Fuel accumulation in a high-frequency boreal wildfire regime: from wetland to upland
Although it is increasingly accepted that young (e.g., â ¤30 years) stands originating from wildfire are considerably less flammable than older stands in the boreal forest of North America, the role of fuel availability and structure in this phenomenon has not been thoroughly investigated. As a regi...
| Main Authors: | , , , , , |
|---|---|
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
NRC Research Press (a division of Canadian Science Publishing)
2017
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/1807/77660 http://www.nrcresearchpress.com/doi/abs/10.1139/cjfr-2016-0475 |
| Summary: | Although it is increasingly accepted that young (e.g., â ¤30 years) stands originating from wildfire are considerably less flammable than older stands in the boreal forest of North America, the role of fuel availability and structure in this phenomenon has not been thoroughly investigated. As a regional study in a high-frequency fire regime, detailed wildfire fuel loading and structure was measured in 66 sites including both wetlands and uplands in the Boreal Plains landscape of Wood Buffalo National Park, in northwestern Canada. Overall, a significant increase in total flammable biomass occurred in upland sites after 97 years but this increase was not consistently observed in wetlands, except where there was dense tree cover. Fuel accumulation was highly moderated by canopy fuels, as surface fuels were relatively constant across differing site types and time since fire, averaging 0.4 kg m-2. Significant but gradual canopy fuel accumulation was observed in moist conifer upland forests dominated by mature black spruce (Picea mariana) or white spruce (Picea glauca) over 100 years since fire. Outside of these mature moist conifer uplands, there was no difference in total fuel loading between other upland forest and across the gradient of treed to open wetlands. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. |
|---|