Articles | Volume 18, issue 12
https://doi.org/10.5194/bg-18-3861-2021
© Author(s) 2021. 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-18-3861-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The importance of antecedent vegetation and drought conditions as global drivers of burnt area
Alexander Kuhn-Régnier
CORRESPONDING AUTHOR
Leverhulme Centre for Wildfires, Environment, and Society, London, SW7 2AZ, UK
Department of Physics, Imperial College London, London, SW7 2AZ, UK
Apostolos Voulgarakis
Leverhulme Centre for Wildfires, Environment, and Society, London, SW7 2AZ, UK
Department of Physics, Imperial College London, London, SW7 2AZ, UK
School of Environmental Engineering, Technical University of Crete, Chania, Kounoupidiana,
Akrotiri, 73100 Chania, Greece
Peer Nowack
Department of Physics, Imperial College London, London, SW7 2AZ, UK
Grantham Institute and the Data Science Institute, Imperial College London, London, SW7 2AZ, UK
Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK
Matthias Forkel
Environmental Remote Sensing Group, TU Dresden, Dresden, Germany
I. Colin Prentice
Leverhulme Centre for Wildfires, Environment, and Society, London, SW7 2AZ, UK
Department of Life Sciences, Imperial College London, London, SW7 2AZ, UK
Sandy P. Harrison
Leverhulme Centre for Wildfires, Environment, and Society, London, SW7 2AZ, UK
Geography and Environmental Science, University of Reading, Reading, RG6 6AB, UK
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18 citations as recorded by crossref.
- Estimating leaf moisture content at global scale from passive microwave satellite observations of vegetation optical depth M. Forkel et al. 10.5194/hess-27-39-2023
- Climate drivers of global wildfire burned area M. Grillakis et al. 10.1088/1748-9326/ac5fa1
- The global drivers of wildfire O. Haas et al. 10.3389/fenvs.2024.1438262
- Land and Atmosphere Precursors to Fuel Loading, Wildfire Ignition and Post‐Fire Recovery M. Alizadeh et al. 10.1029/2023GL105324
- High Resolution Forecasting of Summer Drought in the Western United States R. Abolafia‐Rosenzweig et al. 10.1029/2022WR033734
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- High-resolution mapping of wildfire drivers in California based on machine learning L. Qiu et al. 10.1016/j.scitotenv.2022.155155
- Modelling the daily probability of wildfire occurrence in the contiguous United States T. Keeping et al. 10.1088/1748-9326/ad21b0
- SMLFire1.0: a stochastic machine learning (SML) model for wildfire activity in the western United States J. Buch et al. 10.5194/gmd-16-3407-2023
- The response of wildfire regimes to Last Glacial Maximum carbon dioxide and climate O. Haas et al. 10.5194/bg-20-3981-2023
- Winter and spring climate explains a large portion of interannual variability and trend in western U.S. summer fire burned area R. Abolafia-Rosenzweig et al. 10.1088/1748-9326/ac6886
- Reconstructing burnt area during the Holocene: an Iberian case study Y. Shen et al. 10.5194/cp-18-1189-2022
- Monitoring post-fire recovery of various vegetation biomes using multi-wavelength satellite remote sensing E. Bousquet et al. 10.5194/bg-19-3317-2022
- Forest fire threatens global carbon sinks and population centres under rising atmospheric water demand H. Clarke et al. 10.1038/s41467-022-34966-3
- A data-driven model for Fennoscandian wildfire danger S. Bakke et al. 10.5194/nhess-23-65-2023
- Assessing the sensitivity of multi-frequency passive microwave vegetation optical depth to vegetation properties L. Schmidt et al. 10.5194/bg-20-1027-2023
- A machine learning approach to quantify meteorological drivers of ozone pollution in China from 2015 to 2019 X. Weng et al. 10.5194/acp-22-8385-2022
- Global environmental controls on wildfire burnt area, size, and intensity O. Haas et al. 10.1088/1748-9326/ac6a69
1 citations as recorded by crossref.
Latest update: 01 Nov 2024
Short summary
Along with current climate, vegetation, and human influences, long-term accumulation of biomass affects fires. Here, we find that including the influence of antecedent vegetation and moisture improves our ability to predict global burnt area. Additionally, the length of the preceding period which needs to be considered for accurate predictions varies across regions.
Along with current climate, vegetation, and human influences, long-term accumulation of biomass...
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