The wildfires that broke out over the past week in France and Spain, which have already burned more than 115,000 hectares and forced over 320,000 people from their homes, have stood out for the sheer violence and scale of the flames. The French authorities admit that it may take months to extinguish them.
They are the latest examples of what the operational and scientific community has, since the second half of the 2010s, come to describe as “sixth-generation fires”, especially after the blazes in Pedrógão Grande in Portugal (2017) and in Greece (2018), each of which claimed more than 100 lives.

This new pattern first became more evident in Europe, although it was also identified in 2017 in Chile, where it returned in an even more devastating form in 2024, a year in which 137 people lost their lives. These same characteristics have also been observed in other parts of the world, notably in Australia (2019–20), on the west coast of the United States (2020) and in Canada (2023).
The major shift in fire behaviour is being driven by climate change, explains Domingos Xavier Viegas to Euronews, a professor at the Faculty of Science and Technology at the University of Coimbra (FCTUC) and a specialist in rural fires. With higher temperatures, less rainfall and lower levels of humidity, the soil and vegetation become drier, greatly increasing the “conditions for ignition” and the “area available to burn”.
What sets a sixth-generation wildfire apart?
The destructive potential of these megafires stems from the energy they release, which can alter the weather conditions around them and exhaust traditional firefighting resources, however robust these may be.
When more than ten megawatts (MW) per metre are being released, the fire can no longer be put out through the direct action of firefighters, Xavier Viegas explains. “If we translate that into flame length, a front that is releasing ten MW will have flames roughly ten metres high,” he adds.
“What is happening is that, nowadays, we sometimes have fires which, in certain phases of their spread, reach intensities three, four, five, even six times higher. In other words, it is impossible to fight flames that can be up to 60 metres long,” the specialist notes.
A thermal load of this magnitude makes these fires self-feeding, so they cease to be just a phenomenon controlled by the local atmosphere and begin to influence it as well.
Exceptionally dense smoke clouds form, carrying enormous heat, changing wind direction, producing electrical discharges and hurling embers several kilometres ahead, which in turn ignite new fires.






