2020 ESA Annual Meeting (August 3 - 6)

COS 171 Abstract - Modern area burned in a historical context in the Jemez Mountains, New Mexico

Ellis Q. Margolis1, Calvin A. Farris2, Craig D. Allen3, L.B. Johnson4, Donald A. Falk5, Thomas W. Swetnam6 and Christopher H. Guiterman6, (1)U.S. Geological Survey, New Mexico Landscapes Field Station, Santa Fe, NM, (2)National Park Service, (3)U.S. Geological Survey, New Mexico Landscapes Field Station, Los Alamos, NM, (4)Center for Water and the Environment, Natural Resources Research Institute, University of Minnesota-Duluth, Duluth, MN, (5)School of Natural Resources and the Environment, The University of Arizona, Tucson, AZ, (6)Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ
Background/Question/Methods

Fire was a keystone process in dry conifer forests of the West for millennia, but was excluded by human land use for over a century. Fire activity is currently increasing, driven in-part by a combination of increased fuels and increasing aridity. Are the recent “record” levels of area burned large in a historical context? The goal of our research was to reconstruct area burned at the landscape scale using the largest network of tree-ring fire scars for a mountain range in North America: The Jemez Mountains, New Mexico, with > 8,000 fire scars from > 1,300 trees, systematically sampled across > 250,000 ha of montane forest. Reconstructed area burned was compared with modern area burned derived from instrumental fire atlases.

Results/Conclusions

Modern “record” fire years (e.g., 2011 – including the 60,000 ha Las Conchas Fire) were not exceptionally large in terms of area burned in a 350-year context. Multiple historical fire years burned over twice the area of modern record fire years. Even with increasing modern burning, there is still a fire deficit in the Jemez Mountains. Importantly, recent fires have burned with uncharacteristically large patches of high severity fire (> 2,000 ha) that are not present in the historical fire record. These high-severity patches are likely converting centuries-old forests to non-forest. This contrast between area burned and severity emphasizes the need to restore frequent, low- to moderate-severity fire that historically burned with spatial extents unprecedented in the modern record.