Table_3_Assessing the broadscale effects of wildfire under extreme drought conditions to boreal peatlands.xlsx

• Main Authors: Laura L. Bourgeau-Chavez (11652415), Jeremy A. Graham (14280794), Dorthea J. L. Vander Bilt (14280797), Michael J. Battaglia (11652418)
• Format: Dataset
• Language: unknown
• Published: 2022
• Subjects: Agroforestry; Forestry Biomass and Bioproducts; Forestry Fire Management; Forestry Management and Environment; Forestry Pests; Health and Diseases; peatland; wildfire; drought; boreal; fire severity; ecosystem vulnerability; soil organic layer; seasonality; Canada; Northwest Territories; taiga; Taiga plains; Taiga shield
• Online Access: https://doi.org/10.3389/ffgc.2022.965605.s008

Climate warming and changing fire regimes in the North American boreal zone have the capacity to alter the hydrology and ecology of the landscape with long term consequences to peatland ecosystems and their traditional role as carbon sinks. It is important to understand how peatlands are affected by wildfire in relation to both extent of burn and severity of burn to the organic soil (peat) layers where most of the C is stored. Peatlands cover more than 75% of the landscape in the southern Northwest Territories, Canada where extreme drought led to widespread wildfires in 2014–2015. To assess the wildfire effects across a 14.6 million ha study area including 136 wildfire events, we used an integration of field data collection, land cover mapping of peatland and upland ecotypes, Landsat-8-based mapping of burn severity to the soil organic layers, and MODIS-hotspot mapping of fire progression for season of burning. The intersection of these geospatial products allows for a broadscale assessment of wildfire effects across gradients of ecotype, ecoregions, seasons, and year of burn. Using a series of chi-squared goodness of fit tests, we found that peatlands are more susceptible to wildfire on the Taiga shield where they are smaller and hydrologically isolated by the rocky landscape. There burning affected proportionally larger peat areas with an evenness of burn severity to the organic soil layers which may lead to less spatial diversity in post-fire recovery, making the landscape less resilient to future fire. The most resilient peatlands are expected to be hydrologically well-connected to both ground water systems and larger peatland complexes such as those on the Taiga plains which exhibited large unburned and singed patches across the landscape, and greater variability in burn severity across seasons and ecotypes. Understanding the tipping point of drought conditions at which the landscape becomes connected, and peatlands are susceptible to wildfire with deeper burning of the organic soil layers is important for ...