From NOAA (Michon Scott):
On December 30, 2021, the Marshall Fire ripped through suburban neighborhoods on the west side of the Denver-Boulder metropolitan area. Spread by high winds and fueled by dry conditions, the wildfire left two people presumed dead, burned more than 6,000 acres, and destroyed more than 1,000 homes, according to news reports.
High winds, even with occasional hurricane-force gusts, are not unusual in this “foothills” region, where the eastern prairies meet the Rockies. The day of the windstorm, atmospheric pressure dropped sharply east of the Rockies, and strong downslope winds followed. At the base of the foothills west of Denver, wind gusts reached 100 miles per hour.
But winds alone didn’t account for the destruction. In the months leading up to this wildfire, climate conditions set the stage for a disaster. The spring of 2021 brought unusually wet conditions, encouraging vigorous plant growth. Starting in June, though, precipitation levels fell below average, and remained well below average for the rest of the year.
Although snow fell in the Rocky Mountains to the west, the Denver-Boulder area remained dry. Denver recorded its first measurable snow of the season—just 0.3 inches—on December 10, 2021. It was the latest first-snowfall date on record, and after that light snowstorm, dry conditions resumed.
As moisture remained elusive, temperatures remained unusually warm, soaring more than 20 degrees F above average early in December 2021 and hitting 10 or more degrees above average many days throughout the month.
Where the wildfire struck—in the southeastern corner of Boulder County, Colorado—unusually dry conditions took hold in September. By early October, dry conditions had worsened into drought. By late December, drought conditions were extreme.
As of January 4, 2022, the cause of the fire was still under investigation, but its origin had been pinpointed to an area west of Marshall Lake. Once ignited, the fire spread with ferocious speed, charging toward the north and east. The warm, dry conditions in the months before the Marshall Fire broke out supplied the fire with plentiful fuel. Winds carried embers across paved areas, dropping those embers on parched vegetation that was ready to burn, along with buildings and vehicles.
Unable to fight the flames amid hurricane-force gusts, first responders focused on evacuation. Residents, diners, and shoppers were caught off guard, some forced to flee at a moment’s notice. Besides seeing and smelling smoke and flames, area residents heard multiple booms—potentially resulting from the fire reaching propane tanks. Only when the winds slowed late in the evening of December 30 could firefighters begin extinguishing the flames.
Days after the fire, two people remained missing and were presumed deceased. The tally of homes damaged stood at 149. The tally of homes burned to the ground stood at 1,084. Dozens of businesses had also been damaged or destroyed.
In terms of acreage burned, the Marshall Fire was dwarfed by many other blazes, including the state’s three largest wildfires, which all struck within weeks of each other in 2020: Cameron Peak, East Troublesome, and Pine Gulch. But in terms of residences lost, the Marshall Fire was the most destructive in Colorado history. The Marshall Fire did not strike in a sparsely populated, mountainous region. The fire burned a densely populated suburban area where most residents had not previously considered wildfire a threat.
Starting on the afternoon of December 31—one day after the fire—significant snow finally fell in the Denver-Boulder metro area.
9NEWS. (2021, December 30). Costco evacuation due to Marshall Fire. Accessed January 4, 2021.
Colorado Division of Fire Prevention and Control. Historical wildfire information. Accessed January 4, 2022.
Denver7 News. (2021, December 30). Better weather conditions are expected Friday. [December 31, 2021]. Accessed January 4, 2022.
Denver7 News. (2021, December 10). Denver celebrates 0.3 inches of snow — its first measurable snowfall of the season. Accessed January 4, 2022.
Fish, S., Paul, J. (2022, January 1). MAP: These are the 991 structures destroyed and 127 damaged in the Marshall fire. The Colorado Sun. Accessed January 4, 2022.
Flynn, C. (2022, January 6). Nearly 1,100 homes destroyed in Marshall Fire, valued at over $500 million. KDVR. Accessed January 6, 2022.
Heberton, B. (2022, January 1). Colorado’s most destructive fire a result of extreme winds, expanding wildland-urban interface, and a stressed climate. Weather5280. Accessed January 4, 2022.
National Interagency Fire Center. Map of the Marshall Fire burn area. Accessed January 4, 2022.
National Weather Service. High Winds and Marshall Fire on December 30, 2021. Accessed January 4, 2022.
U.S. Drought Monitor. Accessed January 4, 2022.
WXChasing. (2021, December 31). Louisville, Colo: First light shows destruction from Marshall Fire- Drone 4k. Accessed January 4, 2022.
La Niña, climate change, and bad luck: the climate context of Colorado’s Marshall Fire
From NOAA (Rebecca Lindsey):
As we wrote last week, the Marshall Fire in northern Colorado on December 30, 2021, was a devastating finale to a record-warm, record-dry fall in the state’s eastern plains and foothills. Several experts interviewed for this story, including Deputy Colorado State Climatologist Becky Bolinger, said that, because the risk of drought and warm extremes are increasing as a result of human-caused global warming, it’s reasonable to think that global warming contributed in some way to the devastation caused by the Marshall Fire.
But they also said that as a winter grass fire, the Marshall Fire is different from the warm-season forest fires in the West, which scientists have strongly linked to global warming. Namely, winter fires are much more wind-driven than summer fires, and there’s no evidence that the fierce winds that drove the fire that day were anything other than natural, if extreme, variability. Likewise, there’s no strong evidence to link the excessively wet spring (which built up the vegetation) to climate change.
The lack of snow is a final complicated piece. “December is one of the months that has warmed the most in this area,” said Bolinger, “but there has been no long-term decline in total December snowfall.” That makes it hard to know what to make of the record-low snowfall in the area through December, which intensified the drought.
“This was a complex event,” said Bolinger. “Some factors probably are connected to climate change and others probably aren’t.”
This is not a final answer
All extreme events have more than one cause. So Did global warming cause that event? isn’t a yes or no question. The best scientists can do is figure out whether human-caused global warming played a role, and if so, how big a role. Scientists have a name for the process of figuring that out: extreme event attribution.
Attribution research generally has two parts: analysis of historical data and climate model experiments. Experts check to see if there have been changes over time in the extreme events themselves or in the weather patterns that produce them. They also identify climate models that are capable of simulating that type of event, and use them to create two virtual worlds: one with and one without increased greenhouse gases. They compare the frequency and intensity of extreme events between the two simulated worlds to estimate the influence of global warming.
That kind of thing takes time, of course. The more unusual or complex the event, the more difficult an attribution analysis is to conduct. That’s likely to be the case with the Marshall Fire, which arose from a rare mash-up of extreme weather and climate factors that each were capable of raising the fire risk individually. Until a formal attribution study is completed, any explanations of the event should be thought of as these experts’ educated guesses, not a final answer.
What we know about fires in the West
According to the fourth National Climate Assessment, “Increased heat, drought, and insect outbreaks, all linked to climate change, have increased wildfires” in the U.S. Southwest, defined in the report as the states of California, Nevada, Utah, Arizona, Colorado, and New Mexico. A recent analysis funded by NOAA’s Climate Program Office concluded that human-caused global warming was the leading cause of the rapid increase in Western wildfires between the end of the 20th century (1984-2000) and the beginning of the 21st (2000-2018). A NOAA Drought Task Force report also concluded that global warming played a role in the severity of the ongoing 2020-21 Southwest drought.
Modeling experiments have found that warming due to increasing greenhouse gases is going to dramatically increase the risk of very large fires in parts of the West over the next 50 years. Fire seasons are getting longer, a trend that is likely to continue, turning fire-fighting into more of a year-round activity in places.
Colorado’s record-setting Cameron Peak Fire, which ignited in mid-August 2020, may be a preview of that. In early September 2020, 8-14 inches of snow fell on the ~100,000-acre fire without extinguishing it. The blaze went on to double in size—setting a new record for the state’s largest fire—by the end of October. Despite a second significant snow event in late October, the fire was not fully contained until early December.
What’s different about the Marshall Fire
The main reason experts gave for being somewhat cautious about using all that research to unequivocally link the Marshall Fire to global warming was that most of it has focused on warm-season forest fires. And while all fires have some ingredients in common, winter grass fires like the Marshall are different in ways that complicate the connection.
“A difference between warm and cold season for fire in places like California and Colorado is that the cold season generally is more windy, so fire behavior could be more complex,” wrote Yizhou Zhuang via email. Zhuang is a climate researcher at University of California – Los Angeles whose work connected global warming to the rapid increase in Western fires in recent decades. He and his colleagues found that the increase was due to increases in how “thirsty” the summer atmosphere is for soil and plant moisture —what experts call the vapor pressure deficit, or “VPD” for short. Rising temperatures are increasing those deficits.
But for the Marshall fire, Zhuang wrote, “preliminary data actually showed that the VPD condition on the day when the fire started (12/30/2021) was high, although not extreme (~75th percentile); the strong wind condition (~99th percentile) could be more important for the fire spread.”
Climate researcher Rong Fu, one of Zhuang’s collaborators, agreed that natural weather variability may play a bigger role in winter fires than it does in summer fires. Having said that, she wrote in an email, “I believe the vapor pressure deficits that would have occurred during the warm season and the 2020/21 drought contributed to the flammability and amount of dead and dry plants, which provided a perfect bio-fuel for the Marshall fire.”
In other words, the influence of human-caused global warming on the Marshall Fire could be less than it would be on a typical summer forest fire, but still play a role. That’s the perspective of Deputy State Climatologist for Colorado, Becky Bolinger.
“It’s true,” she said, “that the Marshall Fire is a bit different than the warm-season forest fires that are the basis for much of the research connecting Western fire activity and global warming. Still, big winter grassfires in the state have historically been connected to warmth and drought, just like mountain fires. We were having a record drought; global warming is increasing the frequency of droughts. We were having record warmth; global warming is increasing the frequency of heat extremes. It seems pretty safe to conclude that global warming trends played at least some role in setting this up.”
While agreeing that less is known about the connection between winter grassfires and global warming, western climate and hydrology expert John Abatzoglou, of University of California Merced, commented via email, “A warming climate may increase the likelihood of these events by keeping fuels dry later into the year.” Combined with a delayed onset of snowfall, as happened this year, the dry fuels “would prime the system to have fires that spread rapidly and resist control” during the winter downslope wind season.
Abatzoglou shared the results of modeling experiments his team has done that compare past, current, and future risk of very high fire danger days across the U.S. The map below is based on the impact of a high greenhouse gas emissions pathway on the moisture of 100-hour fuels—dead vegetation between 1 and 3 inches in diameter, which takes about 100 hours to respond to changes in weather conditions.
Between the 1971-2000 reference period and the present (2010-2039), the models projected a small increase—basically going from 2 days to 3 days—in the number of winter days with 100-hour fuel moisture in the bottom ten percent of the record. Aside from the human structures, most, though not all, of the places that burned in the Marshall fire were likely 1 and 10-hr fuels (grasses and other plants), which respond to weather changes more quickly, so the impacts could be a bit different. But a similar analysis of the impact of warming on 10-hour fuels around in the area around Boulder found a similar pattern. Models suggest human-caused climate change has increased the number of December days with high fire risk.
Abatzoglou concluded, “Drier fuels in the downslope wind season would up the odds of significant fire weather conditions.”
Bolinger made a similar point. “Historically, our warm, dry season and our windy season don’t overlap,” she said. “The fall warming trend may cause the two to seasons to overlap more often, which would make cold-season fires a more frequent threat.”
What about La Niña?
In terms of natural influences, Bolinger added that La Niña—the cool phase of the El Niño-Southern Oscillation climate pattern in the tropical Pacific—may also have played a role. “The typical U.S. fall and winter climate signal for La Niña is wet in the Pacific Northwest and dry in the Southwest. Northern Colorado is right on the boundary between those two strong signals, which means a little shift either way can bring us opposite results. Overall, though, dry falls are slightly more common than wet,” Bolinger said, “which means the ongoing La Niña might also have played a role in the current drought.”
Strategies such as controlled or “prescribed” fire to reduce fire fuels, stringent building codes requiring fire-resistant materials, and vegetation-limited buffer-zones around homes and businesses can make communities more resilient to wildfire. Yet in many places, such fire-resilient adaptations are not adopted, even following a devastating fire. Meanwhile, the country is spending more than $2 billion a year to fight wildfires, according to the National Interagency Fire Center.
To some experts, these trends are evidence that the West’s default fire strategy—a combination of fire suppression at the wildland-urban interface and fuels reduction in national forests and other public lands—is no match for the current and future fire risk. Instead, they say, we need “a new paradigm that hinges on the critical need to adapt to inevitably more fire in the West in the coming decades.”
Among their suggestions is greater use of prescribed (low-intensity) fire, targeting fuel reductions like tree thinning to areas near homes and communities, encouraging community-focused fire planning, and shifting more of the costs of fire-fighting from federal land agencies like the U.S. Forest Service to state, local, and private jurisdictions where the decisions about whether and how to build in fire-risk areas are being made.