- Influence of Fire on the Carbon Cycle and Climate G. Lasslop et al. 10.1007/s40641-019-00128-9
- Climate and fire drivers of forest composition and openness in the Changbai Mountains since the Late Glacial M. Meng et al. 10.1016/j.fecs.2023.100127
- Response of simulated burned area to historical changes in environmental and anthropogenic factors: a comparison of seven fire models L. Teckentrup et al. 10.5194/bg-16-3883-2019
- The spatial and temporal impact of agricultural crop residual burning on local land surface temperature in three provinces across China from 2015 to 2017 W. Zhang et al. 10.1016/j.jclepro.2020.124057
- A horizon scan of global biological conservation issues for 2024 W. Sutherland et al. 10.1016/j.tree.2023.11.001
- Chemical Fingerprinting of Biomass Burning Organic Aerosols from Sugar Cane Combustion: Complementary Findings from Field and Laboratory Studies E. Hartner et al. 10.1021/acsearthspacechem.3c00301
- Carbon balance and fire emissions in Andean cypress (Austrocedrus chilensis) forests of Patagonia, Argentina G. Defossé et al. 10.1071/WF19183
- Methane Emissions in Boreal Forest Fire Regions: Assessment of Five Biomass-Burning Emission Inventories Based on Carbon Sensing Satellites S. Zhao et al. 10.3390/rs15184547
- Integration of a Deep‐Learning‐Based Fire Model Into a Global Land Surface Model R. Son et al. 10.1029/2023MS003710
- Influence of uncertainties in burned area estimates on modeled wildland fire PM2.5 and ozone pollution in the contiguous U.S. S. Koplitz et al. 10.1016/j.atmosenv.2018.08.020
- Survey-based inventory for atmospheric emissions from residential combustion in Vietnam L. Huy et al. 10.1007/s11356-020-11067-6
- Linking fire and the United Nations Sustainable Development Goals D. Martin 10.1016/j.scitotenv.2018.12.393
- Holocene fire activity during low-natural flammability periods reveals scale-dependent cultural human-fire relationships in Europe E. Dietze et al. 10.1016/j.quascirev.2018.10.005
22 citations as recorded by crossref.
- Scientists’ warning on wildfire — a Canadian perspective S. Coogan et al. 10.1139/cjfr-2019-0094
- Mid-Holocene European climate revisited: New high-resolution regional climate model simulations using pollen-based land-cover G. Strandberg et al. 10.1016/j.quascirev.2022.107431
- Impacts of different biomass burning emission inventories: Simulations of atmospheric CO2 concentrations based on GEOS-Chem M. Su et al. 10.1016/j.scitotenv.2023.162825
- Evidence for fire in the Pliocene Arctic in response to amplified temperature T. Fletcher et al. 10.5194/cp-15-1063-2019
- Fire air pollution reduces global terrestrial productivity X. Yue & N. Unger 10.1038/s41467-018-07921-4
- The Reading Palaeofire Database: an expanded global resource to document changes in fire regimes from sedimentary charcoal records S. Harrison et al. 10.5194/essd-14-1109-2022
- The black carbon cycle and its role in the Earth system A. Coppola et al. 10.1038/s43017-022-00316-6
- Modelling Human-Fire Interactions: Combining Alternative Perspectives and Approaches A. Ford et al. 10.3389/fenvs.2021.649835
- Reduced global fire activity due to human demography slows global warming by enhanced land carbon uptake C. Wu et al. 10.1073/pnas.2101186119
- Global and Regional Trends and Drivers of Fire Under Climate Change M. Jones et al. 10.1029/2020RG000726
- Influence of Fire on the Carbon Cycle and Climate G. Lasslop et al. 10.1007/s40641-019-00128-9
- Climate and fire drivers of forest composition and openness in the Changbai Mountains since the Late Glacial M. Meng et al. 10.1016/j.fecs.2023.100127
- Response of simulated burned area to historical changes in environmental and anthropogenic factors: a comparison of seven fire models L. Teckentrup et al. 10.5194/bg-16-3883-2019
- The spatial and temporal impact of agricultural crop residual burning on local land surface temperature in three provinces across China from 2015 to 2017 W. Zhang et al. 10.1016/j.jclepro.2020.124057
- A horizon scan of global biological conservation issues for 2024 W. Sutherland et al. 10.1016/j.tree.2023.11.001
- Chemical Fingerprinting of Biomass Burning Organic Aerosols from Sugar Cane Combustion: Complementary Findings from Field and Laboratory Studies E. Hartner et al. 10.1021/acsearthspacechem.3c00301
- Carbon balance and fire emissions in Andean cypress (Austrocedrus chilensis) forests of Patagonia, Argentina G. Defossé et al. 10.1071/WF19183
- Methane Emissions in Boreal Forest Fire Regions: Assessment of Five Biomass-Burning Emission Inventories Based on Carbon Sensing Satellites S. Zhao et al. 10.3390/rs15184547
- Integration of a Deep‐Learning‐Based Fire Model Into a Global Land Surface Model R. Son et al. 10.1029/2023MS003710
- Influence of uncertainties in burned area estimates on modeled wildland fire PM2.5 and ozone pollution in the contiguous U.S. S. Koplitz et al. 10.1016/j.atmosenv.2018.08.020
- Survey-based inventory for atmospheric emissions from residential combustion in Vietnam L. Huy et al. 10.1007/s11356-020-11067-6
- Linking fire and the United Nations Sustainable Development Goals D. Martin 10.1016/j.scitotenv.2018.12.393
Latest update: 24 Apr 2024
Short summary
Temperature affects fire occurrence and severity. Warming will increase fire-related carbon emissions and thus atmospheric CO2. The size of this feedback is not known. We use charcoal records to estimate pre-industrial fire emissions and a simple land–biosphere model to quantify the feedback. We infer a feedback strength of 5.6 3.2 ppm CO2 per degree of warming and a gain of 0.09 ± 0.05 for a climate sensitivity of 2.8 K. Thus, fire feedback is a large part of the climate–carbon-cycle feedback.
Temperature affects fire occurrence and severity. Warming will increase fire-related carbon...
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