Climate forcing of regional fire years in the upper Great Lakes Region, USA
Colleen M. Sutheimer A H * , Jed Meunier B , Igor Drobyshev C D , Michael C. Stambaugh E , Sara C. Hotchkiss F , Eric Rebitzke G and Volker C. Radeloff AA SILVIS Lab, Department of Forest and Wildlife Ecology, University of Wisconsin–Madison, 1630 Linden Drive, Madison, WI 53706, USA.
B Forest Economics and Ecology Section, Division of Forestry, Wisconsin Department of Natural Resources, 2801 Progress Road, Madison, WI 53716, USA.
C Southern Swedish Forest Research Centre, Swedish University of Agricultural Sciences, P.O. Box 49, 230 53 Alnarp, Sweden.
D Institut de recherche sur les forêts, Université du Québec en Abitibi-Témiscamingue (UQAT), 445 boul. de l’Université, Rouyn-Noranda, QC J9X 5E4, Canada.
E Center for Tree-Ring Science, School of Natural Resources, University of Missouri, Columbia, MI 65211, USA.
F Department of Botany, University of Wisconsin–Madison, 430 Lincoln Drive, Madison, Wisconsin 53706, USA.
G Hiawatha and Ottawa National Forests, USDA Forest Service, 820 Rains Drive, Gladstone, MI 49837, USA.
H Present address: Applied Conservation Ecology Lab, Department of Renewable Resources, University of Alberta, 751 General Services Building, Edmonton, AB T6G 2H1, Canada.
International Journal of Wildland Fire 32(5) 796-813 https://doi.org/10.1071/WF22205
Submitted: 6 October 2022 Accepted: 11 February 2023 Published: 16 March 2023
© 2023 The Author(s) (or their employer(s)). Published by CSIRO Publishing on behalf of IAWF. This is an open access article distributed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License (CC BY-NC-ND)
Abstract
Background: Drivers of fire regimes vary among spatial scales, and fire history reconstructions are often limited to stand scales, making it difficult to partition effects of regional climate forcing versus individual site histories.
Aims: To evaluate regional-scale historical fire regimes over 350 years, we analysed an extensive fire-scar network, spanning 240 km across the upper Great Lakes Region in North America.
Methods: We estimated fire frequency, identified regionally widespread fire years (based on the fraction of fire-scarred tree samples, fire extent index (FEI), and synchronicity of fire years), and evaluated fire seasonality and climate–fire relationships.
Key results: Historically, fire frequency and seasonality were variable within and among Great Lakes’ ecoregions. Climate forcing at regional scales resulted in synchronised fires, primarily during the late growing season, which were ubiquitous across the upper Great Lakes Region. Regionally significant fire years included 1689, 1752, 1754, 1791, and 1891.
Conclusions: We found significant climate forcing of region-wide fire regimes in the upper Great Lakes Region.
Implications: Historically, reoccurring fires in the upper Great Lakes Region were instrumental for shaping and maintaining forest resilience. The climate conditions that helped promote widespread fire years historically may be consistent with anticipated climate–fire interactions due to climate change.
Keywords: climate–fire interactions, dendroecology, ecoregions, fire history, Lake Superior, Michigan, natural disturbance regimes, Pinus resinosa Ait., Upper Peninsula.
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