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Fire Behavior
Photosynthesis
Biomass is Destroyed
Four Phases of Combustion Process
1). Pre-ignition
Heat is required to raise a fuel to ignition temperature (600 degrees F)
Four Phases of Combustion Process
2). Ignition
Process where a rapid, exothermic reaction is initiated, which causes the material to undergo changes, producing temperatures greatly in excess of the ambient (Drysdale 1985).
Four Phases of Combustion Process
3). Combustion
Flaming=volatiles that are produced in the preheating phase ignite to form a visible flame
Smoldering=the remaining carbon may burn as a solid by surface oxidation
Four Phases of Combustion Process
4). Extinction
Opposite of ignition (termination of combustion)
Moisture content of fuel can play a large role
SMOKE
incomplete combustion where volatile products remain suspended as very small droplets of liquid plus residual carbonized particles that float in the air
Fire intensity-the rate at which a fire releases heat energy
Energy released/unit area/time (Btu/ft/sec)
BEHAVE FIRE MODEL
3 Basic Types of Fire Behavior
Fire Behavior Terminology
1). Running
2). Creeping
3). Smoldering
4). Spotting
Fire Behavior Terminology
5). Torching
6). Crowning
7). Flare-up
8). Blowup
Topography-- Slope Position
Topography-- Slope Position
Front Fire Backing Fire
Topography-- Slope Steepness
Pinyon-Juniper
Ponderosa Pine
Mixed Conifer
Spruce/Fir
Alpine
North South
5,000 ft6,000 ft7,000 ft
8,000 ft9,000 ft
10,000 ft
11,000 ft12,000 ft13,000 ft
14,000 ft
Topography-- Aspect and Elevation
Aspect
SOUTHSOUTH
NORTHNORTH
Heavy fuelsShadeMoist
Light fuelsSunnyDry
Topography-- Barriers
Topography-- Box Canyon
Chimney Effect- Occurs when unstable air conditions at the surface create a convection current through the canyon, drawing air in at the base of the canyon and exhausting it at the top
Radiant Heat Across Narrow Canyon
Spotting Across Narrow Canyon
1. insolation—solar radiation that is intercepted by Earth (surface and atmosphere)
Influenced by: a) angle of incoming radiation b) length of time exposure
Weather-Temperature
Weather-Temperature
patterns of heat gain/loss daily
Midnight 6 noon 6 Midnight
Coolest time
Hottest time-maximum amount absorbed
Temp Energy Flow
Spatial patterns on heat/cold
Day
Night
warm
cold
Weather-Temperature
The amount of humidity the air can hold at a specific temperature compared to the amount that it is actually holding is called the relative humidity.
Weather-Relative Humidity
Red line is fuel moisture--note lag time
WINDWARD LEEWARD
Rainshadow
Dewpoint
Chinook Winds
Adiabatic lapse rate-change in temperature with altitude due to pressure
Weather-Air Stability
Weather-Wind/Storm Relationships
Weather-Wind
horizontal movement of air
Weather-Types of Wind
Mountains Cause Channeling of Wind
Convection Column-rapidly rising superheated smoke can soar 35,000 feet or higher into the atmosphere and cause a rapid indraft of cooler air to the fire on the ground
Weather-Fire
El Nino is a disruption of the ocean-atmosphere system in the tropical Pacific that has implications for weather around the globe
1) Fuel-QuantityWays to Classify Fuels:
Oven dry weight of fuels in a given area
2) Fuel-Size and Shape
Duff is the organic forest horizons (fermentation and humus layers) that accumulate above the mineral soil
Litter is the surface layer consisting of freshly fallen leaves, needles, twigs, stems, and bark.
3) Fuel-Arrangement
Uniform Fuels
Patchy Fuels
Ladder Fuels
4) Fuel-Components
3) GROUND
2) SURFACE
1) AERIAL
How are fuels characterized?
1) Direct-sampling
2) Planar transect
3) Photo guides
4) Prediction models
Fuel-Moisture Content
Fuel moisture-percent of dry weight of fuel
Live fuel moisture- can range from 1-over 100 percentDead fuel moisture- often below 10 percent
Timelag Intervals-time required to lose 63 percent (2/3) of difference between original moisture content and equilibrium moisture content at a constant temperature and relative humidity
Fuel changes over time
1) Abrupt
2) Diurnal
3) Seasonal
4) Annual
• Unusually dry fuels.
• Large amount of light fuel (shrubs, grass, needles).
• Fuels exposed to direct sunlight.
• Fuels dried by prolonged drought.
• Ladder fuels that allow a surface fire to move into the crowns of shrubs or trees.
• Crown foliage dried by surface fire.
• Concentration of snags.
Indicators of Problem and Extreme Fire Behavior
Fuel IndicatorsFuel Indicators
Indicators of Problem and Extreme Fire Behavior
• Steep slopes.• Chutes, saddles, and box canyons which
provide conditions for “chimney effect.”• Narrow canyons may increase fire spread by
radiant heat and spotting.
Topography IndicatorsTopography Indicators
• Strong Wind.
• Sudden changes in wind direction and velocity due to weather fronts.
• High, fast-moving clouds may indicate unusual surface winds.
• Unexpected calm may indicate wind shift.
• Thunderstorms above or close to the fire.
• Unusually high temperatures and low relative humidity.
• Dust devils and whirlwinds developing.
• Bent smoke column.
Indicators of Problem and Extreme Fire Behavior
Weather IndicatorsWeather Indicators
• Keep an eye on the smoke column. Indicates direction of fire spread, location of spot fires, and changes in fire intensity.
• Many simultaneous fires starting or smoldering fires beginning to pick up in intensity.
• Fire begins to torch small groups of trees or shrubs.
• Frequent spot fires occurring.
• Firewhirls beginning to develop inside the main fire.
• Crown fires.
Indicators of Problem and Extreme Fire Behavior
Fire Behavior IndicatorsFire Behavior Indicators