Data and code for: Rocky Mountain subalpine forests now burning more than any time in recent millennia

The 2020 fire season punctuated a decades-long trend of increased fire activity across the western United States, nearly doubling the total area burned in the central Rocky Mountains since 1984. Understanding the causes and implications of such extreme fire seasons, particularly in subalpine forests that have historically burned infrequently, requires a long-term perspective not afforded by observational records. We place 21st century fire activity in subalpine forests in the context of climate and fire history spanning the past 2,000 y using a unique network of 20 paleofire records. Largely because of extensive burning in 2020, the 21st century fire rotation period is now 117 y, reflecting nearly double the average rate of burning over the past 2,000 y. More strikingly, contemporary rates of burning are now 22% higher than the maximum rate reconstructed over the past two millennia, during the early Medieval Climate Anomaly (MCA) (770 to 870 Common Era), when Northern Hemisphere temperatures were ∼0.3 °C above the 20th century average. The 2020 fire season thus exemplifies how extreme events are demarcating newly emerging fire regimes as climate warms. With 21st century temperatures now surpassing those during the MCA, fire activity in Rocky Mountain subalpine forests is exceeding the range of variability that shaped these ecosystems for millennia.

Methods
Datasets used in this study are all publicly available through the links described in the manuscript (i.e., MTBS, NIFC, GridMET, LANDFIRE) or data repositories associated with the original publications (i.e., http://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/fire-history for Calder et al. (2015), https://doi.org/10.5061/dryad.q2b8t for Higuera et al. (2014), https://doi.org/10.6084/m9.figshare.988687.v19 for Dunnette et al. (2014)). This Dryad repository includes all data used here, as well as all code use for analysis and to generate figures.