Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals
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 (FRI) were found to be 112 ± 49 years (based on fire scars) and 106 ± 36 years (based on...
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ftpubmed:oai:pubmedcentral.nih.gov:5618805 2023-05-15T15:02:43+02:00 Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals Kharuk, Viacheslav I. Dvinskaya, Mariya L. Petrov, Ilya A. Im, Sergei T. Ranson, Kenneth J. 2016-04-07 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5618805/ http://www.ncbi.nlm.nih.gov/pubmed/28966554 https://doi.org/10.1007/s10113-016-0964-9 en eng http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5618805/ http://www.ncbi.nlm.nih.gov/pubmed/28966554 http://dx.doi.org/10.1007/s10113-016-0964-9 Article Text 2016 ftpubmed https://doi.org/10.1007/s10113-016-0964-9 2017-12-03T01:19:45Z 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 (FRI) were found to be 112 ± 49 years (based on fire scars) and 106 ± 36 years (based on fire scars and tree natality dates). FRI 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 FRI 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. Text Arctic Siberia PubMed Central (PMC) Arctic Regional Environmental Change 16 8 2389 2397 |
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Article Kharuk, Viacheslav I. Dvinskaya, Mariya L. Petrov, Ilya A. Im, Sergei T. Ranson, Kenneth J. Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals |
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Article |
description |
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 (FRI) were found to be 112 ± 49 years (based on fire scars) and 106 ± 36 years (based on fire scars and tree natality dates). FRI 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 FRI 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. |
format |
Text |
author |
Kharuk, Viacheslav I. Dvinskaya, Mariya L. Petrov, Ilya A. Im, Sergei T. Ranson, Kenneth J. |
author_facet |
Kharuk, Viacheslav I. Dvinskaya, Mariya L. Petrov, Ilya A. Im, Sergei T. Ranson, Kenneth J. |
author_sort |
Kharuk, Viacheslav I. |
title |
Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals |
title_short |
Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals |
title_full |
Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals |
title_fullStr |
Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals |
title_full_unstemmed |
Larch Forests of Middle Siberia: Long-Term Trends in Fire Return Intervals |
title_sort |
larch forests of middle siberia: long-term trends in fire return intervals |
publishDate |
2016 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5618805/ http://www.ncbi.nlm.nih.gov/pubmed/28966554 https://doi.org/10.1007/s10113-016-0964-9 |
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Arctic |
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Arctic |
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Arctic Siberia |
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Arctic Siberia |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5618805/ http://www.ncbi.nlm.nih.gov/pubmed/28966554 http://dx.doi.org/10.1007/s10113-016-0964-9 |
op_doi |
https://doi.org/10.1007/s10113-016-0964-9 |
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Regional Environmental Change |
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16 |
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