Learn about wildland fire
In this section
Forest Management Services of the Government of the Northwest Territories (GNWT) seeks opportunities to transfer, adopt, adapt or develop appropriate technologies that complement the environmental mandate.
Forest Management Services facilitates the timely development, adoption and dissemination of scientific fire research and best practices to support GNWT fire management activities and assist with making critical forest management, policy and investment decisions.
Forest Management Services aims to:
- provide leadership in fire science and technology advancements
- increase the integration of science and technology in operational fire management decision making
- target information and technology transfer
- use scientific and traditional knowledge to identify and mitigate wildland fire risk
- encourage collaborative projects
- encourage experience and information sharing
Why do wildland fires burn?
Three elements are needed for a fire to start and continue to burn:
- fuel (wood, brush, lichen)
- oxygen (from the air)
- ignition source (heat from lightning or man)
If any one of these three elements is missing, there can be no fire. The basic principal of wildland firefighting, therefore, is to remove one or more of these elements in the quickest and most effective way.
Why do wildland fires spread?
The primary factors that influence the spread of fires are:
Light, small or fast-burning fuels
Dry grass, dead leaves and tree needles, brush and small trees. Light fuels ignite quickly and cause rapid spread of fire. They act as kindling for heavier fuels and burn out faster. Some green fuels such as tree needles have high oil content, and are fast-burning when they are not in an active growing stage.
Heavy, large or slow-burning fuels
Logs, stumps, branch wood and deep duff (the topsoil or partly decayed leaves and tree needles found under dense stands of brush or trees). Heavy fuels take longer to ignite, spread slower, burn longer and throw off large volumes of heat when dry.
Snags struck by lightning can sometimes be the cause of forest fires, particularly if they are left to burn/fall to the ground without follow-up assessment and/or suppression.
Due to the unique falling challenges posed by burning snags, this task is left to certified Danger Tree fallers. All burning trees are considered suspect and must be properly assessed.
In some cases if snags are actively burning inside, it may be desirable to suppress or extinguish the fire before falling cuts are made, as falling cuts can increase the amount of oxygen available to the fire and could result in the fire flaring up. If crews have any doubt about having sufficient resources to control a fire once a burning snag strikes the ground, the tree is left standing and a suitable No Work Zone is placed around it. It is then regularly monitored until the tree falls and the fire is completely extinguished.
The ease of ignition and rate of burning are influenced by the size of fuels.
Fuel spacing describes the distribution of fuels in a given area.
Fuel continuity is an important factor in the behaviour of fire because it indicates how quickly and why a fire may spread.
A wide range of fuel continuity conditions will be found in most forested areas. However, for simplicity in determining fire behaviour, two broad classifications of fuel spacing will be discussed: horizontal and vertical.
Horizontal spacing is the spacing of the fuel as it lies on the ground. When fuels are close together, the fire will spread faster.
When fuels are patchy, scattered or separated by natural barriers such as rock, outcropping, streams, or areas of bare ground, the fire will be irregular and spread more slowly.
A common method used in fire suppression is to break the continuity of the fuel by separating burning fuels from unburned fuels.
When fuels are closely spaced vertically, fire will spread rapidly as the fuels are pre-heated prior to ignition. When fuels are spaced far apart vertically, the heat is not sufficient to ignite the fuels above.
As the amount of flammable material in a given area increases, the amount of heat produced by the fire also increases.
The hottest fires, as well as those most difficult to control, occur in areas containing the greatest quantity of fuel.
In evaluating fuel volume, it should be noted that a lot of small material such as fine deadwood, means that there is a lot of kindling material to light other fuels. A lot of either small or large-sized material means that there is a good chance of a hot fire. When fires start in areas containing a lot of large-sized material, there will be intense heat transfer to fuels lying in the path of the fire.
One of the most important factors affecting the behaviour of a fire is weather. The three most important components of weather are:
The stronger the wind, the faster the spread of the fire. Wind brings an additional supply of air to the fire. It flattens the flame which pre-heats the fuel ahead and causes spot fires by blowing sparks and embers ahead of the main fire into a new source of fuel.
Winds generally blow upslope at 5 to 10 miles per hour during the day because sun-warmed air rises. At night, they reverse and blow downslope because cooler night air sinks. The wind at night is not usually as strong as the wind during the day.
When you are planning a fire attack, the direction of canyon and slope winds should be carefully considered. Air currents flow up a canyon and slope during the day and down during the night.
Other wind behaviour characteristics which must be considered:
- prevailing winds usually blow from late morning to late afternoon and may blow at 15 to 30 km per hour or higher by mid-afternoon
- cumulus clouds may indicate possible change in wind speed and direction
- winds usually flow out from the edges of a thunderstorm and may reach speeds of 115 km per hour
- gusty winds are very hazardous to fire-fighters because they change speed and direction rapidly
Fuels pre-heated by the sun burn more rapidly than cold fuels. The temperatureof the ground also affects the movement of air currents, as explained previously. Prolonged high temperatures also affect the endurance and efficiency of the firefighters.
Moisture in the form of water vapour is always present in the air. The measurement of that moisture is called humidity and is always expressed as a percentage.
Warm air absorbs more moisture and produces a lower humidity. As air cools, the humidity increases. The amount of moisture in the air affects the moisture in the fuel. This is an important factor in firefighting, since wet and most green fuels will not burn freely. Air is usually drier during the day than at night. Fires, then, burn more slowly at night, under normal circumstances, because the fuels absorb moisture from the damp night air.
This partially explains why a fire burns out of control in the afternoon and yet may be controlled by the same crew at night. Every effort should be made to control a fire before burning conditions build up the next day. In British Columbia, the goal of all firefighters is to control or extinguish any fire within the first burning period.
This doesn't mean that an attempt to suppress a fire should not be made during the day. Most fires are controlled during the day. If a fire cannot be controlled during the day, an all-out effort must be made at night.
The 'lay of the land' is called topography. This is an important factor in the rate and direction of fire spread and is usually broken into three categories:
Slope is the steepness of the land and has the greatest influence on fire behaviour.
The steepness of the slope affects both the rate and direction of the fire spread. Fires usually move faster uphill than downhill and the steeper the slope, the faster the fire will move. This is because:
- on the uphill side, the flames are closer to the fuel
- the fuels become drier and ignite more quickly than if on the level ground
- wind currents are normally uphill and this tends to push heat flames into new fuels
- convected heat rises along the slope causes a draft which further increases the rate of spread
- burning embers and chunks of fuel may roll downhill into unburned fuels, increasing spread and starting new fires
Aspect is the direction the land faces - north, south, east or west. The aspect of a slope influences a fire's behaviour in several ways:
- southern aspects receive more direct heat from the sun, drying both the soil and the vegetation
- fuels are usually drier and less dense on southern slopes than fuels on northern slopes
- heating by the sun also causes earlier and stronger slope winds
- on south-facing slopes, there will normally be higher temperatures, stronger winds, lower humidity and lower fuel moistures
These are all the conditions needed for quick starts and a rapid rate of fire spread.
Terrain or special land features may control wind flow in a relatively large area. Wind flows like water in a stream and will try to follow the path of least resistance.
Most wildland fires in the Northwest Territories are the result of lightning. Lightning-caused fires can destroy timber, cut forest products, equipment and structures, but are also a natural part of the ecosystem.
The Canadian Lightning Detection Network consists of a network of lightning locators that provide complete coverage of the province. Wildland Fire Operations pays an annual fee for real-time access to the data. This network can detect more than 90% of all lightning strikes occurring in the NWT.
To collect the data, the lightning locators continuously detect and record all cloud-to-ground lightning strikes as they occur. After triangulation, the data is sent to a large main-frame computer. All of this takes about 60 milliseconds. The information is then sent to the Forest Management Division.
Once received, the latitude and longitude, time and polarity of the strike is moved into a database and is available for plotting on computer-generated maps. Wildland fire personnel can then check lightning hot spots for new wildfires and allocate resources more effectively.
Lightning can strike almost anywhere (up to 15 kilometres from a storm cell) so may not be affected by rain. Dry lightning can also occur and is a potent ignition source because there is not enough moisture with the storm to interfere with ignition or fire spread. More information about keeping your family safe when lightning strikes can be found the Environment Canada and Climate Change (ECCC) website.
To find out which areas are at greatest risk of being struck by lightning, view ECCC's Canadian Lightning Danger Map.