Abstract
Fire history within the northern larch forests of Central Siberia was studied (65 + °N). Fires within this area are predominantly caused by lightning strikes rather than human activity. Mean fire return intervals (FRIs) were found to be 112 ± 49 years (based on firescars) and 106 ± 36 years (based on firescars and tree natality dates). FRIs were increased with latitude increase and observed to be about 80 years at 64°N, about 200 years near the Arctic Circle and about 300 years nearby the northern range limit of larch stands (~71° + N). Northward FRIs increase correlated with incoming solar radiation (r = −0.95). Post-Little Ice Age (LIA) warming (after 1850) caused approximately a doubling of fire events (in comparison with a similar period during LIA). The data obtained support a hypothesis of climate-induced fire frequency increase.
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Acknowledgments
This work was supported by Russian Scientific Foundation, Project #14-24-00112. Field measurements in 2012 were supported in part NASA’s Terrestrial Ecology Program.
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Editor: Xiangzheng Deng.
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Kharuk, V.I., Dvinskaya, M.L., Petrov, I.A. et al. Larch forests of Middle Siberia: long-term trends in fire return intervals. Reg Environ Change 16, 2389–2397 (2016). https://doi.org/10.1007/s10113-016-0964-9
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DOI: https://doi.org/10.1007/s10113-016-0964-9