Articles | Volume 18, issue 1
https://doi.org/10.5194/nhess-18-157-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-18-157-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Jan 2018
Research article |
| 11 Jan 2018
| 11 Jan 2018
Hydrometeorological conditions preceding wildfire, and the subsequent burning of a fen watershed in Fort McMurray, Alberta, Canada
Department of Geography and Environmental Management, University of
Waterloo, Waterloo, Ontario, N2L 3G1, Canada
Dan K. Thompson
Natural Resources Canada, Canadian Forest Service, Northern Forestry
Centre, 5320 122 Street Northwest, Edmonton, Alberta, T6H 3S5, Canada
James H. Sherwood
Department of Geography and Environmental Management, University of
Waterloo, Waterloo, Ontario, N2L 3G1, Canada
Jonathan S. Price
Department of Geography and Environmental Management, University of
Waterloo, Waterloo, Ontario, N2L 3G1, Canada
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Cited
27 citations as recorded by crossref.
- Reviews and syntheses: Arctic fire regimes and emissions in the 21st century J. McCarty et al. 10.5194/bg-18-5053-2021
- Extent and effect of the 2019-20 Australian bushfires on upland peat swamps in the Blue Mountains, NSW K. Fryirs et al. 10.1071/WF20081
- Hydrogeologic setting overrides any influence of wildfire on pore water dissolved organic carbon concentration and quality at a boreal fen S. Davidson et al. 10.1002/eco.2141
- Using soil moisture information to better understand and predict wildfire danger: a review of recent developments and outstanding questions E. Krueger et al. 10.1071/WF22056
- Peatlands promote fire refugia in boreal forests of northern Alberta, Canada C. Kuntzemann et al. 10.1002/ecs2.4510
- Seasonally-decomposed Sentinel-1 backscatter time-series are useful indicators of peatland wildfire vulnerability K. Millard et al. 10.1016/j.rse.2022.113329
- Methane emissions from fens in Alberta’s boreal region: reference data for functional evaluation of restoration outcomes A. Bienida et al. 10.1007/s11273-020-09715-2
- Ecohydrological interactions in a boreal fen–swamp complex, Alberta, Canada M. Elmes et al. 10.1002/eco.2335
- Wetlands as integral parts of surface water–groundwater interactions in the Athabasca Oil Sands Area: Review and synthesis O. Volik et al. 10.1139/er-2023-0064
- Preceding Fall Drought Conditions and Overwinter Precipitation Effects on Spring Wildland Fire Activity in Canada C. Hanes et al. 10.3390/fire3020024
- Deeper burning in a boreal fen peatland 1‐year post‐wildfire accelerates recovery trajectory of carbon dioxide uptake M. Morison et al. 10.1002/eco.2277
- Changes to the hydrology of a boreal fen following the placement of an access road and below ground pipeline M. Elmes et al. 10.1016/j.ejrh.2022.101031
- Evaluating the hydrological response of a boreal fen following the removal of a temporary access road M. Elmes et al. 10.1016/j.jhydrol.2020.125928
- Seasonal ground ice impacts on spring ecohydrological conditions in a western boreal plains peatland B. Van Huizen et al. 10.1002/hyp.13626
- Organic matter decomposition at a constructed fen in the Athabasca Oil Sands region: Effect of substrate type and environmental conditions M. Coulas et al. 10.1016/j.scitotenv.2021.145708
- Water table dynamics in a constructed wetland, Fort McMurray, Alberta H. Spennato et al. 10.1002/hyp.13308
- Shortening fire return interval predisposes west‐central Canadian boreal peatlands to more rapid vegetation growth and transition to forest cover E. Jones et al. 10.1111/gcb.17185
- Microclimatic Effects of a Forest-to-Peatland Transition on Aerodynamic Resistance to Water Vapour Transfer in the Sub-humid Boreal Plains A. Green et al. 10.1007/s10546-020-00572-3
- A high-resolution reanalysis of global fire weather from 1979 to 2018 – overwintering the Drought Code M. McElhinny et al. 10.5194/essd-12-1823-2020
- Changes to the hydrophysical properties of upland and riparian soils in a burned fen watershed in the Athabasca Oil Sands Region, northern Alberta, Canada M. Elmes et al. 10.1016/j.catena.2019.104077
- PEAT‐CLSM: A Specific Treatment of Peatland Hydrology in the NASA Catchment Land Surface Model M. Bechtold et al. 10.1029/2018MS001574
- Recent Crown Thinning in a Boreal Black Spruce Forest Does Not Reduce Spread Rate nor Total Fuel Consumption: Results from an Experimental Crown Fire in Alberta, Canada D. Thompson et al. 10.3390/fire3030028
- Growing season evapotranspiration in boreal fens in the Athabasca Oil Sands Region: Variability and environmental controls O. Volik et al. 10.1002/hyp.14020
- Advances in wetland hydrology: the Canadian contribution over 75 years J. Price et al. 10.1080/07011784.2023.2269137
- Hydrologic function of a moderate-rich fen watershed in the Athabasca Oil Sands Region of the Western Boreal Plain, northern Alberta M. Elmes & J. Price 10.1016/j.jhydrol.2018.12.043
- Peatland Hydrological Dynamics as A Driver of Landscape Connectivity and Fire Activity in the Boreal Plain of Canada . Thompson et al. 10.3390/f10070534
- Wildfire overrides hydrological controls on boreal peatland methane emissions S. Davidson et al. 10.5194/bg-16-2651-2019
27 citations as recorded by crossref.
- Reviews and syntheses: Arctic fire regimes and emissions in the 21st century J. McCarty et al. 10.5194/bg-18-5053-2021
- Extent and effect of the 2019-20 Australian bushfires on upland peat swamps in the Blue Mountains, NSW K. Fryirs et al. 10.1071/WF20081
- Hydrogeologic setting overrides any influence of wildfire on pore water dissolved organic carbon concentration and quality at a boreal fen S. Davidson et al. 10.1002/eco.2141
- Using soil moisture information to better understand and predict wildfire danger: a review of recent developments and outstanding questions E. Krueger et al. 10.1071/WF22056
- Peatlands promote fire refugia in boreal forests of northern Alberta, Canada C. Kuntzemann et al. 10.1002/ecs2.4510
- Seasonally-decomposed Sentinel-1 backscatter time-series are useful indicators of peatland wildfire vulnerability K. Millard et al. 10.1016/j.rse.2022.113329
- Methane emissions from fens in Alberta’s boreal region: reference data for functional evaluation of restoration outcomes A. Bienida et al. 10.1007/s11273-020-09715-2
- Ecohydrological interactions in a boreal fen–swamp complex, Alberta, Canada M. Elmes et al. 10.1002/eco.2335
- Wetlands as integral parts of surface water–groundwater interactions in the Athabasca Oil Sands Area: Review and synthesis O. Volik et al. 10.1139/er-2023-0064
- Preceding Fall Drought Conditions and Overwinter Precipitation Effects on Spring Wildland Fire Activity in Canada C. Hanes et al. 10.3390/fire3020024
- Deeper burning in a boreal fen peatland 1‐year post‐wildfire accelerates recovery trajectory of carbon dioxide uptake M. Morison et al. 10.1002/eco.2277
- Changes to the hydrology of a boreal fen following the placement of an access road and below ground pipeline M. Elmes et al. 10.1016/j.ejrh.2022.101031
- Evaluating the hydrological response of a boreal fen following the removal of a temporary access road M. Elmes et al. 10.1016/j.jhydrol.2020.125928
- Seasonal ground ice impacts on spring ecohydrological conditions in a western boreal plains peatland B. Van Huizen et al. 10.1002/hyp.13626
- Organic matter decomposition at a constructed fen in the Athabasca Oil Sands region: Effect of substrate type and environmental conditions M. Coulas et al. 10.1016/j.scitotenv.2021.145708
- Water table dynamics in a constructed wetland, Fort McMurray, Alberta H. Spennato et al. 10.1002/hyp.13308
- Shortening fire return interval predisposes west‐central Canadian boreal peatlands to more rapid vegetation growth and transition to forest cover E. Jones et al. 10.1111/gcb.17185
- Microclimatic Effects of a Forest-to-Peatland Transition on Aerodynamic Resistance to Water Vapour Transfer in the Sub-humid Boreal Plains A. Green et al. 10.1007/s10546-020-00572-3
- A high-resolution reanalysis of global fire weather from 1979 to 2018 – overwintering the Drought Code M. McElhinny et al. 10.5194/essd-12-1823-2020
- Changes to the hydrophysical properties of upland and riparian soils in a burned fen watershed in the Athabasca Oil Sands Region, northern Alberta, Canada M. Elmes et al. 10.1016/j.catena.2019.104077
- PEAT‐CLSM: A Specific Treatment of Peatland Hydrology in the NASA Catchment Land Surface Model M. Bechtold et al. 10.1029/2018MS001574
- Recent Crown Thinning in a Boreal Black Spruce Forest Does Not Reduce Spread Rate nor Total Fuel Consumption: Results from an Experimental Crown Fire in Alberta, Canada D. Thompson et al. 10.3390/fire3030028
- Growing season evapotranspiration in boreal fens in the Athabasca Oil Sands Region: Variability and environmental controls O. Volik et al. 10.1002/hyp.14020
- Advances in wetland hydrology: the Canadian contribution over 75 years J. Price et al. 10.1080/07011784.2023.2269137
- Hydrologic function of a moderate-rich fen watershed in the Athabasca Oil Sands Region of the Western Boreal Plain, northern Alberta M. Elmes & J. Price 10.1016/j.jhydrol.2018.12.043
- Peatland Hydrological Dynamics as A Driver of Landscape Connectivity and Fire Activity in the Boreal Plain of Canada . Thompson et al. 10.3390/f10070534
- Wildfire overrides hydrological controls on boreal peatland methane emissions S. Davidson et al. 10.5194/bg-16-2651-2019
Discussed (final revised paper)
Latest update: 25 Apr 2024
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Short summary
The infrequent coinciding of several hydrometeorological conditions common to the Western Boreal Plain, including low autumn soil moisture, modest snowpack, lack of spring precipitation, and high spring air temperatures and winds, ultimately led to the widespread Horse river fire in May of 2016. Monitoring antecedent soil moisture would aid management strategies in producing of more accurate overwintered Drought Code calculations, providing early warning signals ahead of spring wildfire seasons.
The infrequent coinciding of several hydrometeorological conditions common to the Western Boreal...
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