Recent increases in eastern Siberian wildfires are investigated, attributing 79% of the increase in summer vapor pressure deficit (VPD) to background eastern Siberian Arctic warming (BAW) related to summer Russian Arctic sea-ice decline. The remaining 21% is linked to internal atmospheric variability from changes in Siberian blocking events. These changes in blocking events, influenced by BAW, result in more persistent, widespread, and intense high-latitude warming and VPD, thus contributing to increased wildfires.
Publisher
Nature Communications
Published On
Jun 26, 2024
Authors
Binhe Luo, Dehai Luo, Aiguo Dai, Cunde Xiao, Ian Simmonds, Edward Hanna, James Overland, Jiaqi Shi, Xiaodan Chen, Yao Yao, Wansuo Duan, Yimin Liu, Qiang Zhang, Xiyan Xu, Yina Diao, Zhina Jiang, Tingting Gong
Tags
wildfires
eastern Siberia
vapor pressure deficit
Arctic warming
climate change
atmospheric variability
sea-ice decline
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