Tim Brown, director of the Western Regional Climate Center at the Institute for Desert Research in Reno, Nevada, said the excessive heat caused vegetation to be exceptionally dry and more prone to burning. Temperature, humidity, wind and solar radiation dry out the brush and are key elements of fire. “We call this evaporative demand,” he said. And in recent weeks, he added, “the western cascades have been really dry due to the need for evaporation.”
These dry conditions are likely to have been exacerbated by climate change, according to Meg Kravchuk, a professor at the Oregon College of Forestry. They “prepared the landscape” for the wildfire, she said.
The critical moment came on Monday and Tuesday, when a storm blew hot air from the high desert in eastern Oregon over the mountains, quickly spreading fires to the more densely populated western part of the state, according to Josh Clarke, a fire meteorologist with the Washington State Department of Natural Resources.
Those winds were the strongest the state has seen in at least 30 years, Clark said. And when they crossed the mountains, the winds swept through the river canyons, compressed the air, warming it even more and pushing it westward like fur.
As these fires raced westward, they encountered unusually dry conditions, which in turn allowed the already burning fires to spread quickly, Dr. “Fire can move very quickly and just explode in these canyons,” she said.