The fire triangle, conditions and distribution: where and why wildfires occur
A wildfire needs heat, fuel and oxygen (the fire triangle); risk is highest in the seasonally hot-and-dry, fuel-rich biomes — Mediterranean scrub, the Australian bush, Californian chaparral and the boreal forests — where dry vegetation and severe fire weather coincide.
A wildfire is an uncontrolled fire that spreads through natural vegetation — forest, scrub or grassland. (It is called a bushfire in Australia and a forest fire in many other regions, but it is the same hazard.) Like any fire, it depends on three things, summarised by the fire triangle: heat (an ignition source hot enough to start combustion), fuel (dry, flammable vegetation), and oxygen (supplied by the air and by wind). Remove any one side of the triangle and the fire goes out — a principle that underpins almost every management strategy. Wildfire risk is therefore highest where all three are abundant at the same time.
The conditions that influence wildfire risk (learn these — they ARE the distribution):
| Condition | Why it raises risk |
|---|---|
| Fuel — vegetation TYPE, FLAMMABILITY and DENSITY | Some vegetation is highly flammable — oily eucalypt leaves and bark, resinous chaparral and conifers burn fiercely; dense, continuous vegetation (a high 'fuel load') lets fire spread fast, while sparse or green fuel does not |
| Climatic factors | A reliably hot, dry season desiccates vegetation and creates a regular 'fire season'; biomes with a marked dry season (Mediterranean, savanna, much of the temperate and boreal interior) are most at risk |
| Recent weather | Drought and a heatwave dry the fuel to tinder; strong, hot, dry winds drive the flames, supply oxygen and carry embers — short-term weather can turn a fuel-rich landscape into extreme fire danger within days |
The global distribution. Putting the conditions together gives the recognisable belts of high wildfire risk:
- Mediterranean climate regions — the Mediterranean basin (Greece, Portugal, Spain), California, central Chile, the Cape of South Africa and parts of southern Australia: hot, dry summers and flammable scrub (chaparral, maquis, fynbos).
- Australian bush — fire-adapted eucalypt forest and woodland, exceptionally flammable because of oils and shedding bark; the setting for the 2019–20 'Black Summer'.
- Western North America — Californian chaparral and the dry conifer forests of the western USA and Canada (e.g. the 2023 Canadian wildfire season).
- Boreal forest (taiga) of Canada, Alaska and Siberia — vast coniferous fuel that burns in the short, dry summer, much of it ignited by lightning.
- Tropical savanna grasslands — grass cures and burns readily in the dry season (many fires here are deliberately set for land management).
Note the pattern the conditions explain: the wettest places (equatorial rainforest) and the driest true deserts rarely burn — rainforest is too damp, true desert has too little fuel. High wildfire risk needs enough fuel to burn AND a dry-enough season to ignite and carry it — which is why the seasonally dry, fuel-rich biomes dominate the map.
- Fire triangle: a wildfire needs heat (ignition), fuel (dry vegetation) and oxygen (air/wind); remove any side and it goes out.
- Three risk conditions: fuel (type, flammability, density), climatic factors (a hot dry season), recent weather (drought, heatwave, strong winds).
- High-risk belts: Mediterranean scrub (chaparral/maquis/fynbos), the Australian eucalypt bush, western North America, the boreal forest, and savanna grasslands.
- Highly flammable fuels — eucalypt (oils/bark), chaparral and conifers (resin) — burn fiercely; dense continuous fuel spreads fire fast.
- Rainforest is too wet and true desert has too little fuel — high risk needs fuel AND a dry season together.
- Recent weather can switch a fuel-rich landscape into extreme danger within days (drought + heatwave + wind).