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Maybe you’re reading this in a downpour. Perhaps you’re reading it because you have questions about the upcoming hurricane season. Or maybe you’re reading it because you’re one of the 150 million Americans enduring record-breaking temperatures in this week’s heat dome.
Whatever the reason, you have a question: Is this climate change?
There’s an old maxim — that, like many things, is often dubiously attributed to Mark Twain — that goes something like, “Climate is what you expect and weather is what you get.” Weather refers to the event itself, while climate refers to the trends (averaged over 30 years or more, usually) that might make such an event more or less likely.
Climate change is almost always an exacerbating factor in the case of something like a heat wave or a heat dome. In other situations, the picture is far more complicated and uncertain. It can take years to understand if and how climate change made an extreme weather event more likely, and while organizations like World Weather Attribution work hard to provide quick and accurate estimations, getting the science wrong can fuel climate skepticism and bolster deniers’ arguments. While it might be tempting to pin all extreme weather on climate change, the truth is, not all of it is.
Still, we do know a lot about how climate change influences the weather — and we’re always learning more. While this guide is far from the be-all and end-all of attribution and should be referred to with caveats, here is what we know about how climate change is shaping the extreme weather we see today.
“When you’re looking at heat extremes, there is almost always a climate change signal,” Clair Barnes, a research associate with World Weather Attribution, told me. “I don’t think there’s ever not been a climate change signal since I’ve been doing it in the last couple of years.”
As the planet warms, local temperatures respond everywhere. There are not as many complicating variables in this relationship as there are with something like drought. “With heat waves, it’s the same answer every time: It got hotter because it’s got hotter,” Barnes said.
The Intergovernmental Panel on Climate Change has found that the kind of heat waves that would have occurred once in a decade before the Industrial Revolution now occur almost three times more frequently and are 1.2 degrees Celsius (or 2.2 degrees Fahrenheit) warmer. The most extreme examples — like the 2021 heat dome over the Pacific Northwest — appear to have been possible only because of warming caused by greenhouse gas emissions. Additionally, about 37% of global heat-related deaths, which amount to tens of thousands of deaths per year, are attributable to climate change.
There have, of course, always been heat waves. But it is with high confidence that scientists say they are hotter and last longer now than they would otherwise because of climate change.
Did climate change do it? It is “virtually certain” that heat waves are more frequent and hotter than they otherwise would be because of climate change.
WWA doesn’t specifically study wildfires since they aren’t technically “weather” (though once they form, they can make their own). Instead, the organization studies the conditions that make a fire more likely. In the American West, this deadly combo usually involves high pressure, extremely dry air, and some wind.
Globally, burned areas decreased between 1998 and 2015, but that isn’t because fire-weather conditions are improving — rather, regional leaders have gotten better at things like land use and fire management. Fire weather, meanwhile, is increasing and lasting longer due to climate change. In particular, hotter temperatures — especially hotter overnight temperatures — make it more difficult to combat the fires that do ignite. (Most fires in the U.S. start due to human negligence or arson, rather than by natural causes such as lightning strikes.)
This is especially the case in California, where 10 of the state’s largest fires have occurred in the past two decades, with five in 2020 alone; a 2023 National Integrated Drought Information System-funded study further found a 320% increase in burned areas in the state between 1996 and 2021 due to contributions of human-caused climate change, with that number expected to grow in the coming decades.
On average, wildfire weather season lengthened by two weeks around the globe from 1979 to 2019. The IPCC has medium confidence in the claim that fire weather has become more probable in the U.S., Europe, Australia, and parts of Europe over the past century, and high confidence that fire weather will increase regionally due to global warming in the coming years.
Did climate change do it? Climate change has almost certainly exacerbated the heat, humidity, and drought conditions necessary for wildfires to start. The actual ignition of the fire is frequently human-caused, however, and complicating variables such as local vegetation, forest management, and land use can also muddle the picture.
Tropical cyclones are large and complicated storm systems. Ocean temperatures, the El Niño-Southern Oscillation, wind shear, barometric pressure, atmospheric moisture, the shape of the continental shelf, emergency preparedness measures, and pure luck all affect how destructive a given storm might be — when or if it makes landfall. Climate change can put a thumb on the scale, but it is far from a lone actor.
Hurricanes — the strongest manifestation of a tropical cyclone — essentially work by transferring heat from the ocean into wind energy. Because the ocean absorbs excess heat from the warming atmosphere, scientists expect to see more “major” hurricanes of Category 3 or above in the coming years.
The storms aren’t just getting more powerful, though. Because of the interaction between ocean heat and energy in a hurricane, the storms also intensify more rapidly and are “more than twice as likely to strengthen from a weak Category 1 hurricane to a major Category 3 or stronger hurricane in a 24-hour period than they were between 1970 and 1990,” according to new research published last year.
WWA says it cannot attribute the intensification of any individual storm to climate change due to relatively limited modeling so far, so the organization instead looks at how climate change may have amplified associated rainfall and storm surges. Rainfall and flooding are, in fact, more deadly than high wind speeds in hurricanes, and both are understood to be increasing because of climate change. Put simply, a warmer atmosphere can hold more water, which means worse deluges. Researchers linked extreme rainfall during Hurricanes Katrina, Maria, and Irma to climate change; Hurricane Harvey, which flooded up to 50% of the properties in Harris County, Texas, when it made landfall in 2017, had a rainfall total 15% to 38% greater than it would have been in a pre-industrial world, researchers found. Additionally, rising sea levels caused by climate change will worsen coastal flooding during such events.
However, “trends indicate no significant change in the frequency of tropical cyclones globally,” according to the IPCC. That is, there aren’t more hurricanes; the ones that form are just more likely to become major hurricanes. Scientists understand far less about what climate change means for the smaller Category 1 or 2 storms, or if it will impact the diameter of the storms that do form.
Did climate change do it? The greenhouse effect is making the atmosphere warmer, and in a warmer climate, we’d expect to see more major hurricanes of Category 3 and above. Evidence also points to hurricanes intensifying much more rapidly in today’s climate than in the past. Climate does not seem to play a role in the overall number of storms, though, and other critical factors like the path of a storm and the emergency preparedness of a given community have a significant impact on the potential loss of life but aren’t linked to a warmer atmosphere. Hurricanes are complicated events and there is still much more research to be done in understanding how exactly they’re impacted by climate change.
In the winter, your skin might feel dry, and your lips might chap; in the summer, many parts of the country feel sticky and swampy. This is simple, observable physics: Cold air holds less moisture, and warm air holds more. The “Clausius-Clapeyron” relation, as it is known, tells us that in 1 degree C warmer air, there is 7% more moisture. All that moisture has to go somewhere, so quite literally, when it rains, it pours. (That is, when and where it rains: WWA notes that “an attribution study in northern Europe found that human influence has so far had little effect on the atmospheric circulation that caused a severe rainfall event.”)
Like heat, the relationship between warm air and rainfall is well understood, which is why the IPCC is highly confident in the attributable influence of climate change on extreme rain. While it may seem confusing that both droughts and intense rainfall are symptoms of climate change, the warming atmosphere seems to increase precipitation variability, making events on the extreme margins more likely and more frequent.
Increased precipitation can have counterintuitive results, though. Rain occurring over fewer overall days due to bursts of extreme rainfall, for example, can actually worsen droughts. And while it might seem like more water in the atmosphere would mean snowier winters, that’s only true in certain places. Because it’s also warmer, snowfall is declining globally while winters are getting wetter — and as a result, probably more miserable.
But what does “more rain” really mean? Rain on its own isn’t necessarily bad, but when it overwhelms urban infrastructure or threatens roads and houses, it can quickly become deadly. Flooding, of course, is often the result of extreme rain, but “the signal in the rainfall is not necessarily correlated to the magnitude of the floods because there are other factors that turn rain into a flood,” Barnes, the research associate with WWA, told me, citing variables such as land use, water management, urban drainage, and other physical elements of a landscape.
Landslides, likewise, are caused by everything from volcanic eruptions to human construction, but rain is often a factor (climate-linked phenomena like wildfires and thawing permafrost also contribute to landslides). The IPCC writes with “high confidence” that landslides, along with floods and water availability, “have the potential to lead to severe consequences for people, infrastructure, and the economy in most mountain regions.”
Did climate change do it? More extreme rainfall is consistent with our understanding of climate change’s effects. Many other local, physical factors can compound or mitigate disasters like floods and mudslides, however.
When I spoke with Barnes, of WWA, she told me, “It’s really easy to define a heat wave. You just go, ‘It was hot.’” Droughts, not so much. For one thing, you have to define the time span you’re looking at. There are also different kinds of drought: meteorological, when there hasn’t been enough rain; hydrological, when rivers are low possibly because something else is diverting water from the natural cycle; and agricultural, when there is not enough water specifically for crops. Like flooding, many different infrastructural and physical factors go into exacerbating or even creating various kinds of droughts.
Drought as we mean it here, though, is a question of soil moisture, Barnes told me. “That’s really hard to get data on,” she said, “and we don’t necessarily understand the feedback mechanisms affecting that as well as we understand heat waves.” As recently as 2013, the IPCC had only low confidence that trends in drought could be attributed to climate change.
We have a better understanding of how drought and climate change interact now, including how higher temperatures drive evaporation and cut into snowpack, leading to less meltwater in rivers. The IPCC’s most recent report concluded that “even relatively small incremental increases in global warming (+0.5C) cause a worsening of droughts in some regions.” The IPCC also has high confidence that “more regions are affected by increases in agricultural and ecological droughts with increasing global warming.”
WWA’s attribution studies have, however, found examples of droughts that have no connection to climate change. The organization flags that it has the highest confidence in the climate affecting droughts in the Mediterranean, southern Africa, central and eastern Asia, southern Australia, and western North America and lower confidence in central and west Africa, western and central Europe, northeast South America, and New Zealand.
Did climate change do it? Maybe. Some droughts have a strong climate signal — California’s, for example. Still, researchers remain cautious about attribution for these complicated events due in part to their significant regional variability.
Tornadoes are extremely difficult to study. Compared to droughts, which can last years, tornadoes occupy a teeny tiny area and last for just a blip in time. They “wouldn’t even register” on the models WWA uses for its attribution studies, Barnes said. “It would probably look like a slightly raised average wind speed.” The IPCC, for its part, has only “low confidence” in a connection between climate change and “severe convective storms” like tornadoes, in part due to the “short length of high-quality data records.”
But we are learning more every day. This spring, researchers posited that Tornado Alley is moving east and “away from the warm season, especially the summer, and toward the cold season.” Though it’s not entirely clear why this is happening, one theory is that it relates to how climate change is affecting regional seasonality: winters and nights are becoming warmer in certain areas, and thus more conducive to tornado formation, while others are becoming too hot for storms to form during the normal season.
Did climate change do it? Researchers aren’t entirely sure but there doesn’t appear to be a correlation between tornado formation and climate change. Still, warmer temperatures potentially make certain areas more or less prone to tornadoes than they were in the past.
We say “it was a dark and stormy night” because “it was a severe convective storm” doesn’t have the same ring. But an SCS — which forms when warm, moist air rises into colder air — is the most common and most damaging weather phenomenon in the United States. You probably just call it a thunderstorm.
Severe convective storms cause many localized events that we think of as “weather,” including heavy rainfall, high winds, tornadoes, hail, thunder, and lightning. Because heat and moisture are necessary ingredients for these kinds of storms, and because the atmosphere is getting both warmer and wetter, climate models “consistently” and confidently predict an “increase in the frequency of severe thunderstorms,” the IPCC notes — but, “there is low confidence in the details of the projected increase.” Trends remain poorly studied and highly regionally dependent; in the United States, for example, there is still no evidence of a “significant increase in convective storms, and hail and severe thunderstorms.” Still, other research suggests that for every 1.8 degree F of warming, the conditions favorable to severe convective storms will increase in frequency by up to 20%.
Hail forms during severe convective storms when the hot, moist air rises to a region of the atmosphere where it is cold enough to freeze. Like thunderstorms more generally, data is fairly limited on hail, making it difficult to study long-term trends (most climate models also do not look directly at hail, studying convective storms more broadly instead). However, it’s been hypothesized that climate change could create larger and more destructive hail in the future; if thunderstorm updrafts grow stronger, as projected, then they could hold hail at freezing high altitudes for longer, allowing individual hailstones to grow larger before falling back to Earth. One study even suggested that with continued warming, there could be a 145% increase in “significant severe hail” measuring at least 2 inches in diameter — that is, a little smaller than a tennis ball.
Did climate change do it? Everything we know about thunderstorms suggests that a warmer, wetter atmosphere will mean severe convection storms become both more frequent and more intense. But there is still very little available data to track the long-term trends, so attributing any one storm to climate change would be nearly impossible.
Just as virtually all heat waves worldwide are worsened by climate change, “nearly every instance of extreme cold across the world has decreased in likelihood,” according to the WWA. While the organization has run attribution studies on “a few” heavy snowfall events, it has either found no link to climate change or has been unable to state a conclusion confidently. On the other hand, the loss of snow cover, permafrost, Arctic sea ice, and glaciers has a high-confidence link to human-caused climate change in the IPCC report.
Just because climate change makes extreme cold and snowstorms less likely does not mean they won’t happen. Research published in Nature earlier this year suggests climate change could bring more snow to certain places, as extremely cold parts of the world warm to snow-friendly temperatures, and increased precipitation from a warmer atmosphere results in more flurries. Parts of Siberia and the northern Great Plains are even experiencing a deepening snowpack.
Did climate change do it? Probably not — though there are notable exceptions.
An earthquake is usually caused by the release of energy when two tectonic plates suddenly slip past each other (though they can also be caused by fossil fuel extraction). But before you dismiss earthquakes as having no connection to climate change, there is one place where there could be a link: water.
As Emily Pontecorvo wrote for Heatmap this spring, “Changes in surface water, whether because of heavy rain, snow, or drought, could either increase or relieve stress on geologic faults, causing them to shift.” Admittedly, even if there is a relationship between climate change, water, and earthquakes, it appears to be small — so small that humans probably can’t feel any resulting quakes.
Did climate change do it? It’s highly unlikely.
Earlier this year, extreme turbulence on a Singapore-bound flight from London killed one person and injured at least 20 others. While such events remain rare — the U.S. National Transportation Safety Board recorded just 101 serious injuries caused by turbulence on millions of flights between 2013 and 2022 — extreme turbulence appears to be increasing, potentially because of climate change.
According to one study, severe turbulence is up 55% between 1979 and 2020, seemingly due to an increase in wind shear at high altitudes caused by the temperature contrast between the equator and the North Pole. (This relationship is a little bit complicated, but essentially, at higher altitudes, the temperature over the pole has been declining due to rapid Arctic temperature changes even as it’s increased at the equator; lower in the troposphere, the opposite is happening). Other studies have similarly shown that doubling the concentration of carbon dioxide in the atmosphere could increase moderate-to-severe turbulence by as much as 127%.
Data, however, is limited and fairly subjective, leading to some skepticism in the scientific community and inaccurate dismissals by climate-change deniers. As with many complex weather phenomena, our understanding of how climate change interacts with turbulence will likely grow in the coming years as the field of research develops.
Did climate change do it? Potentially in some cases, but there is still much to learn about the connection between the two.
Desertification differs from drought in that it describes a decline in soil fertility, water, and plant life to the point of total “land degradation.” (In contrast, land can become productive again after a drought.) Like other compound disasters, desertification results from natural processes, climatic conditions, and land management practices such as grazing and deforestation.
According to the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services, land degradation is “almost always” the result of these “multiple interacting causes,” and the warming climate certainly isn’t helping. Heat stress can kill off vegetation, making landscapes more prone to desertification, as well as drive aridification.
In the resulting drylands — which comprise about 46% of global land area — you can expect dust storms (also known as haboobs), and sand storms resulting from the wind kicking up loose soils. While there have always been sand storms, one study suggests that climate change is one of the critical drivers of global annual dust emissions increasing by 25% between the late 19th century and today.
However, “climate change impacts on dust and sand storm activity remain a critical gap,” writes the IPCC, and more research is desperately needed to address this. By the UN’s estimate, dust storms were associated with the deaths of 402,000 people in 2005. As many as 951 million people, mainly in South Asia, Central Asia, West Africa, and East Asia, could be vulnerable to the impacts of desertification if climate change continues.
Did climate change do it? It was potentially a factor, but we have lots more to learn.
Are locust swarms technically “weather”? Not really. But so long as we’re on the topic of weather events of Biblical proportions, locust swarms might as well be addressed, too.
And the answer may surprise you: Climate appears to be a driver of locust swarms, which threaten food security and exacerbate famines throughout Africa, the Middle East, and South Asia. Locusts prefer “arid areas punched by extreme rainfall,” according to one study that looked at the connection between swarms and climate change, and while much of that pattern is fixed in the natural El Niño–Southern Oscillation cycle, a warming climate will also “lead to widespread increases in locust outbreaks with emerging hotspots in west central Asia.” In particular, the research found that in a low-emissions scenario, locust habitat could increase by 5%, while in a high-emissions scenario, it could increase by 13% to 25% between 2065 and 2100.
Did climate change do it? It’d likely be tricky to attribute any one locust swarm to climate change, but as with many other natural phenomena, climate likely plays a compounding factor.
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The failure of the once-promising sodium-ion manufacturer caused a chill among industry observers. But its problems may have been more its own.
When the promising and well funded sodium-ion battery company Natron Energy announced that it was shutting down operations a few weeks ago, early post-mortems pinned its failure on the challenge of finding a viable market for this alternate battery chemistry. Some went so far as to foreclose on the possibility of manufacturing batteries in the U.S. for the time being.
But that’s not the takeaway for many industry insiders — including some who are skeptical of sodium-ion’s market potential. Adrian Yao, for instance, is the founder of the lithium-ion battery company EnPower and current PhD student in materials science and engineering at Stanford. He authored a paper earlier this year outlining the many unresolved hurdles these batteries must clear to compete with lithium-iron-phosphate batteries, also known as LFP. A cheaper, more efficient variant on the standard lithium-ion chemistry, LFP has started to overtake the dominant lithium-ion chemistry in the electric vehicle sector, and is now the dominant technology for energy storage systems.
But, he told me, “Don’t let this headline conclude that battery manufacturing in the United States will never work, or that sodium-ion itself is uncompetitive. I think both those statements are naive and lack technological nuance.”
Opinions differ on the primary advantages of sodium-ion compared to lithium-ion, but one frequently cited benefit is the potential to build a U.S.-based supply chain. Sodium is cheaper and more abundant than lithium, and China hasn’t yet secured dominance in this emerging market, though it has taken an early lead. Sodium-ion batteries also perform better at lower temperatures, have the potential to be less flammable, and — under the right market conditions — could eventually become more cost-effective than lithium-ion, which is subject to more price volatility because it’s expensive to extract and concentrated in just a few places.
Yao’s paper didn’t examine Natron’s specific technology, which relied on a cathode material known as “Prussian Blue Analogue,” as the material’s chemical structure resembles that of the pigment Prussian Blue. This formula enabled the company’s batteries to discharge large bursts of power extremely quickly while maintaining a long cycle life, making it promising for a niche — but crucial — domestic market: data center backup power.
Natron’s batteries were designed to bridge the brief gap between a power outage and a generator coming online. Today, that role is often served by lead-acid batteries, which are cheap but bulky, with a lower energy density and shorter cycle life than sodium-ion. Thus, Yao saw this market — though far smaller than that of grid-scale energy storage — as a “technologically pragmatic” opportunity for the company.
“It’s almost like a supercapacitor, not a battery,” one executive in the sodium-ion battery space who wished to remain anonymous told me of Natron’s battery. Supercapacitors are energy storage devices that — like Natron’s tech — can release large amounts of power practically immediately, but store far less total energy than batteries.
“The thing that has been disappointing about the whole story is that people talk about Natron and their products and their journey as if it’s relevant at all to the sodium-ion grid scale storage space,” the executive told me. The grid-scale market, they said, is where most companies are looking to deploy sodium-ion batteries today. “What happened to Natron, I think, is very specific to Natron.”
But what exactly did happen to the once-promising startup, which raised over $363 million in private investment from big name backers such as Khosla Ventures and Prelude Ventures? What we know for sure is that it ran out of money, canceling plans to build a $1.4 billion battery manufacturing facility in North Carolina. The company was waiting on certification from an independent safety body, which would have unleashed $25 million in booked orders, but was forced to fold before that approval came through.
Perhaps seeing the writing on the wall, Natron’s founder, Colin Wessells, stepped down as CEO last December and left the company altogether in June.
“I got bored,” Wessels told The Information of his initial decision to relinquish the CEO role. “I found as I was spending all my time on fundraising and stockholder and board management that it wasn’t all that much fun.”
It’s also worth noting, however, that according to publicly available data, the investor makeup of Natron appears to have changed significantly between the company’s $35 million funding round in 2020 and its subsequent $58 million raise in 2021, which could indicate qualms among early backers about the direction of the company going back years. That said, not all information about who invested and when is publicly known. I reached out to both Wessels and Natron’s PR team for comment but did not receive a reply.
The company submitted a WARN notice — a requirement from employers prior to mass layoffs or plant closures — to the Michigan Department of Labor and Economic Opportunity on August 28. It explained that while Natron had explored various funding avenues including follow-on investment from existing shareholders, a Series B equity round, and debt financing, none of these materialized, leaving the company unable “to cover the required additional working capital and operational expenses of the business.”
Yao told me that the startup could have simply been a victim of bad timing. “While in some ways I think the AI boom was perfect timing for Natron, I also think it might have been a couple years too early — not because it’s not needed, but because of bandwidth,” he explained. “My guess is that the biggest thing on hyperscalers’ minds are currently still just getting connected to the grid, keeping up with continuous improvements to power efficiency, and how to actually operate in an energy efficient manner.” Perhaps in this environment, hyperscalers simply viewed deploying new battery tech for a niche application as too risky, Yao hypothesized, though he doesn’t have personal knowledge of the company’s partnerships or commercial activity.
The sodium-ion executive also thought timing might have been part of the problem. “He had a good team, and the circumstances were just really tough because he was so early,” they said. Wessells founded Natron in 2012, based on his PhD research at Stanford. “Maybe they were too early, and five years from now would have been a better fit,” the executive said. “But, you know, who’s to say?”
The executive also considers it telling that Natron only had $25 million in contracts, calling this “a drop in the bucket” relative to the potential they see for sodium-ion technology in the grid-scale market. While Natron wasn’t chasing the big bucks associated with this larger market opportunity, other domestic sodium-based battery companies such as Inlyte Energy and Peak Energy are looking to deploy grid-scale systems, as are Chinese battery companies such as BYD and HiNa Battery.
But it’s certainly true that manufacturing this tech in the U.S. won’t be easy. While Chinese companies benefit from state support that can prop up the emergent sodium-ion storage industry whether it’s cost-competitive or not, sodium-ion storage companies in the U.S. will need to go head-to-head with LFP batteries on price if they want to gain significant market share. And while a few years ago experts were predicting a lithium shortage, these days, the price of lithium is about 90% off its record high, making it a struggle for sodium-ion systems to match the cost of lithium-ion.
Sodium-ion chemistry still offers certain advantages that could make it a good option in particular geographies, however. It performs better in low-temperature conditions, where lithium-ion suffers notable performance degradation. And — at least in Natron’s case — it offers superior thermal stability, meaning it’s less likely to catch fire.
Some even argue that sodium-ion can still be a cost-effective option once manufacturing ramps up due to the ubiquity of sodium, plus additional savings throughout the batteries’ useful life. Peak Energy, for example, expects its battery systems to be more expensive upfront but cheaper over their entire lifetime, having designed a passive cooling system that eliminates the need for traditional temperature control components such as pumps and fans.
Ultimately, though, Yao thinks U.S. companies should be considering sodium-ion as a “low-temperature, high-power counterpart” — not a replacement — for LFP batteries. That’s how the Chinese battery giants are approaching it, he said, whereas he thinks the U.S. market remains fixated on framing the two technologies as competitors.
“I think the safe assumption is that China will come to dominate sodium-ion battery production,” Yao told me. “They already are far ahead of us.” But that doesn’t mean it’s impossible to build out a domestic supply chain — or at least that it’s not worth trying. “We need to execute with technologically pragmatic solutions and target beachhead markets capable of tolerating cost premiums before we can play in the big leagues of EVs or [battery energy storage systems],” he said.
And that, he affirmed, is exactly what Natron was trying to do. RIP.
They may not refuel as quickly as gas cars, but it’s getting faster all the time to recharge an electric car.
A family of four pulls their Hyundai Ioniq 5 into a roadside stop, plugs in, and sits down to order some food. By the time it arrives, they realize their EV has added enough charge that they can continue their journey. Instead of eating a leisurely meal, they get their grub to go and jump back in the car.
The message of this ad, which ran incessantly on some of my streaming services this summer, is a telling evolution in how EVs are marketed. The game-changing feature is not power or range, but rather charging speed, which gets the EV driver back on the road quickly rather than forcing them to find new and creative ways to kill time until the battery is ready. Marketing now frequently highlights an electric car’s ability to add a whole lot of miles in just 15 to 20 minutes of charge time.
Charging speed might be a particularly effective selling point for convincing a wary public. EVs are superior to gasoline vehicles in a host of ways, from instantaneous torque to lower fuel costs to energy efficiency. The one thing they can’t match is the pump-and-go pace of petroleum — the way combustion cars can add enough fuel in a minute or two to carry them for hundreds of miles. But as more EVs on the market can charge at faster speeds, even this distinction is beginning to disappear.
In the first years of the EV race, the focus tended to fall on battery range, and for good reason. A decade ago, many models could travel just 125 or 150 miles on a charge. Between the sparseness of early charging infrastructure and the way some EVs underperform their stated range numbers at highway speeds, those models were not useful for anything other than short hauls.
By the time I got my Tesla in 2019, things were better, but still not ideal. My Model 3’s 240 miles of max range, along with the expansion of the brand’s Supercharger network, made it possible to road-trip in the EV. Still, I pushed the battery to its limits as we crossed worryingly long gaps between charging stations in the wide open expanses of the American West. Close calls burned into my mind a hyper-awareness of range, which is why I encourage EV shoppers to pay extra for a bigger battery with additional range if they can afford it. You just had to make it there; how fast the car charged once you arrived was a secondary concern. But these days, we may be reaching a point at which how fast your EV charges is more important than how far it goes on a charge.
For one thing, the charging map is filling up. Even with an anti-EV American government, more chargers are being built all the time. This growth is beginning to eliminate charging deserts in urban areas and cut the number of very long gaps between stations out on the highway. The more of them come online, the less range anxiety EV drivers have about reaching the next plug.
Super-fast charging is a huge lifestyle convenience for people who cannot charge at home, a group that could represent the next big segment of Americans to electrify. Speed was no big deal for the prototypical early adopter who charged in their driveway or garage; the battery recharged slowly overnight to be ready to go in the morning. But for apartment-dwellers who rely on public infrastructure, speed can be the difference between getting a week’s worth of miles in 15 to 20 minutes and sitting around a charging station for the better part of an hour.
Crucially, an improvement in charging speed makes a long EV journey feel more like the driving rhythm of old. No, battery-powered vehicles still can’t get back on the road in five minutes or less. But many of the newer models can travel, say, three hours before needing to charge for a reasonable amount of time — which is about as long as most people would want to drive without a break, anyway.
An impressive burst of technological improvement is making all this possible. Early EVs like the original Chevy Bolt could accept a maximum of around 50 kilowatts of charge, and so that was how much many of the early DC fast charging stations would dispense. By comparison, Tesla in the past few years pushed Supercharger speed to 250 kilowatts, then 325. Third-party charging companies like Electrify America and EVgo have reached 350 kilowatts with some plugs. The result is that lots of current EVs can take on 10 or more miles of driving range per minute under ideal conditions.
It helps, too, that the ranges of EVs have been steadily improving. What those car commercials don’t mention is that the charging rate falls off dramatically after the battery is half full; you might add miles at lightning speed up to 50% of charge, but as it approaches capacity it begins to crawl. If you have a car with 350 miles of range, then, you probably can put on 175 miles in a heartbeat. (Efficiency counts for a lot, too. The more miles per kilowatt-hour your car can get, the farther it can go on 15 minutes of charge.)
Yet here again is an area where the West is falling behind China’s disruptive EV industry. That country has rolled out “megawatt” charging that would fill up half the battery in just four minutes, a pace that would make the difference between a gasoline pit stop and a charging stop feel negligible. This level of innovation isn’t coming to America anytime soon. But with automakers and charging companies focused on getting faster, the gap between electric and gas will continue to close.
On the need for geoengineering, Britain’s retreat, and Biden’s energy chief
Current conditions: Hurricane Gabrielle has strengthened into a Category 4 storm in the Atlantic, bringing hurricane conditions to the Azores before losing wind intensity over Europe • Heavy rains are whipping the eastern U.S. • Typhoon Ragasa downed more than 10,000 trees in Yangjiang, in southern China, before moving on toward Vietnam.
The White House Office of Management and Budget directed federal agencies to prepare to reduce personnel during a potential government shutdown, targeting employees who work for programs that are not legally required to continue, Politico reported Wednesday, citing a memo from the agency.
As Heatmap’s Jeva Lange warned in May, the Trump administration’s cuts to the federal civil service mean “it may never be the same again,” which could have serious consequences for the government’s response to an unpredictable disaster such as a tsunami. Already the administration has hollowed out entire teams, such as the one in charge of carbon removal policy, as our colleague Katie Brigham wrote in February, shortly after the president took office. And Latitude Media reported on Wednesday, the Department of Energy has issued a $50 million request for proposals from outside counsel to help with the day-to-day work of the agency.
At the Heatmap House event at New York Climate Week on Wednesday, Senate Minority Leader Chuck Schumer kicked things off by calling out President Donald Trump’s efforts to “kill solar, wind, batteries, EVs and all climate friendly technologies while propping up fossil fuels, Big Oil, and polluting technologies that hurt our communities and our growth.” The born and raised Brooklynite praised his home state. “New York remains the climate leader,” he said, but warned that the current administration was pushing to roll back the progress the state had made.
Yet as Heatmap’s Charu Sinha wrote in her recap of the event, “many of the panelists remained cautiously optimistic about the future of decarbonization in the U.S.” Climate tech investors Tom Steyer and Dawn Lippert charted a path forward for decarbonization technology even in an antagonistic political environment, while PG&E’s Carla Peterman made a case for how data centers could eventually lower energy costs. You can read about all these talks and more here.
Nearly 100 scientists, including President Joe Biden’s chief climate science adviser, signed onto a letter Wednesday endorsing more federal research into geoengineering, the broad category of technologies to mitigate the effects of climate change that includes the controversial proposal to inject sulfur dioxide into the atmosphere to reflect the sun’s heat back into space. In an open letter, the researchers said “it is very unlikely that current” climate goals “will keep the global mean temperature below the Paris Agreement target” of 1.5 degrees Celsius above pre-industrial averages. The world has already warmed by more than 1 degree Celsius.
Earlier this month, a paper in the peer-reviewed journal Frontiers argued against even researching technologies that could temporarily cool the planet while humanity worked to cut planet-heating emissions. But Phil Duffy, Biden’s former climate adviser, said in a statement to Heatmap that the paper “opposes research … that might help protect or restore the polar regions.” He went on via email, “As the climate crisis accelerates, we all agree that we need to rapidly scale up mitigation efforts. But the stakes are too high not to also investigate other possible solutions.”
President Trump and Prime Minister Keir Starmer. Leon Neal/Getty Images
UK Prime Minister Keir Starmer plans to skip the United Nations annual climate summit in Brazil in November, the Financial Times reported on Wednesday. He will do so despite criticizing his predecessor Rishi Sunak a few years ago for a “failure of leadership” after the conservative leader declined to attend the annual confab. One leader in the ruling Labour party said there was a “big fight inside the government” between officials pushing Starmer to attend the event those “wanting him to focus on domestic issues.”
Polls show approval for Starmer among the lowest of any leaders in the West. But he has recently pushed for more clean energy, including signing onto a series of nuclear power deals with the U.S.
The Tennessee Valley Authority has assumed the role of the nation’s testbed for new nuclear fission technologies, agreeing to build what are likely to be the nation’s first small modular reactors, including the debut fourth-generation units that use a coolant other than water. Now the federally-owned utility is getting into fusion. On Wednesday, the TVA inked a deal with fusion startup Type One Energy to develop a 350-megawatt plant “using the company’s stellarator fusion technology.” The deal, first brokered last week but reported Tuesday in World Nuclear News, promises to deploy the technology “once it is commercially ready.” It also follows the announcement just a few days ago of a major offtake agreement for fusion leader Commonwealth Fusion Systems, which will sell $1 billion of electricity to oil giant Eni.
Climate change is good news for foreign fish. A new study in Nature found that warming rivers have brought about the introduction of new invasive species. This, the researchers wrote, shows “an increase in biodiversity associated with improvement of water in many European rivers since the late twentieth century.”