Incident Situation Report
State mobilized firefighting resources are engaged in full suppression efforts on the Davis Coulee Fire in Garfield County, Washington. The blaze has scorched 6,260 hectares (15,470 acres) of heavy canyon brush and wheat stubble under high red-flag wind warnings.
Southeast Washington Interagency Incident Management Team has established containment lines on the southern flank, holding containment at 30% while structural task forces protect rural residences along Lower Deadman Road.
🚨 Evacuation Advisories & Safety Levels
If you are near the Davis Coulee Fire perimeter, stay alert for municipal emergency broadcasts and follow all designated routes. For a complete guide to Ready, Set, Go! levels and vehicle survival tactics, review our guide on evacuation levels explained.
💨 Wildfire Smoke & Atmospheric Plume Dispersion
Heavy convective columns from the Davis Coulee Fire generate significant fine particulate matter ($PM_{2.5}$). Track local air quality indices and wind-driven aerosol drift in real time on our wildfire smoke map.
🛡️ Property Defense & Home Hardening
Ember storms ignite over 90% of residences destroyed in wildland-urban interface fires. Protect your dwelling by implementing proven defensible space tips, clearing roof gutters, and creating a non-combustible Zone 0 perimeter.
Wildlife, Endangered Species & Ecosystem Impact
The Davis Coulee Fire burns across the rugged breaks of the Snake River canyon and foothills of the Blue Mountains. The landscape supports prominent herds of Rocky Mountain Elk (Cervus canadensis nelsoni), upland game birds, and bighorn sheep. Rapid burning of riparian brush along canyon bottoms risks sediment mobilization into ESA-listed steelhead trout streams.
Compare this fire's burned footprint against active blazes worldwide in our wildfire statistics 2026 report.
Washington State Wildfire Trends, Seasonality & Risk Metrics
Comprehensive multi-year telemetry, historical burn extent graphs, and environmental fuel analysis.
| Key Parameter | Regional Value / Characteristics | Operational Significance |
|---|---|---|
| Dominant Fuel Complex | Ponderosa pine, Douglas fir timber litter & Columbia Basin shrub-steppe | Determines crown fire transmission and rate of combustion |
| 10-Yr Mean Burn Area | 480,000 acres (194,200 ha) | Historical baseline for multi-year fire cycle variance |
| Ignition Source Ratio | 62% Lightning · 38% Human / Recreation | Drives prevention patrols vs. dry lightning tracking |
| Critical Fire Weather Driver | East-wind thermal trough inversions & Cascade mountain foehn winds | Triggers Red Flag Warnings and extreme rate of spread |
| Flame Spread Velocity | Moderate to Extreme: 80–220 chains/hr in dry conifer crown canopy | Dictates initial attack evacuation lead times |
| WUI Exposure Rating | Tier 2 High: 1.4 million homes in central and eastern Washington valleys | Determines structural defense assets and evacuation tiers |
Fire Ecology & Suppression Dynamics in Washington State
Washington’s wildfire profile is governed by the topographic barrier of the Cascade Range, which bisects the state into a moist maritime western zone and an arid continental eastern rain shadow. In the Okanogan, Methow, and Yakima valleys, century-long fire exclusion combined with prolonged summer drought has generated excessive 100-hour and 1000-hour dead fuel accumulation. When upper-level atmospheric thermal troughs migrate across the Cascades, dry easterly winds accelerate down mountain canyons, causing sudden canopy crown runs through dense Douglas fir and ponderosa stands.
The Washington Department of Natural Resources (WA-DNR) operates under strict interagency agreements with the Northwest Interagency Coordination Center (NWCC). Backcountry fire containment relies heavily on smokejumper initial attack deployments out of the historic Winthrop Smokejumper Base, coupled with Type 1 Helitack operations dipping from the Columbia River and mountain lakes. Community preparedness is prioritized through the Firewise USA framework to protect isolated valley settlements from destructive ember showers during regional smoke inversions.