Forest fire size amplifies postfire land surface warming

Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger 1 – 3 . The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades 4 , 5 . In return, forest fires feed back to climate by modulating...

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Vydáno v:Nature (London) Ročník 633; číslo 8031; s. 828 - 834
Hlavní autoři: Zhao, Jie, Yue, Chao, Wang, Jiaming, Hantson, Stijn, Wang, Xianli, He, Binbin, Li, Guangyao, Wang, Liang, Zhao, Hongfei, Luyssaert, Sebastiaan
Médium: Journal Article
Jazyk:angličtina
Vydáno: London Nature Publishing Group UK 26.09.2024
Nature Publishing Group
Témata:
704/106/694
704/158/2465
Biogeochemistry
Boreal forests
Carbon aerosols
Climate
Climate change
Coniferous forests
Cooling
Datasets
Energy
Environmental risk
Extreme weather
Feedback
Fire weather
Forest & brush fires
Forest fires
Forest management
Forestry
Forestry - methods
Forestry - trends
Forests
Future climates
Global warming
Global Warming - statistics & numerical data
Heat
Hot Temperature
Humanities and Social Sciences
Land management
multidisciplinary
Northern Hemisphere
Permafrost
Radiation
Satellite observation
Science
Science (multidisciplinary)
Seasons
Soil degradation
Surface temperature
Taiga
Time Factors
Trees
Trees - anatomy & histology
Trees - classification
Trees - growth & development
Trees - metabolism
Wildfires - statistics & numerical data
Canada
United States > US
North America
ISSN:0028-0836, 1476-4687, 1476-4687
On-line přístup:Získat plný text
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Abstract Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger 1 – 3 . The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades 4 , 5 . In return, forest fires feed back to climate by modulating land–atmospheric carbon, nitrogen, aerosol, energy and water fluxes 6 – 8 . However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species 9 , 10 . Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration 11 , 12 as well as permafrost degradation 13 , presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests 14 , 15 , climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes. Climate warming has increased forest fire sizes, amplifying postfire summer warming, with broadleaf trees mitigating this effect; climate-smart forestry should increase broadleaf tree cover to manage future fire risks.
AbstractList Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger 1 – 3 . The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades 4 , 5 . In return, forest fires feed back to climate by modulating land–atmospheric carbon, nitrogen, aerosol, energy and water fluxes 6 – 8 . However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species 9 , 10 . Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration 11 , 12 as well as permafrost degradation 13 , presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests 14 , 15 , climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes. Climate warming has increased forest fire sizes, amplifying postfire summer warming, with broadleaf trees mitigating this effect; climate-smart forestry should increase broadleaf tree cover to manage future fire risks.
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger1-3. The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades4,5. In return, forest fires feed back to climate by modulating land-atmospheric carbon, nitrogen, aerosol, energy and water fluxes6-8. However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species9,10. Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration11,12 as well as permafrost degradation13, presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests14,15, climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes.Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger1-3. The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades4,5. In return, forest fires feed back to climate by modulating land-atmospheric carbon, nitrogen, aerosol, energy and water fluxes6-8. However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species9,10. Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration11,12 as well as permafrost degradation13, presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests14,15, climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes.
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger 1–3 . The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades 4,5 . In return, forest fires feed back to climate by modulating land–atmospheric carbon, nitrogen, aerosol, energy and water fluxes 6–8 . However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species 9,10 . Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration 11,12 as well as permafrost degradation 13 , presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests 14,15 , climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes.
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger1–3. The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades4,5. In return, forest fires feed back to climate by modulating land–atmospheric carbon, nitrogen, aerosol, energy and water fluxes6–8. However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species9,10. Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration11,12 as well as permafrost degradation13, presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests14,15, climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes. Climate warming has increased forest fire sizes, amplifying postfire summer warming, with broadleaf trees mitigating this effect; climate-smart forestry should increase broadleaf tree cover to manage future fire risks.
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger . The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades . In return, forest fires feed back to climate by modulating land-atmospheric carbon, nitrogen, aerosol, energy and water fluxes . However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species . Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration as well as permafrost degradation , presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests , climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes.
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger13. The average forest fire size in Canada, the USA and Australia has doubled or even tripled in recent decades4,5. In return, forest fires feed back to climate by modulating land-atmospheric carbon, nitrogen, aerosol, energy and water fluxes6 8. However, the surface climate impacts of increasingly large fires and their implications for land management remain to be established. Here we use satellite observations to show that in temperate and boreal forests in the Northern Hemisphere, fire size persistently amplified decade-long postfire land surface warming in summer per unit burnt area. Both warming and its amplification with fire size were found to diminish with an increasing abundance of broadleaf trees, consistent with their lower fire vulnerability compared with coniferous species9,10. Fire-size-enhanced warming may affect the success and composition of postfire stand regeneration11,12 as well as permafrost degradation13, presenting previously overlooked, additional feedback effects to future climate and fire dynamics. Given the projected increase in fire size in northern forests14,15, climate-smart forestry should aim to mitigate the climate risks of large fires, possibly by increasing the share of broadleaf trees, where appropriate, and avoiding active pyrophytes.
Author Yue, Chao
Wang, Jiaming
Li, Guangyao
Zhao, Hongfei
Luyssaert, Sebastiaan
Hantson, Stijn
Wang, Xianli
He, Binbin
Wang, Liang
Zhao, Jie
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  orcidid: 0000-0002-8104-3920
  surname: Zhao
  fullname: Zhao, Jie
  organization: College of Natural Resources and Environment, Northwest A & F University, Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, College of Resources and Environment, Linyi University, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A & F University
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  givenname: Chao
  orcidid: 0000-0003-0026-237X
  surname: Yue
  fullname: Yue, Chao
  email: chaoyuejoy@gmail.com
  organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A & F University, College of Forestry, Northwest A & F University, Institute of Future Agriculture, Northwest A & F University
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  givenname: Jiaming
  surname: Wang
  fullname: Wang, Jiaming
  organization: College of Natural Resources and Environment, Northwest A & F University
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  givenname: Stijn
  orcidid: 0000-0003-4607-9204
  surname: Hantson
  fullname: Hantson, Stijn
  organization: Faculty of Natural Sciences, Universidad del Rosario
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  givenname: Xianli
  orcidid: 0000-0001-9873-9767
  surname: Wang
  fullname: Wang, Xianli
  organization: Natural Resources Canada, Canadian Forest Service, Northern Forestry Centre
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  givenname: Binbin
  surname: He
  fullname: He, Binbin
  organization: School of Resources and Environment, University of Electronic Science and Technology of China
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  givenname: Guangyao
  surname: Li
  fullname: Li, Guangyao
  organization: College of Natural Resources and Environment, Northwest A & F University
– sequence: 8
  givenname: Liang
  surname: Wang
  fullname: Wang, Liang
  organization: Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, College of Resources and Environment, Linyi University
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  givenname: Hongfei
  surname: Zhao
  fullname: Zhao, Hongfei
  organization: College of Natural Resources and Environment, Northwest A & F University
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  orcidid: 0000-0003-1121-1869
  surname: Luyssaert
  fullname: Luyssaert, Sebastiaan
  organization: Amsterdam Institute for Life and Environment (A-LIFE), Department of Ecological Sciences, Vrije Universiteit Amsterdam
BackLink https://www.ncbi.nlm.nih.gov/pubmed/39322733$$D View this record in MEDLINE/PubMed
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ContentType Journal Article
Copyright His Majesty the King in Right of Canada as represented by the Minister of Natural Resources, and the Authors 2024
2024. The Author(s).
Copyright Nature Publishing Group Sep 26, 2024
The Author(s) 2024 2024
Copyright_xml – notice: His Majesty the King in Right of Canada as represented by the Minister of Natural Resources, and the Authors 2024
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DOI 10.1038/s41586-024-07918-8
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Snippet Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger 1 – 3 . The average forest fire size in...
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger 1–3 . The average forest fire size in...
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger . The average forest fire size in Canada,...
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger13. The average forest fire size in...
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger1-3. The average forest fire size in...
Climate warming has caused a widespread increase in extreme fire weather, making forest fires longer-lived and larger1–3. The average forest fire size in...
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SubjectTerms 704/106/694
704/158/2465
Biogeochemistry
Boreal forests
Carbon aerosols
Climate
Climate change
Coniferous forests
Cooling
Datasets
Energy
Environmental risk
Extreme weather
Feedback
Fire weather
Forest & brush fires
Forest fires
Forest management
Forestry
Forestry - methods
Forestry - trends
Forests
Future climates
Global warming
Global Warming - statistics & numerical data
Heat
Hot Temperature
Humanities and Social Sciences
Land management
multidisciplinary
Northern Hemisphere
Permafrost
Radiation
Satellite observation
Science
Science (multidisciplinary)
Seasons
Soil degradation
Surface temperature
Taiga
Time Factors
Trees
Trees - anatomy & histology
Trees - classification
Trees - growth & development
Trees - metabolism
Wildfires - statistics & numerical data
Title Forest fire size amplifies postfire land surface warming
URI https://link.springer.com/article/10.1038/s41586-024-07918-8
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