FireALT dataset: estimated active layer thickness for paired burned unburned sites measured from 2001-2023

As the northern high latitude permafrost zone experiences accelerated warming, permafrost has become vulnerable to widespread thaw. Simultaneously, wildfire activity across northern boreal forests and Arctic/subarctic tundra regions impacts permafrost stability through the combustion of insulating organic matter, vegetation, and post-fire changes in albedo. Despite the importance of wildfire-permafrost interactions, little research has been conducted to understand differences across ecosystem types. To address this knowledge gap, we solicited observations of active layer thickness from paired burned and unburned sites across the northern high-latitude permafrost region. We compiled 52,466 permafrost thaw depth observations from 18 contributors collected as part of individual field studies. As thaw depths were taken at various times throughout the season, we estimated end-of-season active layer thickness for each measurement using the square root of additional air thawing degree days between the day of measurement and the date of the end of the thawing season at each site. The FireALT dataset includes 47,952 estimations (27,747 burned, 20,205 unburned) with 32 attributes. There are 193 unique paired burned/unburned measures based on pair id (76), fire year (37 unique years), fire events (63 unique events), and time since fire spread across 12 ecozones that span Canada, Russia, and the United States. The data were collected between 2001 and 2023 and span fire events from 1900 to 2022. Time since fire ranges from zero to 114 years. The FireALT dataset addresses a key challenge: the ability to assess the impacts of wildfire on ALT when measurements are taken at various times throughout the thaw season depending on the time of field campaigns (typically June through August) by estimating ALT at the end of the season maximum.