Publisher Correction: Radiative forcing geoengineering under high CO2 levels leads to higher risk of Arctic wildfires and permafrost thaw than a targeted mitigation scenario
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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1 Online-Ressource.
- Language
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Englisch
- Bibliographic citation
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Publisher Correction: Radiative forcing geoengineering under high CO2 levels leads to higher risk of Arctic wildfires and permafrost thaw than a targeted mitigation scenario ; volume:5 ; number:1 ; day:14 ; month:6 ; year:2024 ; pages:1 ; date:12.2024
Communications earth & environment ; 5, Heft 1 (14.6.2024), 1, 12.2024
- Creator
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Müller, Rhonda C.
Kim, Jin-Soo
Lee, Hanna
Muri, Helene
Tjiputra, Jerry
Yoon, Jin-Ho
Schaepman-Strub, Gabriela
- Contributor
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SpringerLink (Online service)
- DOI
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10.1038/s43247-024-01501-9
- URN
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urn:nbn:de:101:1-2408210905163.214525748046
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:44 AM CEST
Data provider
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Associated
- Müller, Rhonda C.
- Kim, Jin-Soo
- Lee, Hanna
- Muri, Helene
- Tjiputra, Jerry
- Yoon, Jin-Ho
- Schaepman-Strub, Gabriela
- SpringerLink (Online service)
Other Objects (12)
Radiative forcing geoengineering under high CO2 levels leads to higher risk of Arctic wildfires and permafrost thaw than a targeted mitigation scenario
Abrupt increase in Arctic-Subarctic wildfires caused by future permafrost thaw
Methanotrophy across a natural permafrost thaw environment
Informative risk analyses of radiative forcing geoengineering require proper counterfactuals
Impact of solar geoengineering on wildfires in the 21st century in CESM2/WACCM6
Impact of Solar Geoengineering on Wildfires in the 21st Century in CESM2/WACCM6
Phototrophic pigment diversity and picophytoplankton in permafrost thaw lakes
Organic matter stored in ice-rich permafrost : future permafrost thaw and greenhouse gas release
Reply to: Informative analyses of radiative forcing geoengineering require proper counterfactuals
Iron transformation mediates phosphate retention across a permafrost thaw gradient
Dark brown carbon from wildfires: a potent snow radiative forcing agent?
Review article: Inferring permafrost and permafrost thaw in the mountains of the Hindu Kush Himalaya region
Radiative forcing geoengineering under high CO2 levels leads to higher risk of Arctic wildfires and permafrost thaw than a targeted mitigation scenario
Abrupt increase in Arctic-Subarctic wildfires caused by future permafrost thaw
Methanotrophy across a natural permafrost thaw environment
Informative risk analyses of radiative forcing geoengineering require proper counterfactuals
Impact of solar geoengineering on wildfires in the 21st century in CESM2/WACCM6
Impact of Solar Geoengineering on Wildfires in the 21st Century in CESM2/WACCM6
Phototrophic pigment diversity and picophytoplankton in permafrost thaw lakes
Organic matter stored in ice-rich permafrost : future permafrost thaw and greenhouse gas release
Reply to: Informative analyses of radiative forcing geoengineering require proper counterfactuals
Iron transformation mediates phosphate retention across a permafrost thaw gradient
Dark brown carbon from wildfires: a potent snow radiative forcing agent?
Review article: Inferring permafrost and permafrost thaw in the mountains of the Hindu Kush Himalaya region
Radiative forcing geoengineering under high CO2 levels leads to higher risk of Arctic wildfires and permafrost thaw than a targeted mitigation scenario
Abrupt increase in Arctic-Subarctic wildfires caused by future permafrost thaw
Methanotrophy across a natural permafrost thaw environment
Informative risk analyses of radiative forcing geoengineering require proper counterfactuals
Impact of solar geoengineering on wildfires in the 21st century in CESM2/WACCM6
Impact of Solar Geoengineering on Wildfires in the 21st Century in CESM2/WACCM6
Phototrophic pigment diversity and picophytoplankton in permafrost thaw lakes
Organic matter stored in ice-rich permafrost : future permafrost thaw and greenhouse gas release
Reply to: Informative analyses of radiative forcing geoengineering require proper counterfactuals
Iron transformation mediates phosphate retention across a permafrost thaw gradient
Dark brown carbon from wildfires: a potent snow radiative forcing agent?