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Last year, China started construction on an estimated 95 gigawatts (GW) of new coal power capacity, enough to power the entire UK twice over.

It accounted for 93% of new global coal-power construction in 2024.

The boom appears to contradict China’s climate commitments and its pledge to “strictly control” new coal power.

The fact that China already has significant underused coal power capacity and is adding enough clean energy to cover rising electricity demand also calls the necessity of the buildout into question.

Furthermore, so much new coal capacity provides an easy counterargument for claims that China is serious about the energy transition.

Did China really need more coal power?

And now that it is here, do all these brand-new power plants mean China’s greenhouse gas emissions will remain elevated for longer?

This article addresses four common talking points surrounding China’s ongoing coal-power expansion, explaining how and why the current wave of new projects might come to an end.

New coal is not needed for energy security

The explanation for China’s recent coal boom lies in a combination of policy priorities, institutional incentives and system-level mismatches, with origins in the widespread power shortages China experienced in the early 2020s. 

In 2021, a “mismatch” between the price of coal and the government-set price of coal-fired power incentivised coal-fired power plants to cut generation. Furthermore, power shortages in 2020 and 2022 revealed issues of inflexible grid management and limited availability of power plants, when demand spiked due to extreme weather and elevated energy-intensive economic activity, compounded by coal shortages, reduced hydro output and insufficient imported electricity import. 

Following this, energy security became a top priority for the central government. Local governments responded by approving new coal-power projects as a form of insurance against future outages.

Yet, on paper, China had – and still has – more than enough “dispatchable” resources to meet even the highest demand peaks. (Dispatchable sources include coal, gas, nuclear and hydropower.) It also has more than enough underutilised coal-power capacity to meet potential demand growth.

A bigger factor behind the shortages was grid inflexibility. During both the 2020 power crisis in north-east China and the 2022 shortage in Sichuan, affected provinces continued to export electricity while experiencing local shortages.

A lack of coordination between provinces and inflexible market mechanisms governing the “dispatch” of power plants – the instructions to adjust generation up or down – meant that existing resources could not be fully utilised.

Nevertheless, with coal power plants cheap to build and quick to gain approval, many provinces saw them as a reliable way to reassure policymakers, balance local grids and support industry interests, regardless of whether the plants would end up being economically viable or frequently used. 

China’s average utilisation rate of coal power plants in 2024 was around 50%, meaning total coal-fired electricity generation could rise substantially without the need for any new capacity.

At the same time as adding new coal, the Chinese government also addressed energy security through improvements to grid operation and market reforms, as well as building more storage.

The country added dozens of gigawatts of battery storage, accelerated pumped hydro projects and improved trading linkages between electricity markets in different provinces. 

Though these investments could have gone further, they have already helped avoid blackouts during recent summers – when few of the newly-permitted coal power plants had come online. As such, it is not clear that the new coal plants were needed to guarantee security of supply in the first place.

President Xi Jinping has stated that “energy security depends on developing new energy” – using the Chinese term for renewables excluding hydropower and sometimes including nuclear. According to the International Energy Agency, in the long run, resilience will come not from overbuilding coal, but from modernising China’s power system.

New coal power plants do not mean more coal use and higher emissions

It may seem intuitive to imagine that if a country is building new coal power plants, it will automatically burn more coal and increase its emissions.

But adding capacity does not necessarily translate into higher generation or emissions, particularly while the growth of clean energy is still accelerating.

Coal power generation plays a residual role in China’s power system, filling the gap between the power generated from clean energy sources – such as wind, solar, hydro and nuclear – and total electricity demand. As clean-energy generation is growing rapidly, the space left for coal to fill is shrinking.

From December 2024, coal power generation declined for five straight months before ticking up slightly in May and June, mainly to offset weaker hydropower generation due to drought. Coal power generation was flat overall in the second quarter of 2025.

The chart below shows growth in monthly power generation for coal and gas (grey), solar and wind (dark blue) and other low-carbon power sources (light blue).

This illustrates how the rise in wind and solar growth is squeezing the residual demand left for coal power, resulting in declining coal-power output during much of 2025 to date.

Growth in monthly electricity generation in China by source, terawatt hours (TWh).
Growth in monthly electricity generation in China by source, terawatt hours (TWh). Source: CREA.

Another way to consider the impact of new coal-fired capacity is to test whether, in reality, it automatically leads to a rise in coal-fired electricity generation.

The top panel in the figure below shows the annual increase in coal power capacity on the horizontal axis, relative to the change in coal-power output on the vertical axis.

For example, in 2023, China added 47GW of new coal capacity and coal power output rose by 3.4TWh. In contrast, only 28GW was added in 2021, yet output still rose by 4.4TWh.

In other words, there is no correlation between the amount of new coal capacity and the change in electricity generation from coal, or the associated emissions, on an annual basis.

Indeed, the lower panel in the figure shows that larger additions of coal capacity are often followed by falling utilisation. This means that adding coal plants tends to mean that the coal fleet overall is simply used less often.

New coal power has no predictive value for future coal power generation
Top: Annual change in coal power generation, TWh, relative to the change in coal power capacity, GW, with trend line. Bottom: Change in capacity utilisation, %, relative to the change in capacity, with trend line. Source: CREA.

As such, while adding new coal plants might complicate the energy transition and may increase the risk of unnecessary greenhouse gas emissions, an increase in coal use is far from guaranteed.

If instead, clean energy is covering all new demand – as it has been recently – then building new coal plants simply means that the coal fleet will be increasingly underutilised, which poses a threat to plant profitability.

China is not unique in its approach to coal power

The dynamics behind last year’s surge in coal power project construction starts speak to the logic of China’s system, in which cost-efficiency is not always a central concern when ensuring that key problems are solved.

If a combination of three tools – coal power plants, storage and grid flexibility, in this case – can solve a problem more reliably than one alone, then China is likely to deploy all three, even at the risk of overcapacity. 

This approach reflects not just a desire for reliability, but also deeper institutional dynamics that help to explain why coal power continues to be built.

But that does not mean that such a pattern is unique to China.

The figure below shows that, across 26 regions, a peak in coal-fired electricity generation (blue lines) almost always comes before coal power capacity (red) starts to decline.

Moreover, the data suggests that once there has been a peak, generation falls much more sharply than capacity, implying that remaining coal plants are kept on the system even as they are used increasingly infrequently.

Coal power almost always peaks before capacity
Coal-fired power capacity, GW (blue) and generation, TWh (red) across 26 regions, 2000-2024. Source: Ember.

In most cases, what ultimately stopped new coal power projects in those countries was not a formal ban, but the market reality that they were no longer needed once lower-carbon technologies and efficiency gains began to cover demand growth. 

Coal phase-out policies have tended to reinforce these shifts, rather than initiating them. In China, the same market signals are emerging: clean energy is now meeting all incremental demand and coal power generation has, as a result, started to decline.

Coal is not yet playing a flexible ‘supporting’ role

Since 2022, China’s energy policy has stated that new coal-power projects should serve a “supporting” or “regulating” role, helping integrate variable renewables and respond to demand fluctuations, rather than operating as always-on “baseload” generators. 

More broadly, China’s energy strategy also calls for coal power to gradually shift away from a dominant baseload role toward a more flexible, supporting function.

These shifts have, however, mostly happened on paper. Coal power overall remains dominant in China’s power mix and largely inflexible in how it is dispatched. 

The 2022 policy provided local governments with a new rationale for building coal power, but many of the new plants are still designed and operated as inflexible baseload units. Long-term contracts and guaranteed operating hours often support these plants to run frequently, undermining the idea that they are just backups.

Old coal plants also continue to operate under traditional baseload assumptions. Despite policies promoting retrofits to improve flexibility, coal power remains structurally rigid. 

Technical limitations, long-term contracts and economic incentives continue to prevent meaningful change. Coal is unlikely to shift into the flexible supporting role that China says it wants without deeper reform to dispatch rules, pricing mechanisms and contract structures.

Despite all this, China is seeing a clear shift away from coal. Clean-energy installations have surged, while power demand growth has moderated

As a result, coal power’s share in the electricity mix has steadily declined, dropping from around 73% in 2016 to 51% in June 2025. The chart below shows the monthly power generation share of coal (dark grey), gas (light grey), solar and wind (dark blue), and other low-carbon sources (light blue) from 2016 to the present.

Share of monthly electricity generation in China by source
Share of monthly electricity generation in China by source, %. Source: CREA.

When will the coal boom end?

About a decade ago, the end of China’s coal power expansion also looked near. Coal power plant utilisation declined sharply in the mid-2010s as overcapacity worsened. In response, the government began restricting new project approvals in 2016. 

With new construction slowing and power demand rebounding, especially during and after the height of the Covid-19 pandemic, utilisation rates recovered. Not long after, power shortages kicked off the recent coal building spree.

Now, there are new signs that the coal power boom is approaching its end. Permitting is becoming more selective again in some regions, especially in eastern provinces where demand growth is slowing and clean energy is surging. Meanwhile, system flexibility is advancing

Compared to the late 2010s, the current shift appears more structural. It is driven by the rapid expansion of clean energy, which increasingly eliminates the need for large-scale new coal power projects.

Still, the pace of change will depend on how quickly institutions adapt. If grid operators become confident that peak loads can reliably be met with renewables and flexible backup, the rationale for new coal power plants will weaken.

Equally important, entrenched interests at the provincial and corporate levels continue to push for new plants, not just as insurance, but as sources of investment, employment and revenue. Through long-term contracts and utilisation guarantees, this represents institutional lock-in that may delay the shift away from coal.

The next major turning point will come when coal power utilisation rates begin to fall more sharply and persistently. With large amounts of capacity set to come online in the next two years and clean energy steadily displacing coal in the power mix, a sharp drop in coal power plant utilisation appears likely.

Once this happens, the central government might be expected to step in through administrative capacity cuts – forcing the oldest plants to retire – just as it did during overcapacity campaigns in the steel, cement and coal sectors around 2016 and 2017. 

In that sense, China’s coal power phase-out may not begin with a single grand policy declaration, but with a familiar pattern of centralised control and managed retrenchment.

A key question is how quickly institutional incentives and grid operation will catch up with the dawning reality of coal being squeezed by renewable growth, as well as whether they will allow clean energy to lead, or continue to be held back by the legacy of coal.

The upcoming 15th five-year plan presents a crucial test of government priorities in this area. If it wants to bring policy back in line with its long-term climate and energy goals, then it could consider including clear, measurable targets for phasing down coal consumption and limiting new capacity, for example.

While China’s coal power construction boom looks, at first glance, like a resurgence,it currently appears more likely to be the final surge before a long downturn. The expansion has added friction and complexity to China’s energy transition, but it has not reversed it.

The post Guest post: Why China is still building new coal – and when it might stop appeared first on Carbon Brief.

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Ugandan farmers launch UK court case against East African oil pipeline

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Four Ugandan farmers filed a case with London’s High Court on Tuesday, aiming to stop the East African Crude Oil Pipeline (EACOP) from starting to operate by asking the court to apply Uganda’s laws against the project’s UK-registered company.

The controversial 1,443-kilometre (897-mile) pipeline, majority-owned by French energy company ​TotalEnergies, aims to carry crude from Ugandan fields for export through neighbouring Tanzania. About 80% has been built so far, according to its developers.

The pipeline’s first oil exports are expected as soon as October, according to its developers, and the campaign group Avaaz, which is backing the farmers’ crowdfunded lawsuit, called it “one final chance to stop one of the worst oil pipelines on the planet”.

The claim, filed by London law firm Leigh Day, argues that EACOP Ltd’s role in developing and operating the pipeline breaches Ugandan laws that protect citizens’ right to a clean and healthy environment.

    One of the claimants, Racheal Tugume, told a press conference she had been displaced from her land due to the pipeline’s construction, which she said had damaged local rivers, wildlife and ecosystems that communities depend on for their livelihoods just as erratic weather linked to climate change takes an increasing toll.

    “I am very happy that there are people in countries like the UK who are listening to us, who are behind us and who have come to support us,” Tugume said, adding that she hoped the case would bring justice to communities affected by the pipeline.

    Ugandan law in UK court

    While the pipeline is a joint venture led by TotalEnergies, with smaller stakes owned by Ugandan, Tanzanian and Chinese national oil firms, it is operated by EACOP Ltd, a company registered to an office in London’s Canary Wharf financial district.

    EACOP Ltd did not respond to a request for comment.

    The claim appears to be the first attempt to have Uganda’s climate and environmental protections enforced in a foreign court, partly reflecting concerns over whether cases challenging the multibillion-dollar pipeline would get a fair trial in Uganda.

    Ugandans living near new oil pipeline let down by compensation programmes

    Concerns about access to a fair hearing are among the issues the court will consider when deciding if it should take on the case, said Matthew Renshaw, partner at Leigh Day.

    Renshaw said that precedents including the Nigerian oil pollution case against Shell have shown that claims against British-registered companies for harms overseas can be successfully fought in UK courts.

    “We are proud to represent the four brave principled individuals,” Renshaw said.

    Constitutional protections

    The pipeline project has already been subject to repeated lawsuits in several countries, none of which have succeeded. A climate lawsuit filed in Uganda more than a decade ago by a group of young people has yet to conclude. Another at the East African Court of Justice, brought by campaign groups against Uganda and Tanzania, was rejected on procedural grounds last November.

    A separate ongoing lawsuit in TotalEnergies’ home country of France – a refiled version of an earlier failed claim – cannot stop EACOP going ahead, but it does seek damages from TotalEnergies for affected communities.

    With the newly launched case, Leigh Day’s legal adviser Marc Willers said the claim draws on specific Ugandan laws in a bid to stop EACOP’s operations.

    Uganda may see lower oil revenues than expected as costs rise and demand falls

    These include the Ugandan constitution, a 2019 environmental law and the National Climate Change Act 2021, which gives Ugandans the right to bring a case before a court in circumstances where anyone or any entity threatens the country’s ability to mitigate climate change.

    Stopping a “carbon bomb”

    The pipeline, which will link Uganda’s Lake Albert oil fields to Africa’s east coast in Tanzania, has already displaced thousands of people and cuts through the Lake Victoria basin, one of East Africa’s major freshwater systems and a critical water source for around 40 million people.

    According to the BankTrack non-profit, when the pipeline is at peak production, it will carry 216,000 barrels of crude oil per day and release over 33 million tonnes of carbon emissions each year. Over its full lifetime of 25 years, it is estimated to release about 379 million tonnes of greenhouse gas emissions across its value chain including construction, refining and product use.

    A May 2026 report from Earth Insight also warns that the pipeline and related infrastructure could affect 158 wetlands in Uganda, 11 rivers, 44 protected areas and seven key biodiversity areas while disrupting about 2,000 square km of protected wildlife habitats.

    This is why the primary focus of the UK court case is to stop the operation of the pipeline in its tracks, Leigh Day’s Willers said, calling it a “carbon bomb” that would worsen the world’s climate crisis.

    Long wait for first hearing

    While the purpose of the case is to stop the pipeline from launching operations, Renshaw said it could take about 12 months before the case gets a first hearing and about 18 months before it goes to trial.

    Billions unlocked as Green Climate Fund agrees to spend more and save less

    The farmers are, however, seeking an injunction to stop EACOP Ltd from proceeding with operations. In the event that shipments begin, the lawsuit will still seek to stop the pipeline from then on, Renshaw said.

    “We will be doing what we can to expedite matters but it is possible that EACOP will have started operating the pipeline before the claim is heard. If that is the case, the claim would intend to halt operations from that point. For example, the pipeline may operate for just one year rather than 30-plus, resulting in far less harm,” he said.

    The post Ugandan farmers launch UK court case against East African oil pipeline appeared first on Climate Home News.

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    Cited 7 July 2026: ‘Impossible’ heat | Global ocean record | Climate change and the ozone hole

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    Welcome to Cited, your essential guide to new climate research.

    In the news

    ‘HEAT ALERT’: At least 25 people died as a “heat dome” smothered the eastern half of the US, reported the Guardian, with more than 20 states under “stifling temperatures more than 100F (38C)”. More than 140 million people were under heat alerts, the outlet said, with dead bodies found in “homes with no air conditioning, outside their residences, on the street and in parked cars”. Analysis by World Weather Attribution (WWA) found that the combined heat and humidity would have been “virtually impossible” without human-caused warming, reported the New York Times.

    ‘MORTALITY WILL RISE FURTHER’: Meanwhile, extreme heat continued to hit Europe, with Le Monde reporting on temperatures of 40C in France, Portugal and Spain again this past weekend, alongside “devastating” wildfires. Public Health France doubled its preliminary estimate of the “excess deaths” from the extreme heat in late June, from 1,000 to more than 2,000, according to the Guardian. The higher figure was still “probably an underestimate”, the agency said. Analysis published by Carbon Brief put the figure at 2,700 heat-related deaths. A WWA attribution study, covered by Carbon Brief, found that Europe’s June heatwave would have been “virtually impossible” even 50 years ago.

    ‘BOOST TO GLOBAL TEMPERATURES’: The UN World Meteorological Organization (WMO) “raised its forecast for ​the rapid emergence of a strong El Niño in the coming months, ‌warning that the phenomenon is likely to drive global temperatures higher”, reported Reuters. A WMO scientist told the newswire that “El Niño conditions have emerged ⁠in the equatorial Pacific and there is a remarkable agreement between forecast models that ​this will be a strong El Niño”.

    Research picks

    Extremes

    • The annual season when “intense” tropical cyclones occur has lengthened by 10-14 days per decade across the world since the 1980s | Nature Communications
    • There is an “increasing” and “overlooked” global threat from glacial outburst floods from small lakes | Nature Sustainability
    • Female smallholder farmers in sub-Saharan Africa experience crops losses 2-2.5 times greater than male smallholders in periods of extreme heat | Nature Sustainability

    Policy

    • The summaries for policymakers in Intergovernmental Panel on Climate Change (IPCC) mitigation reports over 2001-22 “have not yet become more solution-oriented while abiding by their policy-neutrality principle” | npj Climate Action
    • Two-thirds of countries address inequality in their national pledges under the Paris Agreement – particularly in “countries with lower levels of human development and greater income inequality” | Climate and Development
    • To “future proof” the Paris Agreement’s “well-below 2C” limit, it should be interpreted as a median “peak warming” of 1.6-1.8C, rather than a 66-90% chance of staying below 2C | Nature Climate Change

    Land sink

    • From 2001 to 2015, northern Eurasia absorbed about 0.47bn tonnes of carbon each year – around one-third of the total global land carbon sink | Global Biogeochemical Cycles
    • Model simulations of potential land-use carbon emissions out to 2100 show that “deforestation and forest regrowth dominate variability” of emissions, with policy timing and ambition “exerting strong control” | Nature Communications
    • Tropical forests are facing an increase in areas that exceed critical temperatures where their “photosynthetic system breaks down” | Proceedings of the National Academy of Sciences

    Captured

    On 21 June, global average sea surface temperature (SST) reached a record high for the day of the year, according to the Copernicus Climate Change Service (C3S). Daily SST for the global ocean, excluding polar regions, reached 20.86C on 21 June, exceeding the 20.83C reached on the same day in both 2023 and 2024, the C3S said. Global SST has remained at record levels for every day since. The conditions “could indicate the beginning of a new phase, leading, once more, to uncharted territory”, said C3S director Carlo Buontempo.


    56 hours and 30 hours

    The amount of time that the average lifespan of tropical cyclones in the north-east and north-west Pacific has shortened, respectively, over 1982-2024, according to a study in npj Climate and Atmospheric Science. This shorter lifespan “compresses the time available for weather forecasting and disaster preparedness”, the authors said.


    Spotlight

    The ozone hole and climate change

    As a new “thought experiment” asks whether the hole in the ozone layer could, theoretically, have been identified decades before it was discovered, Carbon Brief explores the interactions between climate change and the ozone hole.

    It is now more than 40 years since the discovery of the hole in the ozone layer over Antarctica, detailed in the journal Nature in 1985.

    A study more than a decade earlier had predicted that chlorine-based substances – such as chlorofluorocarbons (CFCs) – could lead to the destruction of ozone in the stratosphere.

    So, in theory, how early could the ozone hole have been detected?

    New research, published in the Proceedings of the National Academy of Sciences, explored this very question.

    Study co-author Prof Susan Solomon from the Massachusetts Institute of Technology is a leading atmospheric scientist. In the late 1980s, Solomon and colleagues identified the mechanism behind how CFCs were causing ozone depletion.

    The new study is a “thought experiment”, Solomon told Carbon Brief, asking when scientists could have discovered the ozone hole had they had access to modern satellite observations.

    “We found that depletion could have been detected as early as 1957 in the tropical upper stratosphere, where natural variability is especially small,” explained Solomon.

    This would have been before the use of CFCs became widespread, Solomon added. Instead, early ozone depletion was caused by carbon tetrachloride, a chemical used as a cleaning agent, as well as in fire extinguishers and for producing refrigerants.

    For many decades, the ozone hole and global warming have often been confused by the public and the media, Solomon explained:

    “It’s common to imagine that because ozone is so important at shielding us from the UV [ultraviolet] light that causes skin cancer, then having less ozone must mean the Earth would warm up.”

    For example, in a 1995 editorial, the Los Angeles Times congratulated the Nobel prize-winning chemists who identified the threat of CFCs to the ozone layer. The newspaper noted that these processes “threaten calamitous global warming by damaging the Earth’s protective layer of ozone”.

    However, said Solomon, “the Earth is warmed much more by visible light – UV doesn’t really contribute, so ozone depletion doesn’t cause significant warming”.

    Regional impacts

    The depletion of ozone actually has a very small cooling effect at the Earth’s surface. But this is more than outweighed by the warming impact of CFCs and other ozone-depleting substances.

    This warming impact means that efforts to reverse ozone depletion have had a beneficial impact on the climate.

    The Montreal Protocol, a 1987 international agreement to phase out CFCs, “has played – and is playing – a very substantial role in safeguarding climate too”, said Solomon:

    “It turns out that the CFCs and their replacement gases HCFCs [hydrochlorofluorocarbons] are strong greenhouse gases, so phasing out their production has not only avoided a lot of ozone depletion that would otherwise have occurred, it also had a big influence on global warming.”

    HCFCs were considered as “transitional substitutes” for CFCs – they still damaged ozone, but to a lesser extent – until ozone-safe alternatives were commercially available.

    Hydrofluorocarbons (HFCs), which are not ozone depleting, began to be used widely in the 1990s. However, HFCs are also potent greenhouse gases. HFCs and similar replacements are now being phased out under the 2016 Kigali Amendment to the Montreal Protocol.

    While the ozone hole itself has only a very small impact on global temperatures, it does have a clear impact on the regional climate over Antarctica.

    Prof David Thompson from Colorado State University, working with colleagues including Solomon, has published research demonstrating that “changes in southern-hemisphere winds linked to the stratospheric ozone losses extend all the way down to the ground in some seasons”, explained Solomon.

    This has “reduc[ed] warming that would have occurred in interior Antarctica and enhanc[ed] warming in the Antarctic Peninsula region”, she said.

    The knock-on impacts include “wind changes [that] actually extend beyond Antarctica to the mid-latitudes of the southern hemisphere, where they even affect rainfall”, she added.

    Preprints to watch

    Carbon Brief’s pick of new papers under review

    • The drying impact over Africa from using stratospheric aerosol injections to stabilise global temperatures would only be minimised “when combined with a strong decarbonisation effort” | Earth System Dynamics
    • The El Niño-Southern Oscillation and Indian Ocean Dipole could “shape” the playing conditions at the Rugby World Cup 2027 in Australia | Journal of Southern Hemisphere Earth Systems Science
    • A “strong” weakening of the Atlantic Meridional Overturning Circulation (AMOC) would “profoundly alter the climate-carbon cycle system”, underscoring the “importance of explicitly accounting for AMOC risks in long-term climate assessments” | Earth System Dynamics

    Noticeboard

    • 6 July-25 September: Registration open for experts to review the first-order draft of the Intergovernmental Panel on Climate Change’s Working Group I report 
    • 7-15 July: UN High-level Political Forum on Sustainable Development, New York
    • 19 July: Application deadline for a postdoctoral scholar in transdisciplinary climate research at Penn State University, US | Salary: unknown
    • 22 July: Application deadline for PhD project on “climate change impacts on the Antarctic coastal ocean carbon sink” at the University of East Anglia, UK
    • 26 July: Application deadline for PhD projects on “AI for land-atmosphere feedbacks during hydroclimatic extremes” at the Helmholtz School for Integrated Data Science in Environmental & Life Sciences, Germany
    • 29 July: Application deadline for an assistant professor in Earth and environmental geosciences (palaeoclimatology) at Colgate University, US | Salary: $97,500-101,500
    • 31 July: Application deadline for PhD project on Arctic Ocean methane oxidation at Stockholm University, Sweden

    Cited is researched and written by Cecilia Keating, Robert McSweeney, Ayesha Tandon, Daisy Dunne and Dr Giuliana Viglione.

    Please send tips, feedback and upcoming climate research to cited@carbonbrief.org

    This is an online version of Carbon Brief’s fortnightly Cited email newsletter. Subscribe for free here.

    The post Cited 7 July 2026: ‘Impossible’ heat | Global ocean record | Climate change and the ozone hole appeared first on Carbon Brief.

    Cited 7 July 2026: ‘Impossible’ heat | Global ocean record | Climate change and the ozone hole

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    Climate Change

    Guest post: France’s June heatwave caused more than 2,700 heat-related deaths

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    In June 2026, a record-breaking heatwave swept across Europe, with France among the first and hardest hit countries.

    In a new analysis, we estimate that the extreme conditions caused more than 2,700 heat-related deaths in France.

    We also show how France’s extreme temperatures in June exceeded projections from climate models.

    Our findings illustrate the human toll of extreme weather as the world warms.

    We also highlight the challenges in projecting the magnitude of future heatwaves and their impacts on people.

    Outpacing projections

    For most of this century, Europe has seen summer heat extremes that outpace projections from climate models.

    Several different factors likely explain this trend, including reductions in planet-cooling aerosols as nations have cleaned up their air pollution, as well as changes in atmospheric circulation patterns, which models struggle to represent.

    In June 2026, daily high temperatures averaged across France reached 36.9C, shattering the previous June record set in 2022 by 2.4C.

    [For more on the impacts and coverage of Europe’s June heatwave, see Carbon Brief’s explainer.]

    The rise in observed temperatures in France has outpaced projections made by climate models, with June maximum temperatures more in line with what was expected for the 2070s.

    This is illustrated in the figure below, which shows how France’s average maximum daily high temperature for June recorded in 2026 (black line) compares to climate model projections (blue and orange lines).

    Comparison of observed (ERA5, black) and modelled (blue and orange) temperatures across France from 2000 to 2080. Plot shows the maximum daily high temperature recorded in June for each year, after averaging temperatures across France. The model ensembles are bias-corrected CMIP6 model ensembles from the NEX-GDDP (blue) and CIL-GDPCIR (orange) projects. The dashed blue and orange lines are the ensemble averages. Credit: Prof Andrew Dessler.
    Comparison of observed (ERA5, black) and modelled (blue and orange) temperatures across France from 2000 to 2080. Plot shows the maximum daily high temperature recorded in June for each year, after averaging temperatures across France. The model ensembles are bias-corrected CMIP6 model ensembles from the NEX-GDDP (blue) and CIL-GDPCIR (orange) projects. The dashed blue and orange lines are the ensemble averages. Credit: Prof Andrew Dessler.

    Counting the death toll of climate change

    The downstream impacts of these extreme temperatures are lethal.

    Scientists are able to estimate the death toll of high temperatures in many locations, depending on the availability of mortality and climate data.

    There are several ways to do this.

    One option is to examine death certificates to see which deaths have been directly recorded by physicians as related to heat. However, there is strong evidence that this method significantly undercounts heat-related deaths, as most death certificates do not consider environmental factors such as heat when diagnosing the cause of death.

    Alternatively, it is possible to calculate the rate of total (“all-cause”) mortality in a given time period relative to previous time periods – for example, by comparing the total number of deaths in June 2026 compared to the average of previous Junes. This “excess deaths” figure can be used as an estimate of the deaths from a heat wave.

    Using this approach, Public Health France attributed around 2,000 deaths in France to the extreme heat in the week of 22-28 June.

    Finally, scientists can use long-term data on overall mortality and correlate changes in mortality with changes in temperature to understand the statistical relationship between the two.

    Research published in Proceedings of the National Academy of Sciences in 2025 that used this third approach found that mortality rates in France increase rapidly in cold or hot conditions as daily maximum temperatures depart further from approximately 20C.

    This pattern of a U-shaped response of mortality to temperature – shown in the figure below – is very consistent across time periods and regions around the world.

    Chart showing the relationship between extreme heat and mortality in France
    Relationship between daily high temperature and all-cause mortality rates in France, estimated using data over 2004-19. Credit: Dr Christopher Callahan, based on data and methods in Callahan et al. (2025)

    To calculate the death toll of the June 2026 heatwave in France, we compared observed temperatures over 12-29 June to their baseline average over 1980-2025.

    The difference between these two temperatures helps us understand how many more people died than they would have in the absence of such extreme conditions.

    Over 12-29 June, we found that France has experienced around 2,700 heat-related deaths above the average baseline. Day-to-day heat-related mortality rates rose from less than 100 to almost 300 on the hottest days of 24 and 25 June.

    This is shown in the graph below, which illustrates the cumulative total heat-related deaths seen in France over the two-and-a-half week period. The inset shows how heat-related deaths fluctuated on a day-to-day basis during this time.

    Chart showing the number of deaths from heat in France during the June 2026 heatwave
    Estimated heat-related mortality over 12-29 June, based on a U-shaped response of mortality to temperature. The main plot shows cumulative total deaths and the inset shows daily deaths. Credit: Dr Christopher Callahan, based on data and methods in Callahan et al. (2025)

    Recent analysis by World Weather Attribution has already shown that human-caused climate change increased the frequency and intensity of the June heat wave across Europe.

    Meanwhile, previous research has shown there is substantial evidence that heat-related mortality in Europe has already been elevated by greenhouse gas emissions.

    As a result, we can be confident that at least some of the more than 2,700 deaths already seen in France are directly due to the burning of fossil fuels.

    Calculating climate risk

    In April, the UN-led body responsible for coordinating the work of climate modelling centres – the Coupled Modelling Intercomparison Project (CMIP) – unveiled a set of seven new emissions scenarios.

    These are designed to replace the previous scenarios that have been used by scientists to understand how the climate might change in the future. They will feed into the upcoming seven assessment report (AR7) of the Intergovernmental Panel on Climate Change (IPCC).

    The range of future emissions in the new CMIP scenarios is smaller, with scenarios of very high or very low emissions no longer on the table.

    The retirement of the very-high emissions scenario – known as “RCP8.5” – led to certain commentators in the media and in politics, including US president Donald Trump, arguing that the risks of climate change had been “overstated”.

    [For more on false and misleading claims around the new emissions scenarios, see Carbon Brief’s factcheck.]

    Our analysis of June’s heat-related deaths in France suggests that, even if the most severe emissions pathways are no longer needed, climate impacts are taking a heavy toll on society.

    Moreover, the temperatures seen in France show that climate models continue to underpredict the magnitude of heatwaves for a particular level of global warming.

    This is because greenhouse gas emissions are only a first step in estimating the impacts of climate change.

    The second step is converting emissions to changes in the climate at both the global and local levels – or hazards. This includes heatwaves, flash floods and droughts.

    The third step is to determine how changes in the hazards will affect local populations. This can be determined by calculating people’s exposure and vulnerability to hazards.

    Substantial uncertainty persists at every stage of this sequence.

    For example, scientists do not know exactly how the global climate will react to ever-rising greenhouse gas emissions – nor the extent to which global temperature increases will drive local climate hazards. We also do not know how climate change at a local level impacts human health outcomes.

    Managing the future of heat risk

    Almost all heat-related deaths are preventable.

    Adaptation options, such as air conditioning, heat action plans and social support for isolated people, will be crucial as the climate moves away from the typical conditions that people are used to.

    Our previous research showed that France made a lot of progress reducing heat-related mortality after the deadly 2003 summer heatwave by taking many of these actions.

    Adaptation can reduce deaths, but it cannot eliminate the risk created by continued warming.

    Without a move away from fossil fuels, future heatwaves will keep testing the limits of public health systems and more people will die.

    The post Guest post: France’s June heatwave caused more than 2,700 heat-related deaths appeared first on Carbon Brief.

    Guest post: France’s June heatwave caused more than 2,700 heat-related deaths

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