Forest fires are common in places around the world where climates are moist enough to allow the growth of trees and shrubs, but have extended dry, hot periods.
What factors make wildfires burn more?
Wind strength
Humidity
Seasons
Space between fuels
Slope (topography)
Wind strength – this determines the rate of spread – e.g. the Black Saturday fires in Australia were driven by winds of up to 125 km/h (80mph).
Humidity – the drier it is, the longer the fire is likely to last and the more intense it is likely to be.
Seasons – some locations experience drastic differences in temperature depending on the season it is – e.g. in Feb 2009 (Australia’s summer), temperatures had risen about 40 degrees C!
Space between fuels – denser vegetation is likely to lead to the continued spread of the fire.
Slope (topography) – fires on a 20 degree slope will advance at up to four times faster than on a flat surface! Have a look at the next slide…
The ‘ladder effect’ describes the process of fires spreading from the forest floor to the canopy
Pyrophytes = plants which have adapted to tolerate fire – surprisingly, fire acts favourably for some species
Passive Pyrophytes = resist the effects of fire, particularly when it passes over quickly, and hence can out-compete less resistant plants which are damaged.
Active Pyrophytes = have a similar competing advantage to passive pyrophytes, but they also contain volatile oils and hence encourage the incidence of fires which are beneficial to them
Phyrophile = plants which require fire in order to complete their cycle of reproduction.
Eucalyptus is packed full of VOCs (Volatile Organic Compounds) which enhance its flammability – this includes the bark and the leaves.
Lightning strikes the Earth over 100,000 times a day. Of these, 10-20% cause a fire.
Forest fires move faster uphill than downhill! The steeper the slope, the faster the fire travels. If you live on a hill, you might want to leave your house if a wildfire is near.