A Synthesis of The Las Conchas Fire: How Does it Compare? Edward A. Martinez, Sara Brown, New Mexico Highlands University Las Vegas, NM; Richard McNeill, New Mexico Forest and Watershed Restoration Institute, Las Vegas, NM; Joseph Zebrowski, Elyssa Duran, Anita Lavadie, Lorraine Garcia, New Mexico Highlands University Las Vegas, NM Abstract—As wildfires have been increasing in extent and severity throughout the Southwest, so have the fire effects. Unlike many other big fires, the 156,593 acre Las Conchas fire of 2011 uncharacteristically burned more than 61,000 acres in a 24hr period on June 27 where over 50 percent of the total area burned at moderate and high severity. Its severity and extent provided the opportunity to develop better tools to understand and classify severity and its impact on ecological processes, natural resources, and human communities. As a means to contextualize the significance of the Las Conchas fire, the fire effects produced were compared to other recent, regionally relevant large fire events such as the Whitewater-Baldy (2012; 297,845 ac) and Silver fires (2013; 138,705 ac). Furthermore, the impacts to both natural resources and communities based on findings from our studies of the Las Conchas fire were synthesized. The Whitewater Baldy fire was two times larger than the Las Conchas fire and burned an area characterized by mixed-conifer, ponderosa pine, piñonjuniper and grasslands. The Silver fire was the largest fire of 2013 in the southwest. The burned area was characterized by mixed-conifer, ponderosa pine, piñon-juniper, and woodlands. Compared to the over 30 percent area burned at high severity of the Las Conchas, the area burned at high severity was 15 percent and 13 percent respectively for the Whitewater Baldy and Silver fires. Additionally both of these fires burned within their historical range of variability unlike the Las Conchas, where fire behavior was not characteristic of a frequent fire regime. The precipitation after the containment of the Las Conchas fire initiated major movement of soil especially in the high severity burned areas. This mass movement of soil resulted in low NO3-N and PO4 concentrations in soil collected from the high severity study site. Results indicated that NO3-N and PO4 concentrations in soil decreased with an increase in fire severity. Both of these relationships were opposite (nutrient concentrations increased with severity) for NO3-N and PO4 concentrations in surface water runoff collected from the control and the various burn severity sites. A significant negative correlation was determined for presence of vegetation with burn severity and bare ground, i.e., as bare ground and burn severity increased, presence of vegetation (biomass, diversity, and seed bank regeneration) decreased. Similarly, the impact of surface water runoff and debris flows entering the San Antonio Creek was evident in the decreased aquatic insect community structure when comparing pre- and post-fire aquatic insect data. The Las Conchas fire was out of the historic range of variability when we compare it to other large, regional fires. Based on climate change model projections of increased temperatures and increased drought conditions, as well as current forest management policies and fire suppression activities we can speculate that the Las Conchas fire is an excellent representation of future fires in the southwest. It is imperative that fire scientists and fire managers collaborate to develop policies that will allow for the creation of resilient forests that will minimize ecological and social costs of future fires similar to Las Conchas. Keywords: Synthesis, Las Conchas Fire, Nutrients, Vegetation, Soil, Impacts In: Keane, Robert E.; Jolly, Matt; Parsons, Russell; Riley, Karin. 2015. Proceedings of the large wildland fires conference; May 19-23, 2014; Missoula, MT. Proc. RMRS-P-73. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 345 p. USDA Forest Service Proceedings RMRS-P-73. 2015. The content of this paper reflects the views of the authors, who are responsible for the facts and accuracy of the information presented herein. 341