Free Standard AU & NZ Shipping For All Book Orders Over $80!
Register      Login
International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

Mapping smouldering fire potential in boreal peatlands and assessing interactions with the wildland–human interface in Alberta, Canada

S. L. Wilkinson https://orcid.org/0000-0002-4043-6277 A D , A. K. Furukawa https://orcid.org/0000-0001-6437-3314 A , B. M. Wotton B C and J. M. Waddington A
+ Author Affiliations
- Author Affiliations

A School of Earth, Environment and Society, McMaster University, 1280 Main Street West, Hamilton, ON, Canada. L8S 4L8.

B School of Forestry, Daniels Faculty, University of Toronto, 1 Spadina Crescent, Toronto, ON, Canada, M5S 2J5.

C Canadian Forestry Service, Northern Forestry Centre, 1219 Queen St E, Sault Ste. Marie, ON P6A 2E5.

D Corresponding author. Email: wilkisl@mcmaster.ca

International Journal of Wildland Fire 30(7) 552-563 https://doi.org/10.1071/WF21001
Submitted: 6 January 2021  Accepted: 16 April 2021   Published: 18 May 2021

Abstract

Treed peatlands exhibit both crown and smouldering fire potential; however, neither are included in Canadian wildfire management models and, as such, they are not formally represented in management decision-making. The lack of smouldering fire risk assessment is a critical research gap as these fires can represent heavy resource draws and are predominant sources of smoke, air pollutants and atmospheric carbon. Here, for the first time, we combine existing knowledge of the controls on smouldering peat fire with expert opinion-based weightings through a multi-criteria decision analysis, to map the smouldering fire potential (i.e. hazard) of treed peatlands in the Boreal Plains, Alberta, Canada. We find that smouldering potential varies considerably between treed peatlands and that areas of sparser peatland coverage may contain high smouldering-potential peatlands. Further, we find that treed peatlands are a common feature in the wildland–human interface and that proportionally, the area of high smouldering potential is greater closer to roads compared with farther away. Our approach enables a quantitative measure of smouldering fire potential and evidences the need to incorporate peatland–wildfire interactions into wildfire management operations. We suggest that similar frameworks could be used in other peatland dominated regions as part of smouldering fire risk assessments.

Keywords: wildfire management, organic soil, black spruce, wildland fire, wildland–society interface, wildland–urban interface, peat burn severity, carbon.


References

Alberta Agriculture and Forestry (2020) Historical Wildfire Perimeter Data (1931–2019). Available at https://wildfire.alberta.ca/resources/historical-data/spatial-wildfire-data.aspx

Alberta Environment and Parks (2017) Alberta Provincial Digital Elevation Model. Available at https://www.altalis.com/ [Verified 4 May 2021]

Alberta Environment and Parks (2018) Access and Facility Roads. Available at https://www.altalis.com/ [Verified 4 May 2021]

Amiro BD, Stocks BJ, Alexander ME, Flannigan MD, Wotton BM (2001) Fire, climate change, carbon and fuel management in the Canadian boreal forest. International Journal of Wildland Fire 10, 405–413.
Fire, climate change, carbon and fuel management in the Canadian boreal forest.Crossref | GoogleScholarGoogle Scholar |

Bayley SE, Wong AS, Thompson JE (2013) Effects of agricultural encroachment and drought on wetlands and shallow lakes in the boreal transition zone of Canada. Wetlands 33, 17–28.
Effects of agricultural encroachment and drought on wetlands and shallow lakes in the boreal transition zone of Canada.Crossref | GoogleScholarGoogle Scholar |

Benscoter BW, Vitt DH (2008) Spatial patterns and temporal trajectories of the bog ground layer along a post-fire chronosequence. Ecosystems 11, 1054–1064.
Spatial patterns and temporal trajectories of the bog ground layer along a post-fire chronosequence.Crossref | GoogleScholarGoogle Scholar |

Benscoter BW, Wieder RK (2003) Variability in organic matter lost by combustion in a boreal bog during the 2001 Chisholm fire. Canadian Journal of Forest Research 33, 2509–2513.
Variability in organic matter lost by combustion in a boreal bog during the 2001 Chisholm fire.Crossref | GoogleScholarGoogle Scholar |

Bisbee KE, Gower ST, Norman JM, Nordheim EV (2001) Environmental controls on ground cover species composition and productivity in a boreal black spruce forest. Oecologia 129, 261–270.
Environmental controls on ground cover species composition and productivity in a boreal black spruce forest.Crossref | GoogleScholarGoogle Scholar | 28547605PubMed |

Cascio WE (2018) Wildland fire smoke and human health. The Science of the Total Environment 624, 586–595.
Wildland fire smoke and human health.Crossref | GoogleScholarGoogle Scholar | 29272827PubMed |

Cumming SG (2001) Forest type and wildfire in the Alberta boreal mixedwood: what do fires burn? Ecological Applications 11, 97–110.
Forest type and wildfire in the Alberta boreal mixedwood: what do fires burn?Crossref | GoogleScholarGoogle Scholar |

Deane PJ, Wilkinson SL, Moore PA, Waddington JM (2020) Seismic lines in treed boreal peatlands as analogs for wildfire fuel modification treatments. Fire 3, 21–30.
Seismic lines in treed boreal peatlands as analogs for wildfire fuel modification treatments.Crossref | GoogleScholarGoogle Scholar |

Devito KJ, Creed I, Gan T, Mendoza CA, Petrone RM, Silins U, Smerdon B (2005) A framework for broad‐scale classification of hydrologic response units on the Boreal Plain: is topography the last thing to consider? Hydrological Processes 19, 1705–1714.
A framework for broad‐scale classification of hydrologic response units on the Boreal Plain: is topography the last thing to consider?Crossref | GoogleScholarGoogle Scholar |

ESRI Inc. (2019) ArcMap (Version 10.5.1). Available at https://desktop.arcgis.com/en/arcmap/ [Verified 10 December 2020]

ESRI Inc (2020) ArcGIS Pro (Version 2.6). Available at https://www.esri.com/en-us/arcgis/products/arcgis-pro/ [Verified 16 March 2020]

Fenton MM, Waters EJ, Pawley SM, Atkinson N, Utting DJ, Mckay K (2013) Surficial geology of Alberta. AER/AGS Map 601, scale 1:1 000 000. Alberta Energy Regulator. Available at https://ags.aer.ca/publication/dig-2013-0002 [Verified 1 October 2020]

Ferone JM, Devito KJ (2004) Shallow groundwater–surface water interactions in pond–peatland complexes along a Boreal Plains topographic gradient. Journal of Hydrology 292, 75–95.
Shallow groundwater–surface water interactions in pond–peatland complexes along a Boreal Plains topographic gradient.Crossref | GoogleScholarGoogle Scholar |

Flannigan MD, Krawchuk MA, de Groot WJ, Wotton BM, Gowman LM (2009a) Implications of changing climate for global wildland fire. International Journal of Wildland Fire 18, 483–507.
Implications of changing climate for global wildland fire.Crossref | GoogleScholarGoogle Scholar |

Flannigan MD, Stocks B, Turetsky M, Wotton BM (2009b) Impacts of climate change on fire activity and fire management in the circumboreal forest. Global Change Biology 15, 549–560.
Impacts of climate change on fire activity and fire management in the circumboreal forest.Crossref | GoogleScholarGoogle Scholar |

Flannigan MD, Cantin AS, De Groot WJ, Wotton BM, Newbery A, Gowman LM (2013) Global wildland fire season severity in the 21st century. Forest Ecology and Management 294, 54–61.
Global wildland fire season severity in the 21st century.Crossref | GoogleScholarGoogle Scholar |

Flat Top Complex Wildfire Review Committee (2012) Flat Top Complex. (Sustainable Resource Development; Alberta, Canada). Available at https://wildfire.alberta.ca/resources/reviews/documents/FlatTopComplex-WildfireReviewCommittee-A-May18–2012.pdf [Verified 30 November 2020]

Gralewicz NJ, Nelson TA, Wulder MA (2012) Spatial and temporal patterns of wildfire ignitions in Canada from 1980 to 2006. International Journal of Wildland Fire 21, 230–242.
Spatial and temporal patterns of wildfire ignitions in Canada from 1980 to 2006.Crossref | GoogleScholarGoogle Scholar |

Greene R, Devillers R, Luther JE, Eddy BG (2011) GIS‐based multiple‐criteria decision analysis. Geography Compass 5, 412–432.
GIS‐based multiple‐criteria decision analysis.Crossref | GoogleScholarGoogle Scholar |

Greifswald Mire Centre (GMC) (2018) Global Peatland Database. Available at https://greifswaldmoor.de/global-peatland-database-en.html. [Verified 20 March 2021]

Hanes CC, Wang X, Jain P, Parisien MA, Little JM, Flannigan MD (2019) Fire-regime changes in Canada over the last half century. Canadian Journal of Forest Research 49, 256–269.
Fire-regime changes in Canada over the last half century.Crossref | GoogleScholarGoogle Scholar |

Helbig M, Waddington JM, Alekseychik P, Amiro BD, Aurela M, Barr AG, Black TA, Blanken PD, Carey SK, Chen J, Chi J (2020) Increasing contribution of peatlands to boreal evapotranspiration in a warming climate. Nature Climate Change 10, 555–560.
Increasing contribution of peatlands to boreal evapotranspiration in a warming climate.Crossref | GoogleScholarGoogle Scholar |

Hirsch KG, Fuglem P (Eds) (2006) ‘Canadian Wildland Fire Strategy: Background Syntheses, Analyses, and Perspectives.’ (Natural Resources Canada, Canadian Forest Service: Edmonton, Alberta.)

Hokanson KJ, Lukenbach MC, Devito KJ, Kettridge N, Petrone RM, Waddington JM (2016) Groundwater connectivity controls peat burn severity in the boreal plains. Ecohydrology 9, 574–584.
Groundwater connectivity controls peat burn severity in the boreal plains.Crossref | GoogleScholarGoogle Scholar |

Hokanson KJ, Mendoza CA, Devito KJ (2019) Interactions between regional climate, surficial geology, and topography: characterizing shallow groundwater systems in subhumid, low‐relief landscapes. Water Resources Research 55, 284–297.
Interactions between regional climate, surficial geology, and topography: characterizing shallow groundwater systems in subhumid, low‐relief landscapes.Crossref | GoogleScholarGoogle Scholar |

Hokanson KJ, Peterson ES, Devito KJ, Mendoza CA (2020) Forestland-peatland hydrologic connectivity in water-limited environments: hydraulic gradients often oppose topography. Environmental Research Letters 15, 034021
Forestland-peatland hydrologic connectivity in water-limited environments: hydraulic gradients often oppose topography.Crossref | GoogleScholarGoogle Scholar |

Hvenegaard S, Schroeder D, Thompson D (2016) Fire behaviour in black spruce forest fuels following mulch fuel treatments: a case study at Red Earth Creek, Alberta. Technical Report 42. FPInnovations. (Edmonton, Alberta)

Ingram RC, Moore PA, Wilkinson SL, Petrone RM, Waddington JM (2019) Post‐fire soil carbon accumulation does not recover boreal peatland combustion loss in some hydrogeological settings. Journal of Geophysical Research. Biogeosciences 124, 775–788.
Post‐fire soil carbon accumulation does not recover boreal peatland combustion loss in some hydrogeological settings.Crossref | GoogleScholarGoogle Scholar |

Jankowski P (1995) Integrating geographical information systems and multiple criteria decision‐making methods. International Journal of Geographical Information Systems 9, 251–273.
Integrating geographical information systems and multiple criteria decision‐making methods.Crossref | GoogleScholarGoogle Scholar |

Johnson EA, Miyanishi K, O’brien N (1999) Long-term reconstruction of the fire season in the mixedwood boreal forest of Western Canada. Canadian Journal of Botany 77, 1185–1188.
Long-term reconstruction of the fire season in the mixedwood boreal forest of Western Canada.Crossref | GoogleScholarGoogle Scholar |

Johnston DC, Turetsky MR, Benscoter BW, Wotton BM (2015) Fuel load, structure, and potential fire behaviour in black spruce bogs. Canadian Journal of Forest Research 45, 888–899.
Fuel load, structure, and potential fire behaviour in black spruce bogs.Crossref | GoogleScholarGoogle Scholar |

Johnston LM, Flannigan MD (2018) Mapping Canadian wildland fire interface areas. International Journal of Wildland Fire 27, 1–14.
Mapping Canadian wildland fire interface areas.Crossref | GoogleScholarGoogle Scholar |

Kiker GA, Bridges TS, Varghese A, Seager TP, Linkov I (2005) Application of multicriteria decision analysis in environmental decision making. Integrated Environmental Assessment and Management 1, 95–108.
Application of multicriteria decision analysis in environmental decision making.Crossref | GoogleScholarGoogle Scholar | 16639891PubMed |

Krawchuk MA, Cumming SG, Flannigan MD (2009) Predicted changes in fire weather suggest increases in lightning fire initiation and future area burned in the mixedwood boreal forest. Climatic Change 92, 83–97.
Predicted changes in fire weather suggest increases in lightning fire initiation and future area burned in the mixedwood boreal forest.Crossref | GoogleScholarGoogle Scholar |

Malczewski J (2000) On the use of weighted linear combination method in GIS: common and best practice approaches. Transactions in GIS 4, 5–22.
On the use of weighted linear combination method in GIS: common and best practice approaches.Crossref | GoogleScholarGoogle Scholar |

Mayner KM, Moore PA, Wilkinson SL, Petrone RM, Waddington JM (2018) Delineating boreal plains bog margin ecotones across hydrogeological settings for wildfire risk management. Wetlands Ecology and Management 26, 1037–1046.
Delineating boreal plains bog margin ecotones across hydrogeological settings for wildfire risk management.Crossref | GoogleScholarGoogle Scholar |

National Wetlands Working Group (1997) ‘The Canadian Wetland Classification System (2nd edn).’ (Lands Conservation Branch, Canadian Wildlife Service, Environment Canada; Montreal, Quebec).

Natural Resources Canada (2019) CanVec. (EaSS GeoGratis Client Services, Natural Resources Canada, Canada Centre for Mapping and Earth Observation). Available at http://ftp.maps.canada.ca/pub/nrcan_rncan/vector/canvec/doc/ [Verified 15 October 2020]

Parisien MA, Miller C, Parks SA, DeLancey ER, Robinne FN, Flannigan MD (2016) The spatially varying influence of humans on fire probability in North America. Environmental Research Letters 11, 075005
The spatially varying influence of humans on fire probability in North America.Crossref | GoogleScholarGoogle Scholar |

Partners in Protection (2003) ‘FireSmart: Protecting Your Community from Wildfire, 2nd edn.’ (Maryhelen Vicars: Edmonton, AB, Canada).

Rein G, Cleaver N, Ashton C, Pironi P, Torero JL (2008) The severity of smouldering peat fires and damage to the forest soil. Catena 74, 304–309.
The severity of smouldering peat fires and damage to the forest soil.Crossref | GoogleScholarGoogle Scholar |

Robinne FN, Parisien MA, Flannigan MD (2016) Anthropogenic influence on wildfire activity in Alberta, Canada. International Journal of Wildland Fire 25, 1131–1143.
Anthropogenic influence on wildfire activity in Alberta, Canada.Crossref | GoogleScholarGoogle Scholar |

Saaty RW (1987) The analytic hierarchy process – what it is and how it is used. Mathematical Modelling 9, 161–176.
The analytic hierarchy process – what it is and how it is used.Crossref | GoogleScholarGoogle Scholar |

Saaty TL (1977) A scaling method for priorities in hierarchical structures. Journal of Mathematical Psychology 15, 234–281.
A scaling method for priorities in hierarchical structures.Crossref | GoogleScholarGoogle Scholar |

Saraswati S, Petrone RM, Rahman MM, McDermid GJ, Xu B, Strack M (2020) Hydrological effects of resource-access road crossings on boreal forested peatlands. Journal of Hydrology 584, 124748
Hydrological effects of resource-access road crossings on boreal forested peatlands.Crossref | GoogleScholarGoogle Scholar |

Schiks TJ, Wotton BM, Turetsky MR, Benscoter BW (2016) Variation in fuel structure of boreal fens. Canadian Journal of Forest Research 46, 683–695.
Variation in fuel structure of boreal fens.Crossref | GoogleScholarGoogle Scholar |

Smith KB, Smith CE, Forest SF, Richard AJ (2007) ‘A field guide to the wetlands of the boreal plains ecozone of Canada.’ (Ducks Unlimited Canada: Edmonton, Alberta.)

Stinson G, Kurz WA, Smyth CE, Neilson ET, Dymond CC, Metsaranta JM, Boisvenue C, Rampley GJ, Li Q, White TM, Blain D (2011) An inventory‐based analysis of Canada’s managed forest carbon dynamics, 1990 to 2008. Global Change Biology 17, 2227–2244.
An inventory‐based analysis of Canada’s managed forest carbon dynamics, 1990 to 2008.Crossref | GoogleScholarGoogle Scholar |

Strack M, Softa D, Bird M, Xu B (2018) Impact of winter roads on boreal peatland carbon exchange. Global Change Biology 24, e201–e212.
Impact of winter roads on boreal peatland carbon exchange.Crossref | GoogleScholarGoogle Scholar | 28755391PubMed |

Tarnocai C, Kettles IM, Lacelle B (2011) ‘Peatlands of Canada. Geological Survey of Canada.’ (Natural Resources Canada: Ottawa, ON). Available at10.4095/288786 [Verified on 20 March 2020].

Thompson DK, Wotton BM, Waddington JM (2015) Estimating the heat transfer to an organic soil surface during crown fire. International Journal of Wildland Fire 24, 120–129.
Estimating the heat transfer to an organic soil surface during crown fire.Crossref | GoogleScholarGoogle Scholar |

Thompson DK, Parisien MA, Morin J, Millard K, Larsen CP, Simpson BN (2017) Fuel accumulation in a high-frequency boreal wildfire regime: from wetland to upland. Canadian Journal of Forest Research 47, 957–964.
Fuel accumulation in a high-frequency boreal wildfire regime: from wetland to upland.Crossref | GoogleScholarGoogle Scholar |

Thompson DK, Simpson BN, Whitman E, Barber QE, Parisien MA (2019) Peatland hydrological dynamics as a driver of landscape connectivity and fire activity in the Boreal Plain of Canada. Forests 10, 534–540.
Peatland hydrological dynamics as a driver of landscape connectivity and fire activity in the Boreal Plain of Canada.Crossref | GoogleScholarGoogle Scholar |

Thompson DK, Schroeder D, Wilkinson SL, Barber Q, Baxter G, Cameron H, Hsieh R, Marshall G, Moore B, Refai R, Rodell C (2020) 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. Fire 3, 28–38.
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.Crossref | GoogleScholarGoogle Scholar |

Turetsky MR, Amiro BD, Bosch E, Bhatti JS (2004) Historical burn area in western Canadian peatlands and its relationship to fire weather indices. Global Biogeochemical Cycles 18,
Historical burn area in western Canadian peatlands and its relationship to fire weather indices.Crossref | GoogleScholarGoogle Scholar |

Wang X, Thompson DK, Marshall GA, Tymstra C, Carr R, Flannigan MD (2015) Increasing frequency of extreme fire weather in Canada with climate change. Climatic Change 130, 573–586.
Increasing frequency of extreme fire weather in Canada with climate change.Crossref | GoogleScholarGoogle Scholar |

Wilkinson SL, Moore PA, Flannigan MD, Wotton BM, Waddington JM (2018a) Did enhanced afforestation cause high severity peat burn in the Fort McMurray Horse River wildfire? Environmental Research Letters 13, 014018
Did enhanced afforestation cause high severity peat burn in the Fort McMurray Horse River wildfire?Crossref | GoogleScholarGoogle Scholar |

Wilkinson SL, Moore PA, Thompson DK, Wotton BM, Hvenegaard S, Schroeder D, Waddington JM (2018b) The effects of black spruce fuel management on surface fuel condition and peat burn severity in an experimental fire. Canadian Journal of Forest Research 48, 1433–1440.
The effects of black spruce fuel management on surface fuel condition and peat burn severity in an experimental fire.Crossref | GoogleScholarGoogle Scholar |

Wilkinson SL, Moore PA, Waddington JM (2019) Assessing drivers of cross-scale variability in peat smouldering combustion vulnerability in forested boreal peatlands. Frontiers in Forests and Global Change 2, 84–90.
Assessing drivers of cross-scale variability in peat smouldering combustion vulnerability in forested boreal peatlands.Crossref | GoogleScholarGoogle Scholar |

Wilkinson SL, Tekatch AM, Markle CE, Moore PA, Waddington JM (2020) Shallow peat is most vulnerable to high peat burn severity during wildfire. Environmental Research Letters 15, 104032
Shallow peat is most vulnerable to high peat burn severity during wildfire.Crossref | GoogleScholarGoogle Scholar |

Wotton BM, Flannigan MD, Marshall GA (2017) Potential climate change impacts on fire intensity and key wildfire suppression thresholds in Canada. Environmental Research Letters 12, 095003
Potential climate change impacts on fire intensity and key wildfire suppression thresholds in Canada.Crossref | GoogleScholarGoogle Scholar |