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Forested areas in the Western U.S. that are impacted by disturbances such as fire and drought have increased in recent decades. This trend is likely to continue, with the increase in frequency and extent of wildfire activity being especially concerning. Resource managers need reliable scientific information to better understand wildfire occurrence, which can vary substantially across landscapes and throughout time. However, few scientific models capture this variability, and projections of future potential changes in fire occurrence can include some uncertainty. This uncertainty can limit our ability to anticipate potential wildfire impacts on society and ecological systems. Another method to help managers prepare...
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Wildfire burn areas are increasing in the western U.S., a change that has been linked to increased fuel aridity caused by climate change. Recognizing that there will likely be even more large fires in the future presents an opportunity to prepare and adapt to the expected climatic changes. This project addresses three key science questions: 1) Is there a specific level (threshold) of fuel aridity below which large fires more likely, and levels of temperature and humidity that don’t change how these fires begin and spread? 2) if there is a fuel aridity threshold, how often has that level been exceeded in the past? 3) Do climate models predict this threshold will be exceeded more or less often in the future? ...
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A change in wildfire regimes and the expansion of invasive grasses are degrading sagebrush ecosystems, altering wildlife habitats, and threatening property and human livelihoods. In response, land managers often treat large areas of land with fuel reduction or post-fire seeding treatments in an attempt to reduce these risks. However, the trajectories of ecosystem change following treatment are inconsistent across the sagebrush steppe. In some places, treatments are successful, leading to a decrease in invasive grasses which allows native plants to recover. In other places, treatments either have no effect or they facilitate the spread of invasive grasses. Under some climate conditions, native grasses and forbs do...
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The Colorado River provides water to 40 million people in the southwestern United States. Consistent water level declines in Colorado River Basin reservoirs have focused research attention on the long-term changes in winter precipitation and the timing of snowmelt and runoff. Research on how warming temperatures affect winter precipitation and spring snowmelt is ongoing, however, less attention has been given to changes in spring and summer precipitation which also affects water supply, plant growth, and competition between native and non-native plants, and, in turn affects wildfire dynamics and wildlife habitat. The amount and timing of summer precipitation is largely influenced by variation in the North American...
    map background search result map search result map Drought and Disturbances as Drivers of Long-Term Ecological Transformation and Risk Trajectories of Change: How Climate, Wildfire, and Management Drive Shrubland Ecosystem Transitions Modeling Large Fires in Response to Potential Tipping Points in Fuel Dryness Understanding the Effects of Seasonal Precipitation Changes on Hydrology and Ecosystems in the Colorado River Basin Trajectories of Change: How Climate, Wildfire, and Management Drive Shrubland Ecosystem Transitions Understanding the Effects of Seasonal Precipitation Changes on Hydrology and Ecosystems in the Colorado River Basin Modeling Large Fires in Response to Potential Tipping Points in Fuel Dryness Drought and Disturbances as Drivers of Long-Term Ecological Transformation and Risk