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Warming enabled upslope advance in western US forest fires
Mohammad Reza Alizadeh1, John T Abatzoglou2, Charles H Luce3
1Department of Bioresource Engineering, McGill University, Montréal, QC H3A 0G4, Canada.
Summary
Forest fires in western US mountains are increasingly burning at higher elevations. Climate warming is reducing the high-elevation flammability barrier, allowing fires to advance upslope.
Area of Science:
- Ecology
- Climate Science
- Forestry
Background:
- Forest fires have increased in the western US over the past 50 years.
- Elevational fire distribution is critical for understanding montane ecosystem dynamics.
Purpose of the Study:
- To analyze the elevational distribution of forest fires in western US mountains.
- To investigate the relationship between fire spread and climate variables.
- To assess the impact of climate change on high-elevation fire regimes.
Main Methods:
- Analysis of burned area data from 1984 to 2017 in mountainous western US ecoregions.
- Statistical analysis of fire-elevation relationships and vapor pressure deficit (VPD).
- Modeling the impact of climate trends on high-elevation forest flammability.
Main Results:
- The largest increases in burned area occurred above 2,500 m.
- High-elevation fires advanced upslope by a median of 252 m.
- A strong correlation was found between high-elevation fires and warm season VPD.
- Climate warming has reduced the high-elevation flammability barrier, opening 11% more forests to fire.
Conclusions:
- Climate warming is the primary driver of upslope fire advancement in western US mountains.
- Weakening of the high-elevation flammability barrier has significant implications for ecosystems and watersheds.
- Continued warming may transform montane fire regimes, necessitating adaptive management strategies.
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