Articles | Volume 15, issue 11
https://doi.org/10.5194/essd-15-5227-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-15-5227-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Multi-decadal trends and variability in burned area from the fifth version of the Global Fire Emissions Database (GFED5)
Department of Earth System Science, University of California, Irvine, CA, USA
Joanne Hall
Department of Geographical Sciences, University of Maryland, College Park, MD, USA
Dave van Wees
Faculty of Science, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
Niels Andela
BeZero Carbon, London, UK
Stijn Hantson
Earth System Science Program, Faculty of Natural Sciences, Universidad del Rosario, Bogota, Colombia
Louis Giglio
Department of Geographical Sciences, University of Maryland, College Park, MD, USA
Guido R. van der Werf
Faculty of Science, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
Douglas C. Morton
Biospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
James T. Randerson
Department of Earth System Science, University of California, Irvine, CA, USA
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24 citations as recorded by crossref.
- Road fragment edges enhance wildfire incidence and intensity, while suppressing global burned area S. Bowring et al. 10.1038/s41467-024-53460-6
- Drought-fuelled overnight burning propels large fires in North America J. Balch & A. Mahood 10.1038/d41586-024-00536-4
- Soil and Water Bioengineering in Fire-Prone Lands: Detecting Erosive Areas Using RUSLE and Remote Sensing Methods M. Maxwald et al. 10.3390/fire7090319
- California wildfire smoke contributes to a positive atmospheric temperature anomaly over the western United States J. Gomez et al. 10.5194/acp-24-6937-2024
- GloCAB: global cropland burned area from mid-2002 to 2020 J. Hall et al. 10.5194/essd-16-867-2024
- Attribution of summer 2022 extreme wildfire season in Southwest France to anthropogenic climate change M. Lanet et al. 10.1038/s41612-024-00821-z
- INFERNO-peat v1.0.0: a representation of northern high-latitude peat fires in the JULES-INFERNO global fire model K. Blackford et al. 10.5194/gmd-17-3063-2024
- Regional-Scale Assessment of Burn Scar Mapping in Southwestern Amazonia Using Burned Area Products and CBERS/WFI Data Cubes P. Ferro et al. 10.3390/fire7030067
- The rising threat of wildfire: an examination of global forest fire occurrence over the past two decades M. Luo et al. 10.1505/146554824838819860
- State of Wildfires 2023–2024 M. Jones et al. 10.5194/essd-16-3601-2024
- The global drivers of wildfire O. Haas et al. 10.3389/fenvs.2024.1438262
- Model fires, not ignitions: Capturing the human dimension of global fire regimes M. Kasoar et al. 10.1016/j.crsus.2024.100128
- Madagascar's burned area from Sentinel-2 imagery (2016–2022): Four times higher than from lower resolution sensors V. Fernández-García et al. 10.1016/j.scitotenv.2024.169929
- The Global Forest Fire Emissions Prediction System version 1.0 K. Anderson et al. 10.5194/gmd-17-7713-2024
- Are Northern Hemisphere boreal forest fires more sensitive to future aerosol mitigation than to greenhouse gas–driven warming? R. Allen et al. 10.1126/sciadv.adl4007
- A global behavioural model of human fire use and management: WHAM! v1.0 O. Perkins et al. 10.5194/gmd-17-3993-2024
- Assessment of the effectiveness of coarse resolution fire products in monitoring long-term changes in fire regime within protected areas in South Africa M. Zubkova et al. 10.1016/j.jag.2024.104064
- The GFDL Variable‐Resolution Global Chemistry‐Climate Model for Research at the Nexus of US Climate and Air Quality Extremes M. Lin et al. 10.1029/2023MS003984
- Remote sensing for wildfire monitoring: Insights into burned area, emissions, and fire dynamics Y. Chen et al. 10.1016/j.oneear.2024.05.014
- A new lightning scheme in the Canadian Atmospheric Model (CanAM5.1): implementation, evaluation, and projections of lightning and fire in future climates C. Whaley et al. 10.5194/gmd-17-7141-2024
- Annual and Seasonal Patterns of Burned Area Products in Arctic-Boreal North America and Russia for 2001–2020 A. Clelland et al. 10.3390/rs16173306
- High Resolution (30 m) Burned Area Product Improves the Ability for Carbon Emission Estimation in Africa B. Qi et al. 10.1029/2024EF005051
- Global burned area increasingly explained by climate change C. Burton et al. 10.1038/s41558-024-02140-w
- Extratropical forests increasingly at risk due to lightning fires T. Janssen et al. 10.1038/s41561-023-01322-z
23 citations as recorded by crossref.
- Road fragment edges enhance wildfire incidence and intensity, while suppressing global burned area S. Bowring et al. 10.1038/s41467-024-53460-6
- Drought-fuelled overnight burning propels large fires in North America J. Balch & A. Mahood 10.1038/d41586-024-00536-4
- Soil and Water Bioengineering in Fire-Prone Lands: Detecting Erosive Areas Using RUSLE and Remote Sensing Methods M. Maxwald et al. 10.3390/fire7090319
- California wildfire smoke contributes to a positive atmospheric temperature anomaly over the western United States J. Gomez et al. 10.5194/acp-24-6937-2024
- GloCAB: global cropland burned area from mid-2002 to 2020 J. Hall et al. 10.5194/essd-16-867-2024
- Attribution of summer 2022 extreme wildfire season in Southwest France to anthropogenic climate change M. Lanet et al. 10.1038/s41612-024-00821-z
- INFERNO-peat v1.0.0: a representation of northern high-latitude peat fires in the JULES-INFERNO global fire model K. Blackford et al. 10.5194/gmd-17-3063-2024
- Regional-Scale Assessment of Burn Scar Mapping in Southwestern Amazonia Using Burned Area Products and CBERS/WFI Data Cubes P. Ferro et al. 10.3390/fire7030067
- The rising threat of wildfire: an examination of global forest fire occurrence over the past two decades M. Luo et al. 10.1505/146554824838819860
- State of Wildfires 2023–2024 M. Jones et al. 10.5194/essd-16-3601-2024
- The global drivers of wildfire O. Haas et al. 10.3389/fenvs.2024.1438262
- Model fires, not ignitions: Capturing the human dimension of global fire regimes M. Kasoar et al. 10.1016/j.crsus.2024.100128
- Madagascar's burned area from Sentinel-2 imagery (2016–2022): Four times higher than from lower resolution sensors V. Fernández-García et al. 10.1016/j.scitotenv.2024.169929
- The Global Forest Fire Emissions Prediction System version 1.0 K. Anderson et al. 10.5194/gmd-17-7713-2024
- Are Northern Hemisphere boreal forest fires more sensitive to future aerosol mitigation than to greenhouse gas–driven warming? R. Allen et al. 10.1126/sciadv.adl4007
- A global behavioural model of human fire use and management: WHAM! v1.0 O. Perkins et al. 10.5194/gmd-17-3993-2024
- Assessment of the effectiveness of coarse resolution fire products in monitoring long-term changes in fire regime within protected areas in South Africa M. Zubkova et al. 10.1016/j.jag.2024.104064
- The GFDL Variable‐Resolution Global Chemistry‐Climate Model for Research at the Nexus of US Climate and Air Quality Extremes M. Lin et al. 10.1029/2023MS003984
- Remote sensing for wildfire monitoring: Insights into burned area, emissions, and fire dynamics Y. Chen et al. 10.1016/j.oneear.2024.05.014
- A new lightning scheme in the Canadian Atmospheric Model (CanAM5.1): implementation, evaluation, and projections of lightning and fire in future climates C. Whaley et al. 10.5194/gmd-17-7141-2024
- Annual and Seasonal Patterns of Burned Area Products in Arctic-Boreal North America and Russia for 2001–2020 A. Clelland et al. 10.3390/rs16173306
- High Resolution (30 m) Burned Area Product Improves the Ability for Carbon Emission Estimation in Africa B. Qi et al. 10.1029/2024EF005051
- Global burned area increasingly explained by climate change C. Burton et al. 10.1038/s41558-024-02140-w
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
Using multiple sets of remotely sensed data, we created a dataset of monthly global burned area from 1997 to 2020. The estimated annual global burned area is 774 million hectares, significantly higher than previous estimates. Burned area declined by 1.21% per year due to extensive fire loss in savanna, grassland, and cropland ecosystems. This study enhances our understanding of the impact of fire on the carbon cycle and climate system, and may improve the predictions of future fire changes.
Using multiple sets of remotely sensed data, we created a dataset of monthly global burned area...
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