|Title||Investigations of effects of forest fires on the ground thermal regime and permafrost, northwestern Canada|
|Author||Smith, S L; Bonnaventure, P|
|Source||11th International Conference on Permafrost, book of abstracts; by Günther, F (ed.); Morgenstern, A (ed.); 2016 p. 489-490|
|Links||Online - En ligne (PDF, 345 MB)|
|Alt Series||Earth Sciences Sector, Contribution Series 20150405|
|Publisher||Bibliothek Wissenschaftspark Albert Einstein (Potsdam, Germany)|
|Meeting||XI International conference on permafrost; Potsdam,; DE; June 20-24, 2016|
|Province||Alberta; Northwest Territories|
|NTS||84M/11; 84M/12; 96C/07; 96C/08|
|Area||Norman Wells Pipeline|
|Lat/Long WENS||-120.0000 -119.0000 60.0000 59.5000|
|Lat/Long WENS||-125.0000 -124.0000 64.5000 64.2500|
|Subjects||surficial geology/geomorphology; Nature and Environment; permafrost; boreholes; thermal regimes; ground temperatures; Quaternary|
Geoscience, Land-based Infrastructure|
Wildfires are a common occurrence in the boreal forest of northwestern Canada and can have important impacts on the permafrost environments through their influence on the ground thermal
regime. Increases in ground surface temperature due to microclimatic changes associated with organic layer removal or the loss of the coniferous tree cover, can result in increased thaw penetration, permafrost degradation and ground instability where
soils are ice-rich. Understanding the long-term effects of environmental disturbance such as fire on permafrost environments is important for assessments of ecosystem change and for planning infrastructure in the context of a changing climate. The
Geological Survey of Canada has maintained a number of field sites in the Mackenzie transportation/transmission corridor of the Northwest Territories and northern Alberta that have facilitated the characterization of thermal effects of fires on
permafrost terrain up to two decades following initial fire events for sites underlain by warm permafrost in both mineral soils and peatlands.
Study Sites and Methods
The study sites are adjacent to the Norman Wells to Zama pipeline
right-of-way which extends from the central Mackenzie Valley NWT to northern Alberta. This paper focusses on two sites. The first study site is a north facing slope located at kilometre post (KP) 182 (64.3°N, 124.5° W). The site is underlain by
fine-grained soils (silt and clay). Permafrost is generally warm in this area with mean annual ground temperatures above -1°C and underlain by ice-rich soils. The site was burned in 1994 but prior to the event the site was covered by a white spruce
and white birch forest. Burning was more severe at the top of the slope with complete loss of the forest canopy and removal of the organic layer. Five instrumented boreholes, up to 1.9 m deep, were established at the site in 1995 to measure ground
temperatures. Four of these were on the burnt area of the slope at the slope bottom (KP182B), mid-slope (KP182M), slope crest (KP182C) and top of the slope (KP182T). One borehole was also established in an unburnt area (KP182UB). Instrumentation was
also installed to measure air temperature and near surface temperature (3-5 cm depth). A more detailed description of the site and instrumentation is provided in Smith et al. (2015). The second study site is located on a peat plateau at KP783
(59.7°N 119.5°W) in northern Alberta. Two boreholes (20 m deep) were instrumented in 1984 to measure ground temperatures and instrumentation to measure air and ground surface temperature was installed in 1999. The forest cover at the site originally
consisted of stunted black spruce and the site was underlain by thick (7 m) ice-rich frozen peat. Permafrost was 10 to 14 m thick and was at temperatures near 0°C (-0.1 to -0.2°C). The site was severely burned in summer 2004 with burning of
vegetation and the peat surface. The instrumentation at the site allowed a comparison of thermal conditions before and after the fire. Earlier analysis of ground temperature data and additional information about the site can be found in Smith et al.
Results and Discussion
The near surface ground temperature data collected about one year following the 1994 fire at KP182 indicates that before the fire, surface temperatures were below 0°C at the site. Following the fire, surface
temperatures rose above 0°C (Figure 1) at the 4 burned sites with the highest temperatures found at the more severely burned sites in the upper part of the slope (KP182T, KP182C). The annual mean surface temperatures at burned sites were generally
1-2°C warmer than at the unburnt site (KP182UB). At KP783 annual mean surface temperatures following the 2004 fire were generally higher than those recorded prior to the fire (Figure 1). Decreases in surface temperature about 5 years after the fire
at both KP182 and KP 783 were also observed which are assumed to be associated with regrowth of vegetation. At KP182, shallow ground temperatures increased at all burned sites while the change in ground temperature at the unburnt site was relatively
small. The ground warming at burned sites was accompanied by an increase in active layer thickness (determined from shallow temperature measurements) and in the upper portion of the slope where burning was more severe, thaw progressed to depths below
1.5 m shortly after the fire. At the top of the slope, permafrost is likely not sustainable as the ratio between frozen and unfrozen thermal conductivity in the upper portion of the soil is not sufficient to provide the required thermal offset (Smith
et al. 2015). Ground temperature data from other recovering burn sites in mineral soils in the central Mackenzie Valley also indicate that permafrost is degrading. Although burning was severe at the KP783 site, warm permafrost still persists a
decade after the fire with some increase in thaw depth following the fire which has been accompanied by surface settlement. The insulating effect of the peat likely reduces the impact of surface warming on the underlying permafrost. The large
seasonal difference in thermal conductivity of the peat is able to maintain the thermal offset required to sustain permafrost at the site. There is also a high latent heat requirement for thawing the ice-rich peat.
Summary and Conclusion
magnitude of the impact of forest fires on warm permafrost is associated with the severity of the fire and also the properties of the subsurface materials. Where severe burning occurred in areas underlain by mineral soils, degradation of permafrost
is likely occurring. In contrast, at a severely burned peatland site, warm permafrost persists a decade after the fire with the thick peat reducing the impact of the higher surface temperatures. The loss of the surface buffer layer due to burning
will also make the ground thermal regime additionally sensitive to increases in air temperature associated with a warming climate. Warming and thawing of ice-rich permafrost following fires can result in surface settlement and ground instability and
these impacts need to be considered in planning and maintenance of infrastructure in a changing climate.
Field data collection has been supported by Natural Resources Canada and several other sources over the years including
the Program for Energy Research and Development and the Northern Oil and Gas Science Research Initiative. The important contribution of our late colleague Dan Riseborough to the data analysis is also gratefully acknowledged.
Smith, S.L., Burgess, M.M. and Riseborough, D.W., 2008. Ground temperature and thaw settlement in frozen peatlands along the Norman Wells pipeline corridor, NWT Canada: 22 years of monitoring. In: D.L. Kane and K.M. Hinkel (Editors), Ninth
International Conference on Permafrost. Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks Alaska, pp. 1665-1670.
Smith, S.L., Riseborough, D.W. and Bonnaventure, P.P., 2015. Eighteen year record of forest fire effects
on ground thermal regimes and permafrost in the central Mackenzie Valley, NWT, Canada. Permafrost and Periglacial Processes. DOI: 10.1002/ppp.1849
|Summary||(Plain Language Summary, not published)|
This presentation describes the impact of forest fires on the permafrost environments. Results are presented from two sites adjacent to a pipeline
right-of-way: (1) a warm permafrost slope in the central Mackenzie Valley burned in 1994; (2) a peatland in northern Alberta burned in 2004. The loss of vegetation and alterations in surface associated with the fire resulted in warming of the ground
and increases in summer thaw depth. The magnitude of the impact of forest fires on warm permafrost is associated with the severity of the fire and also the properties of the subsurface materials. Where burning was more severe on the slope,
degradation of permafrost is occurring. Although burning was severe at the peatland site, warm permafrost still persists likely due to the insulation provided by the thick peat. These changes in permafrost conditions resulting from natural
disturbances can have implications for landscape stability and infrastructure integrity in adjacent transportation/transmission corridors.