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“At least 14 Tarrant County residents died from extreme heat last summer … Of those who died from heat, at least eight cases included residents with no air conditioning, no working air conditioning, or who had their air conditioning turned off at the time of their death…” –The Fort Worth Star-Telegram, June 25, 2023
Air conditioners aren’t supposed to make that sound. The gray-white box in the window had always rattled, but this morning it has begun to grind. The grandmother puts her hand in front of the AC’s dust-covered gills, feels nothing but a weak, lukewarm breeze.
She thinks about calling her daughter, whose husband installed the unit in her trailer’s living room window the summer before. She shakes her head to herself: No, they have the baby; it’s a 40-minute drive; she’s a burden enough as it is. She doesn’t have internet in the trailer to see the day’s excessive heat warning. Her cell phone, another gift from her daughter, is dead more often than it’s not, and she can’t find the weather app on it half of the time, anyway.
But the grandmother has been hot before — prides herself, even, on her 68 Texan summers. Besides, she’s not planning anything strenuous today, which would elevate her chances of exertional, or “activity-induced,” heat stroke — the kind that makes the news for killing the young, fit, and healthy, like the California couple who were found dead on a trail with their 1-year-old baby and dog in 2021, or the stepfather who died last month while trying to rescue his 14-year-old stepson, who also died, while hiking in 119-degree weather in Texas’ Big Bend National Park. Like the dozens of promising high school and college athletes who collapse during training, games, and meets every year.
Or like the characters in longtime Outside correspondent and adventure historian Peter Stark’s cautionary tales about succumbing to the elements. Stark is perhaps best known for his second-person narrative about what it’s like to die from hypothermia, which recirculates every winter, but he has a particular, morbid fascination with heat strokes, having now written two different versions (a competitive cyclist dies in one; a hungover, hiking surfer is brought back from the brink in the other). “Out of all the research I’ve done into ways to die — or come close to dying — heat stroke is the one I found the scariest,” Stark told an Outside interviewer last year.
Like Stark’s characters, the grandmother is fictional and illustrative. Unlike Stark’s characters, she has not elected into risk. Exertional heat stroke is often described as “sporadic” because it is circumstantial; it is also less deadly since an athlete often begins to feel terrible, or collapses, before the point-of-no-return. “Classic” heat stroke, which results from unbearably high temperatures, “occurs in epidemic form” in the sense that it strikes the vulnerable at once and all together: the ill, the elderly, the unhoused, the bedridden, the prepubescent. Though heat-related mortality can be hard to pin down, by some estimates classic heat stroke is fatal in over 60% of intensive care cases — part of the reason extreme heat is credited as the deadliest weather phenomenon in the United States.
The grandmother goes to her sink and fills a glass of water. She looks out the window, at the tall grass growing alongside her neighbor’s trailer, and thinks about her grandbaby. Her trailer, which had stayed cool overnight before the AC conked out, has already begun to feel muggy, but she isn’t alarmed.
It is 97 degrees outside and getting hotter.
The human body is a contradiction: It can run a marathon in under two hours; it can scale the tallest mountain in the world; and it can survive episodes of extreme cold and starvation. At the same time, it is hilariously delicate: Only about 8.2 degrees separate our core body temperature of 98.6 from multi-organ dysfunction, which begins somewhere around 106 degrees, depending on the person and circumstances. Because this leaves little margin for error, our bodies spring into a well-rehearsed response when blood warmed by our environments at the surface of our skin makes its way to our brain, causing our hypothalamus to rustle through its bag of cooling tricks.
The grandmother’s body begins to run through them as the trailer’s temperature rises to 100 degrees, the point at which the body ceases to give off heat and begins to absorb it. Her hair follicles relax to release any trapped warm air against her skin. Her sweat glands are activated, and soon she’s covered in a light sheen that serves to transport heat away from her body via evaporation. Crucially, her blood vessels dilate so that the warmed blood can pass closer to the surface of the skin, where it will ideally be cooled by the heat pulling away from her body.
But as an older adult, the grandmother’s blood vessels don’t dilate as well as they used to. Her body strains to cool itself and her heart pumps harder. And despite her glass of water, the grandmother begins to notice she feels … off. She is experiencing some of the most common heat-related symptoms, the ones most of us are probably familiar with: Her stomach starts to cramp and she feels slightly nauseous as blood is redirected from her gut to the surface of her skin. She begins, also, to feel fatigued — unbeknownst to her, the drowsiness is because her body is running its cooling mechanisms full-blast, compensating for the broken AC.
But today, these systems are fighting an uphill battle. The trailer is humid, meaning the grandmother’s sweat isn’t evaporating as efficiently as it would in dry air. She has a sunburn from sitting on her lawn the day before, and her body is using water to try to heal it, leaving her with less liquid overall to sweat out. She can’t drink enough water to replenish what she’s lost, either, since the human body can only absorb, at max, one liter of water an hour, and those in extreme heat conditions can lose that or more in the same span of time.
Little does the grandmother know, either, that because it’s now over 95 degrees in her trailer, the fan she’s turned on is no longer having any cooling effect. Her core temperature tips toward 100 degrees.
Heat exhaustion sets in when the core body temperature is between 101°F and 104°F, as the grandmother’s is now. (Core body temperature cannot reliably be read on an oral thermometer, which is part of why the Centers for Disease Control and Prevention recommends watching for symptoms of heat exhaustion and heat stroke rather than taking your own measurements). In addition to her fatigue, she now feels dizzy. Her heart is pounding as her body tries to regulate itself; if she had a preexisting cardiac condition, she would be in even more danger than she already is. She stands up to get more water and feels a woosh of lightheadedness — a result of low pressure stemming from her dilated vessels — and her vision momentarily goes black. She nearly faints, but steadies herself with a hand on the back of a chair.
If a neighbor checked in on her, as the weathermen on TV are advising good samaritans do, they would see that the grandmother looks pale, that she’s grown irritable and unfocused. The neighbor might suggest she take a cold shower before asking her to come to their air-conditioned trailer, or a local cooling center, for the rest of the day. The most crucial thing, though, would be that she gets to a safe temperature, and fast, before her core hits 104, the threshold of heat stroke.
In her delirium, the grandmother thinks to take an Advil, foggily hoping a fever-reducer might help lower her core body temperature. And though the damage wrought by extreme heat is similar internally to that inflicted by a dangerously high fever, the response systems at play in each case are completely different. For extreme heat, there is no magic pill, no shut-off switch for how the grandmother is feeling aside from getting somewhere cool.
It might seem like a simple thing: getting somewhere cool. In this sense, classic heat stroke is, agonizingly, preventable. Though most Americans have air conditioning, over a quarter — 34 million households — “said they could not [financially] meet their energy needs at some point” during 2020, according to Energy Information Administration data. Of those who were struggling, 10% reported enduring dangerously high temperatures in their homes due to concerns about cost.
Because Americans typically do have access to AC, though, losing air conditioning for reasons beyond their control — say, due to grid failure, a localized blackout, or a mechanical issue — actually makes people more susceptible to dangerous heat-related illness, in part because acclimation has such a large role in how well we tolerate heat. The shock of living in climate-controlled rooms and suddenly finding yourself without one can be deadly.
The grandmother’s internal temperature is now over 105 degrees and still rising; she is well within the realm of heat stroke. Her pulse is rapid and now she is confused and agitated — she stumbles, directionless, toward her living room and collapses on the floor. Her body is rationing water away from vital organs, like her kidneys, which begin to shut down. Her brain is swollen. She cycles in and out of consciousness on the floor.
Her body is past the point of being able to bring its temperature back down by itself. A heat stroke victim may stop sweating. Their cells begin to die — the cerebellum, which controls motor functions, is one of the earliest parts of the brain to fail. They may have seizures or hallucinate or, nearing the end, feel a soaring sense of euphoria. Internally, the body is in freefall; by one estimate, there are 27 different pathways to death once heat stroke sets in, ranging from heart failure to the proteins that control blood clotting becoming overactive and cutting off flow to vital organs.
When the grandmother’s daughter arrives and calls the paramedics, it will only have been two hours since the grandmother first noticed her air conditioner’s grinding. “That’s part of what makes [heat stroke] so lethal,” Willamette Week wrote after the heat wave in the Pacific Northwest in 2021 killed an estimated 250 Americans: “You can go from feeling bothered by the heat to dead in 90 minutes.”
Victims of classic heat stroke are often elderly, often have pre-existing health conditions, often are socially isolated, and often are low-income. In an analysis of heat deaths in Multnomah County (where Portland, Oregon, is located) in 2021, The Washington Post found 61 percent of confirmed deaths were in areas with above-average poverty rates. In the same story, the reporters found that a “direct outreach” program in Philadelphia — which includes a “mass notification system,” “the number for a 24-hour hotline staffed by nurses [flashing] from one of the city’s tallest high rises,” and a 5,000-strong volunteer team that mobilizes “to check on high-risk neighbors” — saves an average of 45 lives per year.
If the grandmother had been younger, she might have been treated with “cold-water immersion,” which is one of the fastest and most reliable ways to address heat stroke. (Willamette Week reports Oregon paramedics resourcefully filled body bags with ice and had those suffering from heat stroke crawl inside). In the case of the elderly, though, it is advised to treat heat stroke with more easily tolerable cooling methods, like the application of ice packs and cold, wet gauze.
Either way, the outcome past the threshold of heat stroke is uncertain. As Stark, the master of the cautionary tale, writes, “A study reviewing 58 of the severe heat stroke victims [after a 1995 Chicago heat wave] found that 21 percent died in the hospital soon after admission, 28 percent died within a year, and all the remaining subjects experienced organ dysfunction and neurological impairments.”
But he sees a grim silver lining. “It could be a small measure of good fortune,” writes Stark, “that confusion, semiconsciousness, or coma overcome victims as they succumb to severe heatstroke.”
The laborer puts the nail gun down on the nearest cinderblock and sweeps the back of his hand across his brow, a portrait of I’m hot. Though the elimination of water breaks won’t go into effect until the fall, his employer has threatened to fire anyone who “slacks off” anyway, and the laborer needs this job. He watches for a moment as the heat makes strange shapes in the air above the new asphalt driveway. He thinks he might have a headache coming on.
There are five more hours to go. It’s 96 degrees out with 66% humidity.
And tomorrow will be another scorcher.
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Suburban streets, exploding pipes, and those Santa Ana winds, for starters.
A fire needs three things to burn: heat, fuel, and oxygen. The first is important: At some point this week, for a reason we have yet to discover and may never will, a piece of flammable material in Los Angeles County got hot enough to ignite. The last is essential: The resulting fires, which have now burned nearly 29,000 acres, are fanned by exceptionally powerful and dry Santa Ana winds.
But in the critical days ahead, it is that central ingredient that will preoccupy fire managers, emergency responders, and the public, who are watching their homes — wood-framed containers full of memories, primary documents, material wealth, sentimental heirlooms — transformed into raw fuel. “Grass is one fuel model; timber is another fuel model; brushes are another — there are dozens of fuel models,” Bobbie Scopa, a veteran firefighter and author of the memoir Both Sides of the Fire Line, told me. “But when a fire goes from the wildland into the urban interface, you’re now burning houses.”
This jump from chaparral shrubland into neighborhoods has frustrated firefighters’ efforts to gain an upper hand over the L.A. County fires. In the remote wilderness, firefighters can cut fire lines with axes, pulaskis, and shovels to contain the blaze. (A fire’s “containment” describes how much firefighters have encircled; 25% containment means a quarter of the fire perimeter is prevented from moving forward by manmade or natural fire breaks.)
Once a fire moves into an urban community and starts spreading house to house, however, as has already happened in Santa Monica, Pasadena, and other suburbs of Los Angeles, those strategies go out the window. A fire break starves a fire by introducing a gap in its fuel; it can be a cleared strip of vegetation, a river, or even a freeway. But you can’t just hack a fire break through a neighborhood. “Now you’re having to use big fire engines and spray lots of water,” Scopa said, compared to the wildlands where “we do a lot of firefighting without water.”
Water has already proven to be a significant issue in Los Angeles, where many hydrants near Palisades, the biggest of the five fires, had already gone dry by 3:00 a.m. Wednesday. “We’re fighting a wildfire with urban water systems, and that is really challenging,” Los Angeles Department of Water and Power CEO Janisse Quiñones explained in a news conference later that same day.
LADWP said it had filled its 114 water storage tanks before the fires started, but the city’s water supply was never intended to stop a 17,000-acre fire. The hydrants are “meant to put out a two-house fire, a one-house fire, or something like that,” Faith Kearns, a water and wildfire researcher at Arizona State University, told me. Additionally, homeowners sometimes leave their sprinklers on in the hopes that it will help protect their house, or try to fight fires with their own hoses. At a certain point, the system — just like the city personnel — becomes overwhelmed by the sheer magnitude of the unfolding disaster.
Making matters worse is the wind, which restricted some of the aerial support firefighters typically employ. As gusts slowed on Thursday, retardant and water drops were able to resume, helping firefighters in their efforts. (The Eaton Fire, while still technically 0% contained because there are no established fire lines, has “significantly stopped” growing, The New York Times reports). Still, firefighters don’t typically “paint” neighborhoods; the drops, which don’t put out fires entirely so much as suppress them enough that firefighters can fight them at close range, are a liability. Kearns, however, told me that “the winds were so high, they weren’t able to do the water drops that they normally do and that are an enormous part of all fire operations,” and that “certainly compounded the problems of the fire hydrants running dry.”
Firefighters’ priority isn’t saving structures, though. “Firefighters save lives first before they have to deal with fire,” Alexander Maranghides, a fire protection engineer at the National Institute of Standards and Technology and the author of an ongoing case study of the 2018 Camp fire in Paradise, California, told me. That can be an enormous and time-consuming task in a dense area like suburban Los Angeles, and counterintuitively lead to more areas burning down. Speaking specifically from his conclusions about the Camp fire, which was similarly a wildland-urban interface, or WUI fire, Maranghides added, “It is very, very challenging because as things deteriorate — you’re talking about downed power lines, smoke obstructing visibility, and you end up with burn-overs,” when a fire moves so quickly that it overtakes people or fire crews. “And now you have to go and rescue those civilians who are caught in those burn-overs.” Sometimes, that requires firefighters to do triage — and let blocks burn to save lives.
Perhaps most ominously, the problems don’t end once the fire is out. When a house burns down, it is often the case that its water pipes burst. (This also adds to the water shortage woes during the event.) But when firefighters are simultaneously pumping water out of other parts of the system, air can be sucked down into those open water pipes. And not just any air. “We’re not talking about forest smoke, which is bad; we’re talking about WUI smoke, which is bad plus,” Maranghides said, again referring to his research in Paradise. “It’s not just wood burning; it’s wood, plastics, heavy metals, computers, cars, batteries, everything. You don’t want to be breathing it, and you don’t want it going into your water system.”
Water infrastructure can be damaged in other ways, as well. Because fires are burning “so much hotter now,” Kearns told me, contamination can occur due to melting PVC piping, which releases benzene, a carcinogen. Watersheds and reservoirs are also in danger of extended contamination, particularly once rains finally do come and wash soot, silt, debris, and potentially toxic flame retardant into nearby streams.
But that’s a problem for the future. In the meantime, Los Angeles — and lots of it — continues to burn.
“I don’t care how many resources you have; when the fires are burning like they do when we have Santa Anas, there’s so little you can do,” Scopa said. “All you can do is try to protect the people and get the people out, and try to keep your firefighters safe.”
Plus 3 more outstanding questions about this ongoing emergency.
As Los Angeles continued to battle multiple big blazes ripping through some of the most beloved (and expensive) areas of the city on Thursday, a question lingered in the background: What caused the fires in the first place?
Though fires are less common in California during this time of the year, they aren’t unheard of. In early December 2017, power lines sparked the Thomas Fire near Ventura, California, which burned through to mid-January. At the time it was the largest fire in the state since at least the 1930s. Now it’s the ninth-largest. Although that fire was in a more rural area, it ignited for many of the same reasons we’re seeing fires this week.
Read on for everything we know so far about how the fires started.
Five major fires started during the Santa Ana wind event this week:
Officials have not made any statements about the cause of any of the fires yet.
On Thursday morning, Edward Nordskog, a retired fire investigator from the Los Angeles Sheriff’s Department, told me it was unlikely they had even begun looking into the root of the biggest and most destructive of the fires in the Pacific Palisades. “They don't start an investigation until it's safe to go into the area where the fire started, and it just hasn't been safe until probably today,” he said.
It can take years to determine the cause of a fire. Investigators did not pinpoint the cause of the Thomas Fire until March 2019, more than two years after it started.
But Nordskog doesn’t think it will take very long this time. It’s easier to narrow down the possibilities for an urban fire because there are typically both witnesses and surveillance footage, he told me. He said the most common causes of wildfires in Los Angeles are power lines and those started by unhoused people. They can also be caused by sparks from vehicles or equipment.
At about 27,000 acres burned, these fires are unlikely to make the charts for the largest in California history. But because they are burning in urban, densely populated, and expensive areas, they could be some of the most devastating. With an estimated 2,000 structures damaged so far, the Eaton and Palisades fires are likely to make the list for most destructive wildfire events in the state.
And they will certainly be at the top for costliest. The Palisades Fire has already been declared a likely contender for the most expensive wildfire in U.S. history. It has destroyed more than 1,000 structures in some of the most expensive zip codes in the country. Between that and the Eaton Fire, Accuweather estimates the damages could reach $57 billion.
While we don’t know the root causes of the ignitions, several factors came together to create perfect fire conditions in Southern California this week.
First, there’s the Santa Ana winds, an annual phenomenon in Southern California, when very dry, high-pressure air gets trapped in the Great Basin and begins escaping westward through mountain passes to lower-pressure areas along the coast. Most of the time, the wind in Los Angeles blows eastward from the ocean, but during a Santa Ana event, it changes direction, picking up speed as it rushes toward the sea.
Jon Keeley, a research scientist with the US Geological Survey and an adjunct professor at the University of California, Los Angeles told me that Santa Ana winds typically blow at maybe 30 to 40 miles per hour, while the winds this week hit upwards of 60 to 70 miles per hour. “More severe than is normal, but not unique,” he said. “We had similar severe winds in 2017 with the Thomas Fire.”
Second, Southern California is currently in the midst of extreme drought. Winter is typically a rainier season, but Los Angeles has seen less than half an inch of rain since July. That means that all the shrubland vegetation in the area is bone-dry. Again, Keeley said, this was not usual, but not unique. Some years are drier than others.
These fires were also not a question of fuel management, Keeley told me. “The fuels are not really the issue in these big fires. It's the extreme winds,” he said. “You can do prescription burning in chaparral and have essentially no impact on Santa Ana wind-driven fires.” As far as he can tell, based on information from CalFire, the Eaton Fire started on an urban street.
While it’s likely that climate change played a role in amplifying the drought, it’s hard to say how big a factor it was. Patrick Brown, a climate scientist at the Breakthrough Institute and adjunct professor at Johns Hopkins University, published a long post on X outlining the factors contributing to the fires, including a chart of historic rainfall during the winter in Los Angeles that shows oscillations between very wet and very dry years over the past eight decades. But climate change is expected to make dry years drier in Los Angeles. “The LA area is about 3°C warmer than it would be in preindustrial conditions, which (all else being equal) works to dry fuels and makes fires more intense,” Brown wrote.
And more of this week’s top renewable energy fights across the country.
1. Otsego County, Michigan – The Mitten State is proving just how hard it can be to build a solar project in wooded areas. Especially once Fox News gets involved.
2. Atlantic County, New Jersey – Opponents of offshore wind in Atlantic City are trying to undo an ordinance allowing construction of transmission cables that would connect the Atlantic Shores offshore wind project to the grid.
3. Benton County, Washington – Sorry Scout Clean Energy, but the Yakima Nation is coming for Horse Heaven.
Here’s what else we’re watching right now…
In Connecticut, officials have withdrawn from Vineyard Wind 2 — leading to the project being indefinitely shelved.
In Indiana, Invenergy just got a rejection from Marshall County for special use of agricultural lands.
In Kansas, residents in Dickinson County are filing legal action against county commissioners who approved Enel’s Hope Ridge wind project.
In Kentucky, a solar project was actually approved for once – this time for the East Kentucky Power Cooperative.
In North Carolina, Davidson County is getting a solar moratorium.
In Pennsylvania, the town of Unity rejected a solar project. Elsewhere in the state, the developer of the Newton 1 solar project is appealing their denial.
In South Carolina, a state appeals court has upheld the rejection of a 2,300 acre solar project proposed by Coastal Pine Solar.
In Washington State, Yakima County looks like it’ll keep its solar moratorium in place.