Fire has been a key factor in shaping the ecology of the Greater Yellowstone Ecosystem. Native plant species evolved adaptations so they survive and, in some cases, flourish after periodic fires. Fire influences ecosystem processes and patterns, such as nutrient cycling and plant community composition and structure. Fire regimes in the western United States changed with the arrival of European and American settlers, whose livestock removed grassy fuels that carried fires and whose roads fragmented the continuity of fire-carrying fuels. Most naturally occurring fires were suppressed to the extent possible. The National Park Service aims to restore fire’s role as a natural process in parks when and where this is feasible.
Lightning may ignite dozens of forest fires during a single summer, but most of them go out naturally after burning less than half an acre. Others torch isolated or small groups of trees, become smoldering ground fires, and eventually go out on their own. On rare occasions, wind-driven fires have burned through large areas of forest, as in 1988, when multiple fires crossed more than one million acres in Yellowstone and on surrounding federal lands despite massive efforts to extinguish them. Without frequent small and occasional large fires to create a mosaic of plant communities in different growth stages, biodiversity declines and leaf litter and deadfall accumulate much faster than they can return nutrients to the soil through decay.
Evidence of fires that burned before the park was established in 1872 can be found in soil profiles, charcoal found in lake sediments, landslides, and old-growth trees. Research shows large fires have been occurring in Yellowstone since forests became established following the last glacial retreat 14,000 years ago. Yellowstone’s fire season typically lasts from July to the end of September. The number and extent of fires that occur each year depend on climate and what efforts are made to suppress the fires, as well as weather conditions such as the number and timing of lightning storms and the amount and timing of precipitation.
Afternoon thunderstorms that release little precipitation occur frequently in the northern Rockies. Yellowstone receives thousands of lightning strikes in a typical summer, but most do not result in fires. A snag may smolder for several days and then burn out because fuels are too moist to sustain combustion or too sparse to permit the fire to spread. The park’s forests have few shrubs; understory fuels are predominantly young trees. The moisture content of both live and dead vegetation tends to drop as summer progresses, temperatures increase, and relative humidity decreases. Fuels have often dried out enough to ignite the first wildfire of the year by mid-July.
A forested area that has burned recently enough to contain only young stands of trees usually doesn’t have enough combustible fuel to carry a fire, except under extreme climate conditions. But as the years pass, trees that don’t survive the competition for light and other resources die and eventually fall over. On living trees, older branches die and fall off as they are shaded by new foliage growing above. As a stand grows older and taller, the canopy becomes more broken. This allows enough light to reach the forest floor for a shade-tolerant understory to be established. The accumulation of fuel on the forest floor and the continuity of fuels among the ground, understory, and canopy make older stands more vulnerable to fire. Some forests in Yellowstone may not have burned in at least 300 years and may be particularly prone to lightning ignition.
Nearly all of Yellowstone’s plant communities have burned at one time or another, but their varied characteristics cause fires to behave differently in them. To quickly assess a fire start and its potential to spread, park staff use different vegetation communities as indicators of fuel load, dominant vegetation, and time since the last fire or other disturbance.
The moisture content of dead and downed woody debris and the year’s weather trends are the main factors determining the severity of a given fire season. While fires can occur no matter the fuel moisture, many times conditions are too wet for fires to burn. In fact, 88% of all fires burn fewer than 10 acres. However, when 1,000-hour fuel moistures fall below 13%, fires can grow quickly. If extreme drought continues, all forest types and ages are more likely to burn.
To determine how much water is in the fuel, Yellowstone fire-monitoring staff weigh and oven dry fuel samples to determine the moisture content. In a normal fire season, 1,000-hour fuels within the park may average 14–18% fuel moisture. (Dead fuels are classified according to size, and how long they take to dry out when completely soaked; “1,000-hour fuel moisture” refers to the moisture in large fuels such as downed timber that would generally dry out within 42 days. Kiln-dried lumber is 12%.) )
Active fire behavior is generally not observed until 1,000-hour fuel moisture contents are less than 18%, and only minimal areas are burned until moisture levels drop to 13%. At that point, a fuel-moisture threshold is crossed; lightning strikes in forested areas at 13% fuel moisture quickly result in observable smoke columns and, if fuel and vegetation conditions are right, the fire spreads. Below 12%, younger and more varied forest types burn readily, especially when influenced by high winds. During extreme drought years, 1,000-hour fuel moistures may drop as low as 5%.
Depending on the forest type, fuel moisture, weather, and topography, fires can grow in size by isolated or frequent torching and spotting (transport of burning material by wind and convection currents), or by spreading from tree crown to crown. Fires in Yellowstone’s subalpine forests seldom spread significantly through ground fuels only. Like weather, terrain can be either an ally or adversary in suppressing unwanted fire. A few natural barriers such as the ridge from Electric Peak south to Mount. Holmes; Yellowstone Lake; and the Absaroka Mountains along the eastern boundary of the park are likely to prevent the spread of a low-to-moderate intensity fire, but fire may cross these features by spotting, covering a distance of two to three miles.
Fire managers may be able to predict a fire’s behavior when they know where the fire is burning (vegetation, topography) and the fuel-moisture content. However, predicting fire is much more difficult during extreme drought, such as was experienced in 1988 and in the early 2000s.
Ongoing research in Yellowstone is also showing that forests experiencing stand-replacing fires can affect fire behavior for up to 200 years. When a fire encounters a previously burned forest, its intensity and rate of spread decrease, except under extreme drought conditions. In some cases, the fire moves entirely around the burned area. Thus, fire managers have another tool for predicting fire behavior: They can compare maps of previous fires with a current fire’s location to predict its intensity and spread.
Frequency of Fire
Fire return intervals since European American settlement have ranged from 20–25 years for shrub and grasslands on the northern range to 300 years or more for lodgepole pine forests on the central plateau and subalpine whitebark pine stands. Fire scars on old Douglas-fir trees in the Lamar River valley indicate an average frequency of one fire every 25–60 years.
Until 1900, written records on fires in Yellowstone were sketchy, with generally only large fires reported. From 1900 through 1930, approximately 374 fires burned 11,670 acres. Since 1931, when fire statistics began to be kept more methodically, 1,644 fires have been lightning-caused and 740 were considered human-caused, including those caused by power lines.
The largest fire in the park’s written history prior to 1988 occurred when about 18,000 acres burned at Heart Lake in 1931. In 1989, fire ecologists William Romme and Don Despain suggested that without the fire suppression efforts that began in the 1880s, large fires might have occurred during the dry summers of 1949, 1953, 1960, or 1961. They believe that fire behavior in 1988, in terms of heat release, flame height, and rate of spread, was probably similar to that of the large fires that burned in Yellowstone in the early- to mid-1700s.
In 1988, 50 fires burned a mosaic covering about 800,000 acres in Yellowstone as a result of extremely warm, dry, and windy weather combined with an extensive forest cover of highly flammable fuels. Some of the largest fires originated outside the park, and a total of about 1.4 million acres burned in the Greater Yellowstone Ecosystem.
Some of the areas that burned in 1988 have burned again during the drought conditions of subsequent years, although unique conditions are required for such areas to reburn. Rare, extremely high wind events (greater than 20 mph), more than 80% ground cover of cured elk sedge (Carex spp.), or a continuous fuel bed of 1000-hour logs during very dry conditions, seem required for fires to again carry through areas burned in 1988. Fire behavior of previously burned areas is generally of a very high intensity—probably because of the high fuel load due to dead and fallen trees. Understanding the conditions necessary for recently burned areas (less than 50 years old) to reburn and modeling for the type of fire behavior seen in these areas is a challenge for fire managers in Yellowstone.
Frequently Asks Questions
Fires are a natural part of the Greater Yellowstone Ecosystem and vegetation has adapted to fire and in some cases may be dependent on it. Fire promotes habitat diversity by removing the forest overstory, allowing different plant communities to become established, and preventing trees from becoming established in grassland. Fire increases the rate that nutrients become available to plants by rapidly releasing them from wood and forest litter and by hastening the weathering of soil minerals. This is especially important in a cold and dry climate like Yellowstone’s, where decomposition rates are slower than in more hot and humid areas. Additionally, natural fires provide an opportunity for scientists to study the effects of fire on an ecosystem.
Burned trees and those that have died for other reasons still contribute to the ecosystem. For example, dead standing trees provide nesting cavities for many types of animals; fallen trees provide food and shelter for animals and nutrients for the soil. However, park managers will remove dead or burned trees that pose safety hazards along roads or in developed areas.
Barker, R. 2005. Scorched Earth: How the fires of Yellowstone changed America. Island Press/Washington.
Franke, M. A. 2000. Yellowstone in the afterglow: lessons from the fires. YCR-NR-2000-3. Mammoth, Wyo.: Yellowstone Center for Resources.
Greenlee, J., ed. The ecological implications of fire in Greater Yellowstone: proceedings of the second biennial conference on the Greater Yellowstone Ecosystem. Fairfield, Wash.: International Association of Wildland Fire.
Higuera, P.E. et. al. 2010. Linking tree-ring and sedimentcharcoal records to reconstruct fire occurrence and area burned in subalpine forests of Yellowstone National Park, USA. The Holocene.
International Association of Wildland Fire: https://www.iawfonline.org
National Interagency Fire Center: https://www.nifc.gov
National Park Service Fire and Aviation Management: https://www.nps.gov/subjects/fire/index.htm
Renkin, R.A. and D.G. Despain. 1992. Fuel moisture, forest type, and lightning-caused fire in Yellowstone National Park. Canadian Journal of Forestry Research 22(1):37–45.
Romme, W. H., and D. G. Despain. 1989. Historical perspective on the Yellowstone fires of 1988. Bioscience 39(10):696–699.
Simard, M. et. al. 2011. Do mountain pine beetle outbreaks change the probability of active crown fire in lodgepole pine forests? Ecological Monographs 81(1): 3–24.
Turner, M.G., et al. 2003. Surprises and Lessons from the 1988 Yellowstone Fires. Frontiers in Ecology and the Environment. 1(7):351–358.
Westerling, A. L. et. al. 2011. Continued warming could transform Greater Yellowstone fire regimes by mid- 21st century. Proceedings of the National Academy of Science.
Yellowstone in the Afterglow: Lessons from the Fires (5.7 MB PDF): An in-depth look at the 1988 fires.
Yellowstone Science. 2009. 9th Biennial Scientific Conference: The ‘88 Fires: Yellowstone and Beyond. 17(2).
General Information from Wildland Fire Organizations
NPS Data Store via IRMA (Integrated Resource Management Applications): Literature about wildland fire in Yellowstone and other national parks
National Significant Wildland Fire Potential Outlook: Monthly seasonal outlook by NIFC
US Forest Service Wildland Fire Assessment System: National fire danger forecast
PocketCards Data: Select "Northern Rockies" GACC, scroll to Yellowstone National Park; posted by Fire Danger Subcommittee Fire Environment Committee
Fire Terms Glossary: By the Fire Effects Information System
Last updated: October 22, 2019