Landscape heterogeneity following large fires: insights from Yellowstone National Park, USA

2008 ◽  
Vol 17 (6) ◽  
pp. 742 ◽  
Author(s):  
Tania Schoennagel ◽  
Erica A. H. Smithwick ◽  
Monica G. Turner

We characterised the remarkable heterogeneity following the large, severe fires of 1988 in Yellowstone National Park (YNP), in the northern Rocky Mountains, Wyoming, USA, by focussing on spatial variation in post-fire structure, composition and ecosystem function at broad, meso, and fine scales. Ecological heterogeneity at multiple scales may enhance resilience to large, severe disturbances by providing structural, biological and functional redundancy. Post-fire heterogeneity in stand age, coarse wood abundance, microbial and understorey communities reflected interactions between existing pre-fire patterns and fire severity at different scales, suggesting that environmental context plays an important role in successional responses to large fires. In response to these post-fire patterns, heterogeneity in carbon (C) and nitrogen (N) storage, N mineralisation, decomposition, and productivity was also evident at multiple scales and may confer resiliency to large fires. For example, at broad scales, C storage in YNP appears resistant to changes in age-class structure associated with large stand-replacing fires. In summary, the YNP landscape is recovering rapidly from the 1988 fires through natural mechanisms, owing to the abundance and spatial heterogeneity of post-fire residuals, but other systems with fewer biotic legacies may be less resilient to such large, severe fires.

Author(s):  
Monica Turner ◽  
Rebecca Reed ◽  
William Romme ◽  
Mary Finley ◽  
Dennis Knight

The 1988 fires in Yellowstone National Park (YNP), Wyoming, affected >250,000 ha, creating a striking mosaic of burn severities across the landscape which is likely to influence ecological processes for decades to come (Christensen et al. 1989, Knight and Wallace 1989, Turner et al.1994). Substantial spatial heterogeneity in early post-fire succession has been observed in the decade since the fires, resulting largely from spatial variation in fire severity and in the availability of lodgepole pine (Pinus contorta var. latifolia) seeds in or near the burned area (Anderson and Romme 1991, Tinker et al. 1994, Turner et al. 1997). Post­fire vegetation now includes pine stands ranging from relatively low to extremely high pine sapling density (ca 10,000 to nearly 100,000 stems ha-1) as well as non-forest or marginally forested vegetation across the Yellowstone landscape may influence ecosystem processes related to energy flow and biogeochemisty. We also are interested in how quickly these processes may return to their pre­ disturbance characteristics. In this pilot study, we began to address these general questions by examining the variation in above-ground net primary production (ANPP), leaf area index (LAI) of tree (lodgepole pine) and herbaceous components, and rates of nitrogen mineralization and loss in successional stands 9 years after the fires. ANPP measures the cumulative new biomass generated over a given period of time, and is a fundamental ecosystem property often used to compare ecosystems (Carpenter 1998). Leaf area (typically expressed as leaf area index [LAI], i.e., leaf area per unit ground surface area) influences rates of two fundamental ecosystem processes -­ primary productivity and transpiration -- and is communities (


Author(s):  
Monica Turner ◽  
Robert Gardner ◽  
William Romme

The 1988 fires that burned in Yellowstone National Park presented ecologists with a unique opportunity to investigate ecological responses to large-scale fires (Christensen et al. 1989, Knight and Wallace 1989). The Yellowstone fires created an extremely heterogeneous landscape in terms of both the overall burning patterns and the variable fire severity within burned areas. Large fires rarely consume the entire forest because of the influence of wind variations, topography, vegetation type, natural fire breaks, and the time of day that the fire passed through (Rowe and Scotter 1973, Wright and Heinselman 1973, Van Wagner 1983). Direct fire effects such as tree mortality and organic matter consumption are related to locally variable parameters such as moisture content (Brown et al. 1985, Peterson and Ryan 1986, Ryan et al. 1988), and fire severity and return intervals are often strongly influenced by topographic and edaphic variability (Habeck and Mutch 1973, Romme and Knight 1981, Hemstrom and Franklin 1982, Whitney 1986). Therefore, burned landscapes generally contain areas of low as well as high intensity fire, usually in a complex mosaic (Van Wagner 1983). These variable fire intensities result in a heterogeneous pattern of burn severities (effects of fire on the ecosystem), as well as islands of unburned vegetation. The influence of burn severity on plant reestablishment following fire is well documented (e.g., Lyon and Stickney 1976, Rowe and Scotter 1973, Viereck 1983, Ryan and Noste 1985), and the importance of the effects of limited burns and low-intensity fires on the vegetation mosaic has been recognized (Habeck and Mutch 1973, Rowe 1983). However, few studies have dealt explicitly with the spatial variation of fire effects in a systematic and quantitative way.


Author(s):  
W. Romme ◽  
J. Yavitt ◽  
D. Knight ◽  
J. Fedders

A research project was initiated in 1980 to study the effects of outbreaks of the mountain pine beetle (Dendroctonus ponderosae) on lodgepole pine forest (Pinus contorta spp. latifolia) in Yellowstone National Park and surrounding areas. This native bark beetle recently has killed millions of trees over thousands of square kilometers in the central and northern Rocky Mountains. Major outbreaks first occurred in Grand Teton National Park in the 1950's and in Yellowstone National Park in the 1960's. The outbreak in Yellowstone Park is still spreading.


Author(s):  
Dennis Knight ◽  
William Romme

Fire is now recognized as a major ecosystem process and Yellowstone National Park has recently implemented a fire management plan that permits lightning fires to burn without interference under certain conditions. To predict the kinds of wildfires we can now expect in the Park, and to evaluate the effectiveness of this plan in restoring fire to the Yellowstone ecosystem, it is important to know the natural frequency and size of wildfires under pristine conditions. This study, which began in 1977 and will be completed in June 1979, has the following objectives: (1) to determine the incidence and size of major fires during the last 300-400 years on the 100-km2 Little Firehole River watershed, an area dominated by extensive lodgepole pine and some spruce-fir forests; (2) to determine average fire frequency, i.e., the time interval between successive major fires on any particular site; and (3) to determine the relationships between stand age or successional stage and fuel accumulation or the probability of fire.


Author(s):  
William Romme ◽  
Dennis Knight

Fire is now recognized as a major ecosystem process and Yellowstone National Park has recently implemented a fire management plan that permits lightning fires to burn without interference under certain conditions. To predict the kinds of wildfires we can now expect in the Park, and to evaluate the effectiveness of this plan in restoring fire to the Yellowstone ecosystem, it is important to know the natural frequency and size of wildfires under pristine conditions. This study, which began in 1977 and was completed in August 1979, had the following objectives: (1) to determine the incidence and size of major fires during the last 300-400 years on the 73-km2 Little Firehole River watershed, an area dominated by extensive lodgepole pine and some spruce-fir forests; (2) to determine average fire frequency, i.e., the time interval between successive major fires on any particular sites; (3) to determine the relationships between stand age or successional stage and fuel accumulation or the probability of fire; and (4) to examine the effect of fire on patterns of landscape diversity. Three components of landscape diversity were recognized - richness, evenness, and patchiness. Richness is simply the number of different community types represented, while evenness is an expression of the proportion of the landscape covered by each community type (maximum evenness occurring when every type occupies an equal area). The patchiness component is based on the size and interspersion of the community types.


Author(s):  
Tania Schoennagel ◽  
Monica Turner

Many scientists predict that due to the quick response of fire regimes to changes in climate (Flannigan et al. 1998; Stocks et al. 1998), the most rapid and extensive effects of climate change will be mediated by altered disturbance regimes (Davis and Botkin 1985; Franklin et al. 1992; Graham et al. 1990; Weber and Flannigan 1997). Under climate scenarios expected for C02 doubling, Price and Rind (1994) predict a 44% increase in lightning-caused fires and a 78% increase in total area burned for the U.S. Although regional climate scenarios are still subject to a fairly high degree of uncertainty, regional predictions for Yellowstone National Park (YNP) estimate an increase in aridity (Balling et al. 1992) and mean July temperatures (Bartlein et al. 1997), suggesting that fire frequencies could significantly increase in YNP over the next century. While several models have simulated the response of western coniferous forests to altered fire regimes (Baker et al. 1991; Gardner et al. 1996; Keane et al. 1990; Keane et al. 1995; Romme and Turner 1991), little empirical work on the successional responses to different intervals of stand­replacing fire has been incorporated, and remains a critical element in predicting the effects of climatically altered disturbance regimes in forested landscapes. Previous work in Yellowstone has considered the effects of fire severity, fire size and level of serotiny in explaining initial pathways of postfrre succession across the Yellowstone landscape (Turner et al. 1994; Turner et al. 1997). The effects of the third component of the disturbance regime, fire interval, remains largely unexplored, and represents a fundamental link in predicting potential effects of climate change on the Yellowstone landscape. The specific objectives of our research, therefore, were to assess: Are there a significantly different successional responses following different intervals of stand-replacing fire in Yellowstone National Park? Because serotiny exerts a strong influence on initial post-fire succession in Yellowstone (characterized by variation in lodgepole pine densities), we also sought to track stand-level changes in serotiny over time. In order to flesh out a possible mechanism for why postfrre succession may vary depending upon the age at which the stand burns we asked: What is the temporal variation in lodgepole pine serotiny within the park?


Author(s):  
W. Romme ◽  
J. Yavitt ◽  
D. Knight ◽  
J. Fedders

A research project was initiated in 1980 to study the effects of outbreaks of the mountain pine beetle (Dendroctonus ponderosae) on lodgepole pine forests (Pinus contorta spp. latifolia) in Yellowstone National Park and surrounding areas. This native bark beetle recently has killed millions of trees over thousands of square kilometers in the central and northern Rocky Mountains. Major outbreaks first occurred in Grand Teton National Park in the 1950's and in Yellowstone National Park in the 1960's. The outbreak in Yellowstone Park is still spreading.


2009 ◽  
Vol 18 (7) ◽  
pp. 765 ◽  
Author(s):  
James A. Lutz ◽  
Jan W. van Wagtendonk ◽  
Andrea E. Thode ◽  
Jay D. Miller ◽  
Jerry F. Franklin

Continental-scale studies of western North America have attributed recent increases in annual area burned and fire size to a warming climate, but these studies have focussed on large fires and have left the issues of fire severity and ignition frequency unaddressed. Lightning ignitions, any of which could burn a large area given appropriate conditions for fire spread, could be the first indication of more frequent fire. We examined the relationship between snowpack and the ignition and size of fires that occurred in Yosemite National Park, California (area 3027 km2), between 1984 and 2005. During this period, 1870 fires burned 77 718 ha. Decreased spring snowpack exponentially increased the number of lightning-ignited fires. Snowpack mediated lightning-ignited fires by decreasing the proportion of lightning strikes that caused lightning-ignited fires and through fewer lightning strikes in years with deep snowpack. We also quantified fire severity for the 103 fires >40 ha with satellite fire-severity indices using 23 years of Landsat Thematic Mapper data. The proportion of the landscape that burned at higher severities and the complexity of higher-severity burn patches increased with the log10 of annual area burned. Using one snowpack forecast, we project that the number of lightning-ignited fires will increase 19.1% by 2020 to 2049 and the annual area burned at high severity will increase 21.9%. Climate-induced decreases in snowpack and the concomitant increase in fire severity suggest that existing assumptions may be understated – fires may become more frequent and more severe.


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