Arctic wildfire carbon emissions strongly influenced by midsummer Tibetan Plateau precipitation

Abstract Wildfires in the Arctic are accelerating ecosystem damage and increasing global carbon emissions. Siberia, a major Arctic wildfire hotspot, is shaped by both local weather and distant climate influences. Here we use climate reanalysis data and numerical model experiments to show that summer wildfires in Siberia are strongly influenced by rainfall patterns over the Tibetan Plateau, one of the Northern Hemisphere’s largest summer heat sources. A dipole in Tibetan Plateau rainfall—wetter in the west, drier in the east—coincides with more fires in central Siberia and fewer in the east. This pattern alters high-altitude winds, shifting the jet stream northward and generating air flow changes that create favorable fire conditions across Siberia. Model experiments support a causal link. The resulting carbon dioxide emissions can match annual emissions from all Nordic countries. These findings highlight an overlooked driver of Arctic wildfires and improve our understanding of their role in the global carbon cycle.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-07-16
DOI
https://doi.org/10.1038/s43247-025-02505-9
Citations
1
Primary Topic
Fire effects on ecosystems
Type
article
Field-Weighted Citation Impact
1.11

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article

Arctic wildfire carbon emissions strongly influenced by midsummer Tibetan Plateau precipitation

Ziqian Zhong, Gang Zeng, Hui‐Wen Lai, Tinghai Ou et al.
1 citations
Communications Earth & Environment
Fire effects on ecosystems
1.11
article

Arctic wildfire carbon emissions strongly influenced by midsummer Tibetan Plateau precipitation

Ziqian Zhong, Gang Zeng, Hui‐Wen Lai, Tinghai Ou, Wei‐Chyung Wang, Haolin Luo, Xiaoye Yang, Deliang Chen, Chang-Hoi Ho
article en
1 citations

Abstract

Abstract Wildfires in the Arctic are accelerating ecosystem damage and increasing global carbon emissions. Siberia, a major Arctic wildfire hotspot, is shaped by both local weather and distant climate influences. Here we use climate reanalysis data and numerical model experiments to show that summer wildfires in Siberia are strongly influenced by rainfall patterns over the Tibetan Plateau, one of the Northern Hemisphere’s largest summer heat sources. A dipole in Tibetan Plateau rainfall—wetter in the west, drier in the east—coincides with more fires in central Siberia and fewer in the east. This pattern alters high-altitude winds, shifting the jet stream northward and generating air flow changes that create favorable fire conditions across Siberia. Model experiments support a causal link. The resulting carbon dioxide emissions can match annual emissions from all Nordic countries. These findings highlight an overlooked driver of Arctic wildfires and improve our understanding of their role in the global carbon cycle.

Communications Earth & EnvironmentVol. 6(1)
Albany State University (US), Ewha Womans University (KR), Sun Yat-sen University (CN), Nanjing University of Information Science and Technology (CN), Chengdu University of Information Technology (CN), University at Albany, State University of New York (US), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN), Chalmers University of Technology (SE), University of Gothenburg (SE), Tsinghua University (CN)
Swedish Foundation for International Cooperation in Research and Higher Education, Korea Meteorological Administration, Tsinghua University, Vetenskapsrådet, Göteborgs Universitet, HORIZON EUROPE Framework Programme, National Key Research and Development Program of China
Openalex Percentile: Top 22%
Fire effects on ecosystems
1.11
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