by Christopher Dunagan
Editor’s Note: This series was originally published in the Encyclopedia of Puget Sound.
Climate change is expected to dry out the forests, increasing the number and size of wildfires that could threaten thousands of homes.
The summer of 2015 brought hot, dry winds blowing into Western Washington from the east. Ominous breezes parched the forests, promoted wildfires and foreshadowed a future of increased fire danger on the “wet side” of the Cascade Mountains.
On Aug. 10 of that year, a lightning strike on Mount Ross in North Cascades National Park ignited a slow-moving fire on a precipitous slope. The blaze smoldered along for more than a week before it blew up on Aug. 19, when strong winds pushed the flames toward the small town of Newhalem. The fire grew from about 100 acres to about 3,200 acres in a single day.
Newhalem is a company town owned by Seattle City Light. Employees who live there operate the extensive Skagit River Hydroelectric Project, which provides power to the Seattle region. Cynthia Stahlecker, operations secretary, recalled the intense flames, smoke and heat as the fire approached.
“You could see the fire coming over the hill,” she said, “and then it jumped the river and circled the town. The smoke was so thick that I couldn’t see out the back door. The sound was like a great big jet engine taking off. I have never experienced anything like that, nor do I ever want to again.”
That night, as firefighters battled the smoky blaze at the edge of town, emergency officials organized an evacuation of Newhalem residents as well as those living in nearby Diablo. The North Cascades Highway was blocked to the west, so a convoy of vehicles escaped over the mountains into Eastern Washington.
The convoy, originally bound for Winthrop, was diverted to Wenatchee to avoid an extreme forest fire that has been called the Okanogan Complex Fire. During August of 2015 — the hottest year on record — Eastern Washington suffered through a series of forest fires that burned a record 1.1 million acres, killing three firefighters and destroying 123 homes.
Historically, the evacuation of Newhalem and Diablo stands as one of the few fire-driven escapes from populated areas west of the mountains. But researchers who study the risk of wildfire say a warming climate in Western Washington could bring an increasing number of fires to the doorsteps of more than a million homes scattered through the woods or clustered in small communities throughout Western Washington.
Maritime Climate Changing
Western Washington — between the Pacific Ocean and the Cascade Mountains — is known for its cool, moist breezes blowing in from the sea. For the past 300 years, wildfires have been rare and relatively small, thanks to moist vegetation and infrequent lightning storms. Early loggers talked about their discovery of “asbestos forests,” which would provide a vast supply of quality lumber to a growing nation.
When it comes to fire behavior, Eastern and Western Washington are recognized as “different worlds with very little overlap,” according to Dave Peterson, who studies fire science and climate change at the University of Washington’s School of Environmental and Forest Sciences.
Under natural conditions, fires on the east side tend to be less intense but more frequent. Dry conditions produce less vegetation to fuel the flames. At the same time, lightning strikes occur more often in Eastern Washington, providing the sparks for recurrent fires. This natural cycle can be disrupted when humans put out the fires, allowing fuels to build up. The ultimate consequence is larger and more intense fires.
Meanwhile, the wetter conditions of Western Washington encourage dense vegetation to grow quickly. Potential fuels accumulate over time, not only from the prosperous growth of living trees and underbrush, but also from fallen logs, dead brush and decaying “duff” that builds up on the forest floor. As fuels pile up, fire waits for the right conditions — specifically a long dry spell, a source of ignition and winds to fan the flames.
If humans don’t ignite a fire, a century or more may come and go before all the right conditions come together in Western Washington for a widespread fire to take off and burn with great intensity.
Understanding the differences between Eastern and Western Washington has led some fire researchers to propose a separate strategy for combatting fire hazards on the west side of the mountains. Actively thinning forests and reducing fuel loads may work in Eastern Washington, where such efforts are currently underway. But in Western Washington, vegetation generally grows back too fast for thinning to be an effective treatment, researchers say. Besides, thinning the dense plants that fuel fierce west-side fires could eliminate a variety of species that depend on this special habitat.
Over the past 1,000 years, three major burn periods in Western Washington have been identified by scientists, who estimate fire dates by studying the age of trees growing on the landscape and by examining the “burn scars” left among tree rings, as seen in the cross-section of a log.
One large fire or a series of smaller fires swept across Western Washington around 1308, followed by another great burning period from 1448 to 1538, when several fires occurred. The latest period of conflagration involved a pair of major fires, one about 1668 and the other about 1701.
Because each of these intense “stand-replacing” fires consumed evidence from the ones before, the best documentation comes from the 1701 fire, which burned an estimated 3 million to 10 million acres across Western Washington, according to a technical report developed for the U.S. Forest Service. For comparison, 10 million acres is roughly equivalent to the entire Puget Sound watershed or about 10 times the size of Olympic National Park. Many of the old-growth trees that supplied lumber for a burgeoning industry in the 1800s got their start soon after the 1701 fire wiped out much of the vegetation that existed at the time.
For the past 300 years, fires in Western Washington have been small compared to the great fires of ancient times. They usually occurred during drought years, and the larger fires were generally accompanied by strong winds from the east. Such was the case with the 1902 Yacolt Burn, the largest fire in Washington state history up until 2014. The fire, near the Columbia River, scorched 239,000 acres of forestland in Southwest Washington and nearly that much across the river in Oregon.
Since 1985, Western Washington has seen 11 fires of more than 1,000 acres, which have burned about 50,000 acres in total. That includes the 6,632-acre Goodell Creek fire, which led to the evacuation of Newhalem and Diablo in 2015, as well as the 51,000-acre Norse Peak Fire in 2017 near Mount Rainier, a fire that burned equal areas (about 25,000 acres) in both Eastern and Western Washington.
Compared to Western Washington’s 11 fires that scorched 50,000 acres since 1985, Eastern Washington has experienced 461 fires of over 1,000 acres each, burning a total of about 5.5 million acres — including some areas affected by fire more than once.
While nobody expects climate change to turn Western Washington into Eastern Washington, climate experts say the wetter side of the state may be transitioning out of a period of relatively small and low-intensity fires.
Perhaps aside from climate change yet adding to the concerns, recent weather conditions suggest that Western Washington may be moving out of a fairly long period of sustained dampness that began in the 1930s, according to Peterson.
“We do know that droughts were a lot more common — and lasted longer — prior to 1900,” Peterson said. “There is plenty of fuel out there. If we get back to a more normal drought cycle, we could expect to see those fuels dry out more often.”
Such conditions on top of climate change could lead to an increasing risk of a devastating wildfire across Western Washington, as well as an increasing number of smaller fires.
Predicting the future of wildfire in Western Washington is a real challenge, researchers say, because there are so few fires to be studied. A similar challenge confronts emergency managers who try to convince residents who live in wooded areas that they need to take steps to protect their families and property from wildfire.
“The general public seems to think that fire is not something they need to worry about,” said Kevin Zerbe, state mitigation strategist for the Washington Emergency Management Division. “It’s hard to communicate the level of risk, because there are few historical events we can point to.”
Among the 11 western states, Washington has the greatest amount of residential property in wooded areas, known as the wildland-urban interface, according to the state’s “Enhanced Hazard Mitigation Plan.”
It is not hard to find communities surrounded by nearby forests in Western Washington. Some look much like the town of Paradise, Calif., where in late 2018 a raging wildfire killed 86 people, destroyed 18,000 buildings and burned 150,000 acres. Most of Paradise became piles of ash that previously had been homes and personal belongings.
The blaze, named the Camp Fire, started from an arcing power line. Some experts say climate change contributed to the tinder-dry conditions that led to the most destructive fire in California history.
Northern California is different from Western Washington in many ways, Zerbe said, “but I don’t think it is entirely out of the question to have a fire like that in Western Washington. From a purely exposure standpoint, I think it is possible.”
Although well known for its rains, Western Washington has its moments when extreme drought and high heat come together to dry out the forests. Large amounts of fuel already exist. All that is needed is wind and something to spark a blaze — either a human source or a bolt of lightning.
Brian Potter, a research meteorologist for the U.S. Forest Service, says strong east winds associated with extreme fire conditions are often generated from a thermal trough, which develops along the coast beginning in Northern California and gradually extends into Western Washington. This low-pressure region brings strong and shifting winds up and over the Cascade Mountains, compressing the air in the Puget Sound lowlands and causing even hotter and dryer conditions. The trough is often associated with few clouds and no precipitation.
During fire season, California is generally known for having stronger and more sustained downslope winds than Western Washington. In Southern California, the winds are called Santa Ana winds, while in Northern California they are known as Diablo winds. In recent years, months of summer drought in California followed by extreme dry winds have led to unstoppable fires that have torched entire communities.
Because east winds play a powerful role in Western Washington wildfires, emergency managers would like to know how climate change could affect the frequency and force of the winds. Some climatologists speculate that warmer, more uniform temperatures might even weaken the winds to some degree. A new climate study, just getting underway, could help determine how future winds might alter the threat of a catastrophic wildfire.
The Great Forks Fire
In Washington state, strong east winds during the summer of 1951 were blamed for an inferno on the Olympic Peninsula that raced through 18 miles of forestland in a single day and led to the evacuation of hundreds of residents from the town of Forks.
“The fire made everyday heroes out of men and women who grabbed hoses and watered down houses and businesses,” wrote Mavis Amundson in her 2003 book “The Great Forks Fire.”
The initial fire was ignited on Aug. 6 by a steam-powered loggingtrain traveling through Olympic National Forest. It took dozens of firefighters, some with bulldozers, to bring the fire under control after it had burned 1,600 acres. Fire crews then spent weeks mopping up and putting out the hot spots before no signs of smoke remained. But the fire was not done.
The ominous east winds returned, stronger than ever, on Sept. 19. Somewhere in the burned debris a smoldering ember reignited the blaze, which moved so fast that fire crews had no defense.
“It blew over our heads and jumped ahead of us,” said Lew Evans, an assistant district ranger for the Forest Service, as quoted by Amundson, who went on to describe the fire that headed directly for Forks with flames hundreds of feet high. Although most people were evacuated, some remained in town where they scrambled to extinguish fires caused by falling embers.
“Loggers, sawmill workers, firefighters, shopkeepers, retirees and others helped save their town from the advancing fire,” Amundson wrote. “With little more than bulldozers, shovels, garden hoses, some outdated firefighting equipment and a pitiful water supply, these heroic townspeople helped hold back the forces of nature.”
And yet, despite their efforts, the townsfolk came to realize that they could not overcome the searing forces of the main fire as it neared the edge of town. Forks appeared to be doomed, Amundson wrote.
“Then, out of the west, came a fresh wind that blew in off the Pacific Ocean, cool and moist, and just strong enough to stop the fire’s advance. The town was spared.”
Remarkably, nobody was killed or seriously injured in the Great Forks Fire, which destroyed about two-dozen homes and burned through 33,000 acres of valuable timberland.
Next Month: Part 2
The worst fire year, our warming climate, and strategies for the future.
Christopher Dunagan is a senior writer at the Puget Sound Institute, which is affiliated with the University of Washington.