Fire Weather and Fuel Moisture Flashcards
Fire behavior triangle
Weather, fuel, topography
Wind
Movement of air relative to Earth’s surface
- most variable element in time and space, most difficult to predict, most critical factor in fire behavior (for weather)
- direction it blows (N wind blows from N → S)
Effect of wind on fire behavior
- can carry away moist air and quicken drying of wildland fuels
- brings oxygen
- carries heat, increases fire spread
- affects residence time of flaming front
General wind
Mid to upper levels of troposphere
Local wind
Lower levels of troposphere
- influenced by terrain
- caused by small-scale differences in air temperature and pressure
- upslope and upvalley vs. downslope and downvalley
Upslope and upvalley local winds
Faster spread rates
Downslope and downvalley local winds
Can reverse fire direction
Foehn winds
Strong, warm, dry winds generated by high pressure in mountainous regions
- extreme fire behavior
- Santa Ana winds (1971 windstorm, sudden increase in temperature = decrease in relative humidity)
Effect of humidity on fire behavior
Moisture in atmosphere affects fuel moisture/fire behavior
- less moisture = drier fuels and more extreme fire behavior
Wet bulb temperature
Lowest temperature to which air can be cooled by evaporation (measured using psychrometer)
Dewpoint temperature
Temperature to which air must be cooled to reach saturation
Saturation
When air temperature falls to dewpoint temperature
- when air is fully saturated dry bulb temperature, wet bulb temperature, and dewpoint temperature are the same
- air cannot hold more moisture
Relative humidity
Ratio of amount of moisture in air to amount air could hold when saturated at same air temperature
- warmer air can hold more water
Live fuel moisture
- varies with plant type/growth
- newest foliage = highest moisture content
- deciduous foliage
Live fuel moisture content of evergreens
- Older than 1 year = 80-120%
- Current year = 250%