Climate and wildfires in the North American boreal forest
The area burned in the North American boreal forest is controlled by the frequency of mid-tropospheric blocking highs that cause rapid fuel drying. Climate controls the area burned through changing the dynamics of large-scale teleconnection patterns (Pacific Decadal Oscillation/El Niño Southern Osci...
Published in: | Philosophical Transactions of the Royal Society B: Biological Sciences |
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ftpubmed:oai:pubmedcentral.nih.gov:2606782 2023-05-15T15:08:06+02:00 Climate and wildfires in the North American boreal forest Macias Fauria, Marc Johnson, E.A 2007-11-15 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2606782 http://www.ncbi.nlm.nih.gov/pubmed/18006414 https://doi.org/10.1098/rstb.2007.2202 en eng The Royal Society http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2606782 http://www.ncbi.nlm.nih.gov/pubmed/18006414 http://dx.doi.org/10.1098/rstb.2007.2202 © 2007 The Royal Society Research Article Text 2007 ftpubmed https://doi.org/10.1098/rstb.2007.2202 2013-09-02T09:00:49Z The area burned in the North American boreal forest is controlled by the frequency of mid-tropospheric blocking highs that cause rapid fuel drying. Climate controls the area burned through changing the dynamics of large-scale teleconnection patterns (Pacific Decadal Oscillation/El Niño Southern Oscillation and Arctic Oscillation, PDO/ENSO and AO) that control the frequency of blocking highs over the continent at different time scales. Changes in these teleconnections may be caused by the current global warming. Thus, an increase in temperature alone need not be associated with an increase in area burned in the North American boreal forest. Since the end of the Little Ice Age, the climate has been unusually moist and variable: large fire years have occurred in unusual years, fire frequency has decreased and fire–climate relationships have occurred at interannual to decadal time scales. Prolonged and severe droughts were common in the past and were partly associated with changes in the PDO/ENSO system. Under these conditions, large fire years become common, fire frequency increases and fire–climate relationships occur at decadal to centennial time scales. A suggested return to the drier climate regimes of the past would imply major changes in the temporal dynamics of fire–climate relationships and in area burned, a reduction in the mean age of the forest, and changes in species composition of the North American boreal forest. Text Arctic Global warming PubMed Central (PMC) Arctic Pacific Philosophical Transactions of the Royal Society B: Biological Sciences 363 1501 2315 2327 |
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Research Article |
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Research Article Macias Fauria, Marc Johnson, E.A Climate and wildfires in the North American boreal forest |
topic_facet |
Research Article |
description |
The area burned in the North American boreal forest is controlled by the frequency of mid-tropospheric blocking highs that cause rapid fuel drying. Climate controls the area burned through changing the dynamics of large-scale teleconnection patterns (Pacific Decadal Oscillation/El Niño Southern Oscillation and Arctic Oscillation, PDO/ENSO and AO) that control the frequency of blocking highs over the continent at different time scales. Changes in these teleconnections may be caused by the current global warming. Thus, an increase in temperature alone need not be associated with an increase in area burned in the North American boreal forest. Since the end of the Little Ice Age, the climate has been unusually moist and variable: large fire years have occurred in unusual years, fire frequency has decreased and fire–climate relationships have occurred at interannual to decadal time scales. Prolonged and severe droughts were common in the past and were partly associated with changes in the PDO/ENSO system. Under these conditions, large fire years become common, fire frequency increases and fire–climate relationships occur at decadal to centennial time scales. A suggested return to the drier climate regimes of the past would imply major changes in the temporal dynamics of fire–climate relationships and in area burned, a reduction in the mean age of the forest, and changes in species composition of the North American boreal forest. |
format |
Text |
author |
Macias Fauria, Marc Johnson, E.A |
author_facet |
Macias Fauria, Marc Johnson, E.A |
author_sort |
Macias Fauria, Marc |
title |
Climate and wildfires in the North American boreal forest |
title_short |
Climate and wildfires in the North American boreal forest |
title_full |
Climate and wildfires in the North American boreal forest |
title_fullStr |
Climate and wildfires in the North American boreal forest |
title_full_unstemmed |
Climate and wildfires in the North American boreal forest |
title_sort |
climate and wildfires in the north american boreal forest |
publisher |
The Royal Society |
publishDate |
2007 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2606782 http://www.ncbi.nlm.nih.gov/pubmed/18006414 https://doi.org/10.1098/rstb.2007.2202 |
geographic |
Arctic Pacific |
geographic_facet |
Arctic Pacific |
genre |
Arctic Global warming |
genre_facet |
Arctic Global warming |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2606782 http://www.ncbi.nlm.nih.gov/pubmed/18006414 http://dx.doi.org/10.1098/rstb.2007.2202 |
op_rights |
© 2007 The Royal Society |
op_doi |
https://doi.org/10.1098/rstb.2007.2202 |
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Philosophical Transactions of the Royal Society B: Biological Sciences |
container_volume |
363 |
container_issue |
1501 |
container_start_page |
2315 |
op_container_end_page |
2327 |
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1766339525832867840 |