Drobyshev, Igor
- Southern Swedish Forest Research Centre, Swedish University of Agricultural Sciences
- Université du Québec en Abitibi-Témiscamingue (UQAT)
Research article2017Peer reviewedOpen access
Drobyshev, Igor; Bergeron, Yves; Girardin, Martin P.; Gauthier, Sylvie; Ols, Clementine; Ojal, John
The length of the fire cycle is a critical factor affecting the vegetation cover in boreal and temperate regions. However, its responses to climate change remain poorly understood. We reanalyzed data from earlier studies of forest age structures at the landscape level, in order to map the evolution of regional fire cycles across Eastern North American boreal and temperate forests, following the termination of the Little Ice Age (LIA). We demonstrated a well-defined spatial pattern of post-LIA changes in the length of fire cycles toward lower fire activity during the 1800s and 1900s. The western section of Eastern North America (west of 77 degrees W) experienced a decline in fire activity as early as the first half of the 1800s. By contrast, the eastern section showed these declines as late as the early 1900s. During a regionally fire-prone period of the 1910s-1920s, forests in the western section of Eastern boreal North America burned more than forests in the eastern section. The climate appeared to dominate over vegetation composition and human impacts in shaping the geographical pattern of the post-LIA change in fire activity. Changes in the atmospheric circulation patterns following the termination of the LIA, specifically changes in Arctic Oscillation and the strengthening of the Continental Polar Trough, were likely drivers of the regional fire dynamics.
forest fires; natural disturbances; dendrochronology; climate forcing; boreal biome; forest resilience
Journal of Geophysical Research: Biogeosciences
2017, Volume: 122, number: 10, pages: 2605-2616
Publisher: AMER GEOPHYSICAL UNION
SDG13 Climate action
Forest Science
DOI: https://doi.org/10.1002/2017JG003826
https://res.slu.se/id/publ/93229