Source of the winds
Circulation around high pressure in the West generates strong northeasterly winds at the surface, which accelerate and warm as they blow downslope from the Sierra Nevada into Napa and Sonoma counties in California’s wine country.
Why mountain and canyon winds are stronger
Air from areas of high pressure over elevated ground inland flows down toward sea level in California. The sinking air heats up, loses moisture and speeds up, especially as it squeezes through canyons.
Mountain ranges block winds in some areas while winds howl elsewhere. Winds seek openings through the mountains, much like water would. Canyons and passes provide narrow openings that accelerate the winds like a nozzle on a garden hose does to water.
Terrain’s role with the winds during wildfires
Terrain can play a part in a fire’s progress. On hillsides with gullies or ravines, a chimney effect can cause hot gases to rise up these channels. The fire creates a draft, pulling oxygen in, and blazes roar up rapidly as if in a chimney.
Embers spread new fires
As fires rage and winds blow, hot embers may be carried far away from burning areas. They can touch off smaller spot fires well ahead of or behind a main fire, and these may turn into new wildfires.
Sources: National Weather Service, U.S. Geological Survey, Times reporting