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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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Here at Heatmap, we write a lot about decarbonization — that is, the process of transitioning the global economy away from fossil fuels and toward long-term sustainable technologies for generating energy. What we don’t usually write about is what those technologies actually do. Sure, solar panels convert energy from the sun into electricity — but how, exactly? Why do wind turbines have to be that tall? What’s the difference between carbon capture, carbon offsets, and carbon removal, and why does it matter?
So today, we’re bringing you Climate 101, a primer on some of the key technologies of the energy transition. In this series, we’ll cover everything from what makes silicon a perfect material for solar panels (and computer chips), to what’s going on inside a lithium-ion battery, to the difference between advanced and enhanced geothermal.
There’s something here for everyone, whether you’re already an industry expert or merely climate curious. For instance, did you know that contemporary 17th century readers might have understood Don Quixote’s famous “tilting at windmills” to be an expression of NIMYBism? I sure didn’t! But I do now that I’ve read Jeva Lange’s 101 guide to wind energy.
That said, I’d like to extend an especial welcome to those who’ve come here feeling lost in the climate conversation and looking for a way to make sense of it. All of us at Heatmap have been there at some point or another, and we know how confusing — even scary — it can be. The constant drumbeat of news about heatwaves and floods and net-zero this and parts per million that is a lot to take in. We hope this information will help you start to see the bigger picture — because the sooner you do, the sooner you can join the transition, yourself.
Without further ado, here’s your Climate 101 syllabus:
Once you feel ready to go deeper, here are some more Heatmap stories to check out:
The basics on the world’s fastest-growing source of renewable energy.
Solar power is already the backbone of the energy transition. But while the basic technology has been around for decades, in more recent years, installations have proceeded at a record pace. In the United States, solar capacity has grown at an average annual rate of 28% over the past decade. Over a longer timeline, the growth is even more extraordinary — from an stalled capacity base of under 1 gigawatt with virtually no utility-scale solar in 2010, to over 60 gigawatts of utility-scale solar in 2020, and almost 175 gigawatts today. Solar is the fastest-growing source of renewable energy in both the U.S. and the world.
There are some drawbacks to solar, of course. The sun, famously, does not always shine, nor does it illuminate all places on Earth to an equal extent. Placing solar where it’s sunniest can sometimes mean more expense and complexity to connect to the grid. But combined with batteries — especially as energy storage systems develop beyond the four hours of storage offered by existing lithium-ion technology — solar power could be the core of a decarbonized grid.
Solar power can be thought of as a kind of cousin of the semiconductors that power all digital technology. As Princeton energy systems professor and Heatmap contributor Jesse Jenkins has explained, certain materials allow for electrons to flow more easily between molecules, carrying an electrical charge. On one end of the spectrum are your classic conductors, like copper, which are used in transmission lines; on the other end are insulators, like rubber, which limit electrical charges.
In between on that spectrum are semiconductors, which require some amount of energy to be used as a conductor. In the computing context these are used to make transistors, and in the energy context they’re used to make — you guessed it — solar panels.
In a solar panel, the semiconductor material absorbs heat and light from the sun, allowing electrons to flow. The best materials for solar panels, explained Jenkins, have just the right properties so that when they absorb light, all of that energy is used to get the electrons flowing and not turned into wasteful heat. Silicon fits the bill.
When you layer silicon with other materials, you can force the electrons to flow in a single direction consistently; add on a conductive material to siphon off those subatomic particles, and voilà, you’ve got direct current. Combine a bunch of these layers, and you’ve got a photovoltaic panel.
Globally, solar generation capacity stood at over 2,100 terawatt-hours in 2024, according to Our World in Data and the Energy Institute, growing by more than a quarter from the previous year. A huge portion of that growth has been in China, which has almost half of the world’s total installed solar capacity. Installations there have grown at around 40% per year in the past decade.
Solar is still a relatively small share of total electricity generation, however, let alone all energy usage, which includes sectors like transportation and industry. Solar is the sixth largest producer of electricity in the world, behind coal, gas, hydropower, nuclear power, and wind. It’s the fourth largest non-carbon-emitting generation source and the third largest renewable power source, after wind and hydropower.
Solar has taken off in the United States, too, where utility-scale installations make up almost 4% of all electricity generated.
While that doesn’t seem like much, overall growth in generation has been tremendous. In 2024, solar hit just over 300 terawatt-hours of generation in the U.S., compared to about 240 terawatt-hours in 2023 and just under 30 in 2014.
Looking forward, there’s even more solar installation planned. Developers plan to add some 63 gigawatts of capacity to the grid this year, following an additional 30 gigawatts in 2024, making up just over half of the total planned capacity additions, according to Energy information Administration.
Solar is cheap compared to other energy sources, and especially other renewable sources. The world has a lot of practice dealing with silicon at industrial scale, and China especially has rapidly advanced manufacturing processes for photovoltaic cells. Once the solar panel is manufactured, it’s relatively simple to install compared to a wind turbine. And compared to a gas- or coal-fired power plant, the fuel is free.
From 1975 to 2022, solar module costs fell from over $100 per watt to below $0.50, according to Our World In Data. From 2012 to 2022 alone, costs fell by about 90%, and have fallen by “around 20% every time the global cumulative capacity doubles,” writes OWID analyst Hannah Ritchie. Much of the decline in cost has been attributed to “Wright’s Law,” which says that unit costs fall as production increases.
While construction costs have flat-lined or slightly increased recently due to supply chain issues and overall inflation, the overall trend is one of cost declines, with solar construction costs declining from around $3,700 per kilowatt-hour in 2013, to around $1,600 in 2023.
There are solar panels at extreme latitudes — Alaska, for instance, has seen solar growth in the past few years. But there are obvious challenges with the low amount of sunlight for large stretches of the year. At higher latitudes, irradiance, a measure of how much power is transmitted from the sun to a specific area, is lower (although that also varies based on climate and elevation). Then there are also more day-to-day issues, such as the effect of snow and ice on panels, which can cause issues in turning sunlight into power (they literally block the panel from the sun). High latitudes can see wild swings in solar generation: In Tromso, in northern Norway, solar generation in summer months can be three times as high as the annual average, with a stretch of literally zero production in December and January.
While many Nordic countries have been leaders in decarbonizing their electricity grids, they tend not to rely on solar in that project. In Sweden, nuclear and hydropower are its largest non-carbon-emitting fuel sources for electricity; in Norway, electricity comes almost exclusively from hydropower.
There has been some kind of policy support for solar power since 1978, when the Energy Tax Act provided tax credits for solar power investment. Since then, the investment tax credit has been the workhorse of American solar policy. The tax credit as it was first established was worth 10% of the system’s upfront cost “for business energy property and equipment using energy resources other than oil or natural gas,” according to the Congressional Research Service.
But above that baseline consistency has been a fair amount of higher-level turmoil, especially recently. The Energy Policy Act of 2005 kicked up the value of that credit to 30% through 2007; Congress kept extending that timeline, with the ITC eventually scheduled to come down to 10% for utility-scale and zero for residential projects by 2024.
Then came the 2022 Inflation Reduction Act, which re-instituted the 30% investment tax credit, with bonuses for domestic manufacturing and installing solar in designated “energy communities,” which were supposed to be areas traditionally economically dependent on fossil fuels. The tax then transitioned into a “technology neutral” investment tax credit that applied across non-carbon-emitting energy sources, including solar, beginning in 2024.
This year, Congress overhauled the tax incentives for solar (and wind) yet again. Under the One Big Beautiful Bill Act, signed in July, solar projects have to start construction by July 2026, or complete construction by the end of 2027 to qualify for the tax credit. The Internal Revenue Service later tightened up its definition of what it means for a project to start construction, emphasizing continuing actual physical construction activities as opposed to upfront expenditures, which could imperil future solar development.
At the same time, the Trump administration is applying a vise to renewables projects on public lands and for which the federal government plays a role in permitting. Renewable industry trade groups have said that the highest levels of the Department of Interior are obstructing permitting for solar projects on public lands, which are now subject to a much closer level of review than non-renewable energy projects.
Massachusetts Institute of Technology Researchers attributed the falling cost of solar this century to “scale economies.” Much of this scale has been achieved in China, which dominates the market for solar panel production, especially for export, even though much of the technology was developed in the United States.
At this point, however, the cost of an actual solar system is increasingly made up of “soft costs” like labor and permitting, at least in the United States. According to data from the National Renewables Energy Laboratory, a utility-scale system costs $1.20 per watt, of which soft costs make up a third, $0.40. Ten years ago, a utility-scale system cost $2.90 per watt, of which soft costs was $1.20, or less than half.
Beyond working to make existing technology even cheaper, there are other materials-based advances that promise higher efficiency for solar panels.
The most prominent is “perovskite,” the name for a group of compounds with similar structures that absorb certain frequencies of light particularly well and, when stacked with silicon, can enable more output for a given amount of solar radiation. Perovskite cells have seen measured efficiencies upwards of 34% when combined with silicon, whereas typical solar cells top out around 20%.
The issue with perovskite is that it’s not particularly durable, partially due to weaker chemical bonds within the layers of the cell. It’s also more expensive than existing solar, although much of that comes down inefficient manufacturing processes. If those problems can be solved, perovskite could promise more output for the same level of soft costs as silicon-based solar panels.
The country’s largest source of renewable energy has a long history.
Was Don Quixote a NIMBY?
Miguel de Cervantes’ hero admittedly wasn’t tilting at turbines in 1605, but for some of his contemporary readers in 17th-century Spain, windmills for grinding wheat into flour were viewed as a “dangerous new technology,” author Simon Winchester writes in his forthcoming book, The Breath of the Gods: The History and Future of the Wind. One interpretation of Cervantes’ novel might be that Quixote was “actually doing battle with progress.”
Nearly four and a half centuries later, harnessing the energy of the wind remains controversial, even if the breeze is one of humankind’s longest-utilized resources. While wind is the largest source of renewable electricity generation in the United States today, high construction costs and local opposition have more recently stymied the industry’s continued expansion. The new presidential administration — suspicious of wind’s reliability and place in the American energy mix — has also been doing its very best to stunt any future growth in the sector.
Whether you’re catching up on Trump’s latest regulatory moves, you have your own concerns about the safety of the technology, or this is your first time even thinking about this energy resource, here is the blow-by-blow — sorry! — on wind power in the U.S.
At their most basic conceptual level, wind turbines work by converting kinetic energy — the energy of an object in motion; in this case, air particles — into electrical energy that can be used to power homes, buildings, factories, and data centers.
Like hydroelectric dams, turbines do this by first converting kinetic energy into mechanical energy. The wind turns the turbine blades, which spin a rotor that is connected to a generator. Inside the generator are magnets that rotate around coils of copper wire, creating a magnetic field that pushes and pulls the electrons within the copper. Voilà — and with gratitude to Michael Faraday — now you have an electrical current that can be distributed to the grid.
Turbines typically require an average wind speed of about 9 miles per hour to generate electricity, which is why they are constructed in deserts, mountain passes, on top of hills, or in shallow coastal waters offshore, where there is less in the way to obstruct the flow of wind. Higher elevations are also windier, so utility-scale wind turbines are frequently around 330 feet tall (though the largest turbines tower 600 feet or higher).
It depends on the size of the turbine and also the wind speed. The average capacity of a new land-based wind turbine in the U.S. was 3.4 megawatts in 2023 — but that’s the “nameplate capacity,” or what the turbine would generate if it ran at optimal capacity around the clock.
U.S. Department of Energy
In the U.S., the average capacity factor (i.e. the actual energy output) for a turbine is more like 42%, or close to two-fifths of its theoretical maximum output. The general rule of thumb is that one commercial turbine in the U.S. can power nearly 1,000 homes per month. In 2023, the latest year of data available, land-based and offshore wind turbines in the U.S. generated 425,235 gigawatt-hours of electricity, or enough to power 39 million American homes per year.
A common criticism of wind power is that it “stops working” if the wind isn’t blowing. While it’s true that wind is an intermittent resource, grid operators are used to coping with this. A renewables-heavy grid should combine different energy sources and utilize offline backup generators to prevent service interruptions during doldrums. Battery storage can also help handle fluctuations in demand and increase reliability.
At the same time, wind power is indeed dependent on, well, the wind. In 2023, for example, U.S. wind power generation dropped below 2022 levels due to lower-than-average wind speeds in parts of the Midwest. When you see a turbine that isn’t spinning, though, it isn’t necessarily because there isn’t enough wind. Turbines also have a “cut out” point at which they stop turning if it gets too windy, which protects the structural integrity of the blades and prevents Twisters-like mishaps, as well as keeps the rotor from over-spinning, which could strain or break the turbine’s internal rotating components used to generate electricity.
Though Americans have used wind power in various forms since the late 1800s, the oil crisis of the 1970s brought new interest, development, and investment in wind energy. “The American industry really got going after the suggestion from the Finns, the Swedes, the Danes,” who’d already been making advances in the technology, albeit on single-turbine scales, Winchester, the author of the forthcoming history of wind power, The Breath of the Gods, told me.
In the early 1970s, the Department of Energy issued a grant to William Heronemus, a professor at the University of Massachusetts, Amherst, to explore the potential of wind energy. Heronemus became “really enthusiastic and built wind generators on the campus,” helping to modernize turbines into the more familiar construction we see widely today, Winchester said.
Some of Heronemus’ former students helped build the world’s first multi-turbine wind farm in New Hampshire in 1981. Though the blades of that farm interfered with nearby television reception — they had to be paused during prime time — the technology “seemed to everyone to make sense,” Winchester said. The Energy Policy Act of 1992, which introduced production tax credits for renewables, spurred further development through the end of the millennium.
Heronemus, a former Naval architect, had dreamed in the 1970s of building a flotilla of floating turbines mounted on “wind ships” that were powered by converting seawater into hydrogen fuel. Early experiments in offshore wind by the Energy Research and Development Administration, the progenitor of the Department of Energy, weren’t promising due to the technological limitations of the era — even commercial onshore wind was still in its infancy, and Heronemus’ plans looked like science-fiction.
In 1991, though, the Danes — ever the leaders in wind energy — successfully constructed the Vindeby Offshore Wind Farm, complete with 11 turbines and a total installed capacity of 5 megawatts. The Blyth offshore wind farm in northern Wales soon followed, with the United States finally constructing its first grid-connected offshore wind turbines off of Maine in 2013. The Block Island wind farm, with a capacity of 30 megawatts, is frequently cited as the first true offshore wind farm in the U.S., and began operating off the coast of Rhode Island in 2016.
Though offshore wind taps into higher and more consistent wind speeds off the ocean — and, as a result, is generally considered more efficient than onshore wind — building turbines at sea comes with its own set of challenges. Due to increased installation costs and the greater wear-and-tear of enduring saltwater and storms at sea, offshore wind is generally calculated to be about twice as expensive as onshore wind. “It’s unclear if offshore wind will ever be as cheap as onshore — even the most optimistic projections documented by the National Renewable Energy Laboratory have offshore wind more expensive than the current price of onshore in 2035,” according to Brian Potter in his newsletter, Construction Physics, though he notes that “past projections have underestimated the future cost reductions of wind turbines.”
Scott Eisen/Getty Images
In the decade from 2014 to 2023, total wind capacity in the U.S. doubled. Onshore and offshore wind power is now responsible for over 10% of utility-scale electricity generation in the U.S., and has been the highest-producing renewable energy source in the nation since 2019. (Hydropower, the next highest-producing renewable energy source, is responsible for about 5.7% of the energy mix, by comparison.) In six states — Iowa, Kansas, Oklahoma, New Mexico, South Dakota, and North Dakota — onshore wind makes up more than a third of the current electricity mix, Climate Central reports.
Offshore wind has been slower to grow in the U.S. Even during the Biden administration, when the government targeted developing 30 gigawatts of offshore wind capacity by 2030, the industry faced financing challenges, transmission and integration obstacles, and limits in access to a skilled workforce, per a 2024 paper in Energy Research & Social Science. That same year, the Department of Energy reported that the nation had a total of 80,523 megawatts for offshore wind in operation and in the pipeline, which, under ideal conditions, could power 26 million homes. Many of those offshore projects and plans now face an uncertain future under the Trump administration.
Though we’re far removed from the 1880s, when suspicious Scots dismissed wind energy pioneer James Blyth’s home turbine as “the devil’s work,” there are still plenty of persistent concerns about the safety of wind power to people and animals.
Some worry about onshore wind turbines’ effects on people, including the perceived dangers of electromagnetic fields, shadow flicker from the turning blades, and sleep disturbance or stress. Per a 2014 systematic review of 60 peer-reviewed studies on wind turbines and human health by the National Institutes of Health, while there was “evidence to suggest that wind turbines can be a source of annoyance to some people, there was no evidence demonstrating a direct causal link between living in proximity to wind turbines and more serious physiological health effects.” The topic has since been extensively studied, with no reputable research concluding that turbines have poor health impacts on those who live near them.
Last year, the blade of a turbine at Vineyard Wind 1 broke and fell into the water, causing the temporary closure of beaches in Nantucket to protect people from the fiberglass debris. While no one was ultimately injured, GE Vernova, which owns Vineyard Wind, agreed earlier this year to settle with the town for $10.5 million to compensate for the tourism and business losses that resulted from the failure. Thankfully, as my colleague Jael Holzman has written, “major errors like blade failures are incredibly rare.”
There are also concerns about the dangers of wind turbines to some wildlife. Turbines do kill birds, including endangered golden eagles, which has led to opposition from environmental and local activist groups. But context is also important: The U.S. Fish & Wildlife Service has found that wind farms “represent just 0.03% of all human-related bird deaths in the U.S.” (Illegal shootings, for example, are the greatest cause of golden eagle deaths.) The continued use of fossil fuels and the ecological impacts of climate change also pose a far graver threat to birds than wind farms do. Still, there is room for discussion and improvement: The California Department of Fish and Wildlife issued a call earlier this year for proposals to help protect golden eagles from turbine collisions in its major wind resource areas.
Perhaps the strongest objection to offshore wind has come from concern for whales. Though there has been an ongoing “unusual mortality event” for whales off the East Coast dating back to 2016 — about the same time the burgeoning offshore wind industry took off in the United States — the two have been falsely correlated (especially by groups with ties to the fossil fuel industry). A recent government impact report ordered by Republicans even found that “NOAA Fisheries does not anticipate any death or serious injury to whales from offshore wind-related actions and has not recorded marine mammal deaths from offshore wind activities.” Still, that hasn’t stopped Republican leaders — including the president — from claiming offshore wind is making whales “a little batty.”
Polling by Heatmap has found that potential harm to wildlife is a top concern of both Democrats and Republicans when it comes to the deployment of renewable energy. Although there has been “no evidence to date that the offshore wind build-out off the Atlantic coast has harmed a single whale … studies have shown that activities related to offshore wind could harm a whale, which appears to be enough to override the benefits for some people,” my colleague Jael has explained. A number of environmental groups are attempting to prevent offshore and land-based wind development on conservationist grounds, to varying degrees of success. Despite these reservations, though, our polling has found that Americans on the coast largely support offshore wind development.
Aesthetic concerns are another reason wind faces opposition. The proposed Lava Ridge wind farm in Idaho, which was Heatmap’s most imperiled renewable energy project last year, faced intense opposition, ostensibly due to the visibility of the turbines from the Minidoka National Historic Site, the site of a Japanese internment camp. Coastal homeowners have raised the same complaint about offshore wind that would be visible from the beach, like the Skipjack offshore wind project, which would be situated off the coast of Maryland.
Not good. As one of President Trump’s first acts in office, he issued an executive order that the government “shall not issue new or renewed approvals, rights of way, permits, leases, or loans for onshore or offshore wind projects” until the completion of a “comprehensive assessment” of the industry’s impacts on the economy and the environment. Eight months later, federal agencies were still not processing applications for onshore wind projects.
Offshore wind is in even more trouble because such projects are sited entirely in federal waters. As of late July, the Bureau of Ocean Energy Management had rescinded all designated wind energy areas — a decision that applies to some 3.5 million acres of federal waters, including the Central Atlantic, California, and Oregon. The Department of the Interior has also made moves to end what it calls the “special treatment for unreliable energy sources, such as wind,” including by “evaluating whether to stop onshore wind development on some federal lands and halting future offshore wind lease sales.” The Interior Department will also look into how “constructing and operating wind turbines might affect migratory bird populations.”
The One Big Beautiful Bill Act, meanwhile, put strict restrictions on tax credits available to wind developers. Per Cleanview, the bill jeopardizes some 114 gigawatts of wind energy projects, while the Center for American Progress writes that “more than 17,000 jobs are connected to offshore wind power projects that are already canceled, on hold, or at risk from the Trump administration’s attacks on wind power.”
The year 2024 marked a record for new wind power capacity, with 117 gigawatts of wind energy installed globally. China in particular has taken a keen interest in constructing new wind farms, installing 26 gigawatts worth, or about 5,300 turbines, between January and May of last year alone.
Still, there are significant obstacles to the buildout of wind energy even outside of the United States, including competition from solar, which is now the cheapest and most widely deployed renewable energy resource in the world. High initial construction costs, deepened by inflation and supply-chain issues, have also stymied wind development.
There are an estimated 424 terawatts worth of wind energy available on the planet, and current wind turbines tap into just half a percent of that. According to Columbia Business School’s accounting, if maximized, wind has the potential to “abate 10% to 20% of CO2 emissions by 2050, through the clean electrification of power, heat, and road transport.”
Wind is also a heavy player in the Net Zero Emissions by 2050 Scenario, which aims for
7,100 terawatt hours of wind electricity generation worldwide by the end of the decade, per the International Energy Agency. But current annual growth would need to increase annual capacity additions from about 115 gigawatts in 2023 to 340 gigawatts in 2030. “Far greater policy and private-sector efforts are needed to achieve this level of capacity growth,” IEA notes, “with the most important areas for improvement being facilitating permitting for onshore wind and cost reductions for offshore wind.”
Wind turbines continue to become more efficient and more economical. Many of the advances have come in the form of bigger turbines, with the average height of a hub for a land-based turbine increasing 83% since the late 1990s. The world’s most powerful offshore turbine, Vestas’ V236-15.0 megawatt prototype, is, not coincidentally, also the world’s tallest, at 919 feet.
Advanced manufacturing techniques, such as the use of carbon fiber composites in rotor blades and 3D printed materials, could also lead to increases in efficiency. In a 2024 report, NREL anticipated that such innovations could potentially “unlock 80% more economically viable wind energy capacity within the contiguous United States.”
Floating offshore wind farms are another area of active innovation. Unlike the fixed-foundation turbines mainly used offshore today, floating turbines could be installed in deep waters and allow for development on trickier coastlines like off of Oregon and Washington state. Though there are no floating offshore wind farms in the United States yet, there are an estimated 266 gigawatts of floating turbine capacity in the pipeline globally.