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Carbon emissions from the 2023 Canadian wildfires

Brendan Byrne (), Junjie Liu, Kevin W. Bowman, Madeleine Pascolini-Campbell, Abhishek Chatterjee, Sudhanshu Pandey, Kazuyuki Miyazaki, Guido R. Werf, Debra Wunch, Paul O. Wennberg, Coleen M. Roehl and Saptarshi Sinha
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Brendan Byrne: California Institute of Technology
Junjie Liu: California Institute of Technology
Kevin W. Bowman: California Institute of Technology
Madeleine Pascolini-Campbell: California Institute of Technology
Abhishek Chatterjee: California Institute of Technology
Sudhanshu Pandey: California Institute of Technology
Kazuyuki Miyazaki: California Institute of Technology
Guido R. Werf: Wageningen University and Research
Debra Wunch: University of Toronto
Paul O. Wennberg: California Institute of Technology
Coleen M. Roehl: California Institute of Technology
Saptarshi Sinha: Washington University in St. Louis

Nature, 2024, vol. 633, issue 8031, 835-839

Abstract: Abstract The 2023 Canadian forest fires have been extreme in scale and intensity with more than seven times the average annual area burned compared to the previous four decades1. Here, we quantify the carbon emissions from these fires from May to September 2023 on the basis of inverse modelling of satellite carbon monoxide observations. We find that the magnitude of the carbon emissions is 647 TgC (570–727 TgC), comparable to the annual fossil fuel emissions of large nations, with only India, China and the USA releasing more carbon per year2. We find that widespread hot–dry weather was a principal driver of fire spread, with 2023 being the warmest and driest year since at least 19803. Although temperatures were extreme relative to the historical record, climate projections indicate that these temperatures are likely to be typical during the 2050s, even under a moderate climate mitigation scenario (shared socioeconomic pathway, SSP 2–4.5)4. Such conditions are likely to drive increased fire activity and suppress carbon uptake by Canadian forests, adding to concerns about the long-term durability of these forests as a carbon sink5–8.

Date: 2024
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DOI: 10.1038/s41586-024-07878-z

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