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The UK’s electricity was the cleanest ever in 2024, new Carbon Brief analysis shows, with carbon dioxide (CO2) emissions per unit falling by more than two-thirds in a decade.

This is because the UK has phased out coal and is now getting less than half as much electricity from burning fossil fuels as a decade ago, while renewable generation has more than doubled.

In total, fossil fuels made up just 29% of the UK’s electricity in 2024 – the lowest level on record – while renewables reached a record-high 45% and nuclear was another 13%.

As a result, each unit of electricity generated in 2024 was associated with an average of just 124g of CO2, compared with a “carbon intensity” of 419gCO2 per kilowatt hour (kWh) in 2014.

Other key insights from the data include:

  • In 2024, the country generated just 91 terawatt hours (TWh) of electricity from fossil fuels – mainly gas, as coal was phased out in September – down from 203TWh in 2014 (-55%).
  • Renewable sources more than doubled from 65TWh in 2014 to 143TWh in 2024 (+122%).
  • Gas-fired power stations remained the UK’s single-largest source of electricity in 2024, generating some 88TWh (28%), just ahead of wind at 84TWh (26%).
  • The remaining sources of electricity in 2024 were nuclear (41TWh, 13%), biomass (40TWh, 13%), imports (33TWh, 11%) and solar (14TWh, 4%).
  • Some 61% of electricity – or 68% excluding imports – came from clean sources, both records, but a long way off the government’s target of at least 95% clean power by 2030.
  • The emissions associated with UK electricity supplies has fallen from 150m tonnes of CO2 (MtCO2) in 2014 to below 40MtCO2 in 2024, down 74%.
  • The reduction in the carbon intensity of electricity means that an electric vehicle (EV) now has lifecycle CO2 savings of 70% over a petrol car, up from only 50% in 2014.
  • Similarly, a household using a heat pump instead of a gas boiler is now cutting its heat-related CO2 emissions by 84% per year, rather than only 45% in 2014.

While figures from the National Energy System Operator (NESO) show wind having generated more electricity than gas in 2024, these numbers exclude significant amounts of gas generation, particularly from “combined heat and power” units at industrial sites.

When accounting for all plants burning gas for power in the UK, the fuel remained as the single-largest source of electricity in 2024, slightly ahead of wind.

However, increasing wind power capacity as new projects are completed in the coming months – and below-average wind speeds in 2024 – mean wind is likely to generate more electricity than gas in 2025.

Carbon Brief has published an annual analysis of the UK’s electricity generation in 2023, 2021, 2019, 2018, 2017 and 2016.

Cleanest ever

Having risen to global dominance on the back of coal-fired industrial might, the UK has made significant progress in cleaning up its power supplies over the past 75 years.

It opened the world’s first civil nuclear power plant in the 1950s, burned oil to generate electricity in the 1960s, made a “dash for gas” in the 1990s, and built renewables in the 2000s and 2010s.

In addition, electricity demand has been falling for nearly two decades, as appliances have become more efficient and the economy has shifted away from heavy industry.

These shifts culminated in the closure of the UK’s last coal-fired power station, at Ratcliffe-on-Soar in Nottinghamshire, in September of 2024. This ended a 142-year era of burning the fuel for electricity, and made the UK the first country in the G7 to completely phase out coal power.

The end of coal power, combined with the rise of renewables, means the UK’s electricity was the cleanest ever in 2024, as shown in the figure below.

Specifically, the carbon intensity of electricity fell to just 124gCO2/kWh in 2024. This is 70% lower than it was in 2014 when each unit of electricity was associated with 419gCO2/kWh.

Carbon intensity of UK electricity generation, gCO2/kWh, 1951-2024.
Carbon intensity of UK electricity generation, gCO2/kWh, 1951-2024. Source: Department of Energy Security and Net Zero (DESNZ), NESO and Carbon Brief analysis.

Combined with a reduction in demand, the emissions associated with UK electricity supplies have dropped from 150MtCO2 in 2014 to less than 40MtCO2 in 2024, a reduction of 74%. This includes emissions embedded in imported electricity and lifecycle emissions associated with imported biomass.

Under the government’s target for clean power by 2030, the carbon intensity of electricity generation should fall by another two-thirds by the end of the decade, according to NESO.

In its advice on how to reach the target, NESO set out pathways to clean power by 2030 that would see carbon intensity falling to 50gCO2/kWh or lower, depending on how it is measured.

This will be a very significant challenge. Nevertheless, the power sector has already been transformed over the past decade. It was the UK’s largest source of CO2 until 2014 and is now only the fifth largest, after transport, buildings, industry and agriculture.

Fossil fuel decline

The swift reductions in the carbon intensity of UK electricity are due to a rapid shift away from burning fossil fuels to generate power.

In addition to phasing out coal power, the UK has also seen significant reductions in the amount of gas generation over the past decade, while oil-fired electricity generation is negligible.

In total, fossil-fired power generation has fallen by more than half in the past decade. It has dropped from 203TWh in 2014 to 91TWh in 2024 (-55%), reaching the lowest level since 1955.

This reduction is illustrated in the figure below, which shows how the decline of fossil fuel generation has mainly been offset by the rise of renewables.

Combined electricity generation from wind, biomass, solar and hydro has more than doubled from 65TWh in 2014 to 143TWh in 2024 (+122%). Combined with falls for coal and gas, this means that renewables now generate significantly (57%) more electricity in the UK than fossil fuels.

UK electricity generation by type, TWh, 1920-2024.
UK electricity generation by type, TWh, 1920-2024. Source: DESNZ, NESO and Carbon Brief analysis.

Notably, the carbon intensity of electricity did not fall during the 2000s, because nuclear generation was starting to decline as the nation’s oldest reactors closed down.

With renewables only just starting to ramp up in this period, the country turned back to fossil fuels to replace lost nuclear generation.

In contrast, carbon intensity has fallen rapidly since 2014, despite further nuclear retirements. Nuclear decline and the coal phase out have been more than offset by renewables, imports and falling demand, meaning gas use has also dropped, as shown in the figure below.

Change in UK electricity generation by fuel, TWh, 2014-2024.
Change in UK electricity generation by fuel, TWh, 2014-2024. Source: DESNZ, NESO and Carbon Brief analysis.

While looking ahead to 2030 and beyond, electricity demand is expected to rise as transport and heat are increasingly electrified via EVs and heat pumps (see below).

According to NESO’s recent advice on reaching clean power by 2030, demand for electricity is expected to grow 11% by 2030 and to nearly double by 2050.

Wind powered

Wind has seen the largest increase of any power source in the UK over the past decade. Moreover, it is expected to form the backbone of the nation’s electricity system by 2030.

The rise of wind power and the decline of fossil fuels means that the UK now gets nearly as much electricity from wind as from gas, as shown in the figure below.

Electricity generation by source, TWh, 2012-2024.
Electricity generation by source, TWh, 2012-2024. Source: DESNZ, NESO and Carbon Brief analysis.

Notably, the rise in wind power output has levelled off over the past two years. The main reason for this is that very little new wind capacity has been added.

In 2022, the UK added 3.5 gigawatts (GW) of new wind capacity, including 3.2GW of offshore wind. This dropped to 1.6GW in 2023, of which 1.1GW came from the Seagreen offshore windfarm off the coast of Scotland, which is currently the nation’s largest and the third-largest in the UK.

However, no new offshore windfarms were added in 2024 and only 0.7GW of new onshore capacity was built, mainly the 0.4GW Viking project in the Shetland Islands.

A further reason for the levelling off in wind power output is that windspeeds have been below average for the past two years.

October and November 2024 have seen particularly poor wind conditions in the UK, respectively 7% and 22% below average – and it has been calm elsewhere in Europe too.

Nevertheless, a new record for wind generation was hit on 19 December 2024, with output reaching 22.5GW for the first time, according to NESO.

National Energy System Operator on X: Great Britain has achieved a new maximum wind record for the second time this week

Several large new offshore windfarms are under construction and due to open in 2025 or 2026.

These include Dogger Bank A, a 1.2GW development in the North Sea due to open next year, as are the 0.9GW Moray West and 0.5GW Neart na Goithe windfarms off Scotland.

In 2026, these projects are due to be followed by the 1.2GW Dogger Bank B and 1.4GW Sofia windfarms, also in the mid-North Sea region.

Given these new developments and the likelihood that windspeeds will return towards average levels, it is likely that the UK will get more electricity from wind than from gas in 2025.

Biomass is the second largest source of renewable electricity in the UK, generating 40TWh in 2024. This is up 17% from 34TWh in 2023, but roughly the same as in 2022.

The UK’s largest biomass generator, the Drax former coal plant in Yorkshire, had seen subdued output in recent years due to planned outages for refurbishment.

Note that Drax only accounts for around a third of biomass generation, with other biomass power sources, including landfill gas, sewage gas and anaerobic digestion of organic waste.

The UK’s net imports of electricity also reached a record high in 2024, with cheaper prices on the continent and new interconnector capacity meaning more power flowed into the country.

Lower lifecycle

The UK’s cleaner electricity generation in 2024 makes electrified heat and transport far more beneficial in terms of reducing CO2 emissions.

For example, an average petrol car in the UK generates 2.7 tonnes of CO2 (tCO2) per year. In 2014, an EV would have generated 830kg of CO2 – but in 2024 this was just 245kg.

Based on the CO2 intensity of electricity in 2014, it would have taken 16,000 miles (2.2 years) for an EV to pay off the “carbon debt” associated with producing its battery, relative to a petrol car.

Based on the cleaner electricity generated in 2024, this payback is just 12,000 miles (1.6 years).

Put another way, an EV driven on 2014 electricity across its full lifetime would have had lifecycle CO2 emissions that were 50% lower than a petrol car. Now, the lifecycle saving is 70%.

There have been similar benefits for CO2 emissions from household energy use, particularly those that use an electric heat pump.

In 2014, a household with average demand would have been responsible for 1.1tCO2 from its electricity use. Today, that figure has fallen to 0.3tCO2.

For a household with a heat pump, emissions from home heating will have fallen from 1.4tCO2 in 2014 to just 0.4tCO2 in 2024. This means that instead of cutting their annual CO2 emissions from heat by 45%, as they were in 2014, they are now reducing their CO2 output by 84%.

Methodology

The figures in the article are from Carbon Brief analysis of data from DESNZ Energy Trends chapter 5 and chapter 6, as well as from NESO. The figures from NESO are for electricity supplied to the grid in Great Britain only and are adjusted here to include Northern Ireland.

In Carbon Brief’s analysis, the NESO numbers are also adjusted to account for electricity used by power plants on site and for generation by plants not connected to the high-voltage national grid.

NESO already includes estimates for onshore windfarms, but does not cover industrial gas combined heat and power plants and those burning landfill gas, waste or sewage gas.

Carbon intensity figures from 2012 onwards are taken directly from NESO. Pre-2012 estimates are based on the NESO methodology, taking account of fuel use efficiency for earlier years.

The carbon intensity methodology accounts for lifecycle emissions from biomass. It includes emissions for imported electricity, based on the daily electricity mix in the country of origin.

DESNZ historical electricity data, including years before 2012, is adjusted to align with other figures and combined with data on imports from a separate DESNZ dataset. Note that the data prior to 1951 only includes “major” power producers.

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Q&A: What can – and cannot – be said about global warming’s role in the 2026 Himalayan floods

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On the morning of 26 August, flash floods surged through a Himalayan border region of Nepal and the Chinese region of Tibet, killing more than 1,300 people, with thousands still missing.

In the days since the floods, scientists have examined satellite imagery, drone footage and seismic data in order to understand and explain the forces behind the event.

While initial theories pinned the flood on a glacial collapse, scientists now understand the event as a “multi-hazard cascade”, which began with a bedrock collapse.

Some climate sceptics have tried to use this to falsely claim that human-caused climate change had no impact on the event.

Yet, scientists have noted that, while no formal attribution study has been carried out thus far, warming is making such ice-rock avalanches in the region more likely.

Researchers have highlighted how rapid warming is dramatically reshaping Asia’s high-mountain region – and identified rising temperatures, glacier retreat and permafrost thaw as factors that may have all contributed to the disaster.

Balendra Shah, Nepal’s prime minister, has called the floods a “serious signal that…the risks we must bear in the Himalayan region are increasing” due to climate change.

Here, Carbon Brief unpacks what scientists currently know about the causes of the catastrophic event and what they can – and cannot – say about the role of climate change.

What happened?

A report published on 28 August by the HiRisk scientific consortium of high mountain experts detailed the events that led to the flash floods.

It said that events were set in motion on 26 August when a mass of bedrock, as well as the glacier ice on top of it, broke off a slope of Langtang-Lirung mountain in the Nepalese Himalaya, plunging from approximately 5,200 metres above sea level to the valley floor at 3,000 metres.

The landslide shook the ground hard enough that, at 8:37am Nepal local time, the US Geological Survey (USGS) initially reported a magnitude 4.4 earthquake. Later that day, it clarified the shaking was caused by glacier collapse and debris flow, equivalent to a magnitude 5.2 earthquake.

On the valley floor, the melting ice, water and debris slammed into the Lhende Khola river, a high-altitude river that runs along Nepal’s border with China.

Known downstream as the Bhote Koshi river in Nepal and the Poiqu or Poqu in China, the Lhende Khole feeds a network of rivers across Nepal and the Chinese region of Tibet, including the Trishuli river. (In China, the Lhende Khola is known as the Donglin Tsangpo.)

This image shows a map of Nepal.
The designations employed and the presentation of the material on this map do not imply the expression of any opinion whatsoever on the part of Carbon Brief concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. Credit: Carbon Brief.

A large “debris” lake was briefly formed on the valley floor. When this lake burst, a wall of water and rock travelled downstream, killing more than a thousand people and destroying settlements, roads, bridges, hydropower plants and border posts across Nepal and Tibet.

HiRisk said that the floodwave travelled down rivers as fast as 30km an hour (around 19 miles per hour) and reached Mugling – a Nepalese town more than 130km downstream – at around 1pm local time.

A separate report from the Center for Land Surface Hazards in the US noted that the flood moved “exceptionally fast, was sediment-laden and extreme in scale”. For example, in the Nepalese municipality of Galchhi, the Trishuli river rose by nine metres in 30 minutes, it said.

Writing in the Conversation, Dr Umesh Haritashya, a glaciologist at the University of Dayton in Ohio, explained that the disaster “wasn’t finished when the first wall of water passed [on 26 August]”.

He continued that a new “barrier lake” – estimated to hold a few million cubic metres of water – had developed in a location where two rivers meet in Tibet before crossing into Nepal. This lake burst on 28 August and the river rose again, he said.

On 4 September, the chief of Nepal’s National Disaster ​Risk Reduction and Management Authority, told Reuters that property and infrastructure worth “at least” $2.5bn (£1.9bn) had been lost. Dharma Raj Upreti estimated the cost to build roads and temporary shelters, provide drinking water and ⁠restore power would be around $53m (£39m).

How did bedrock collapse trigger the flash floods?

In the immediate aftermath of the floods, initial reports suggested that the trigger was a collapsing glacier or earthquake in the high mountains of Nepal.

After confirming that a seismic tremor was as a result of falling rock and ice, the USGS said the trigger was likely a “glacial collapse and debris flow”. This was widely picked up by the media.

Subsequently, satellite imagery revealed that an “enormous chunk of the mountainous bedrock” beneath the glacier had also given way, reported the New York Times.

Dr Kristen Cook, a geomorphologist at the Université Grenoble Alpes in France, told the newspaper:

“The rock that the glacier was sitting on collapsed…It was a much larger collapse than we were initially able to see in the satellite imagery.”

The result was a “deluge of rock and ice, which pulverized into mud and water as it surged down the mountainside”, the newspaper said.

Dr Jakob Steiner a geoscientist at the University of Graz in Austria, tells Carbon Brief:

“It was not a glacier that collapsed. It was the mountain below the glacier that collapsed and the glacier had no other chance but to go with it because it was sitting on top of it.

“The trigger for that is something that we are not 100% certain about, but, in the end, it very much looks like simply a mechanical failure of the rock material because of stressors that have built up over a long period of time.”

Failures of “bedrock” – the hard, solid rock that sits below looser rocks and soil – are an “increasingly common occurrence”, says Prof Bethan Davies, a professor of glaciology at Newcastle University. She tells Carbon Brief:

“These massive landslides occur in mountain regions, commonly following rapid deglacierisation [the melting away of a glacier]. Similar events happened in the Chamoli event in 2021 [in the Indian Himalaya] and in the Blatten landslide last year in Switzerland. They’ve also occurred recently in Alaska.”

With a shift in focus from the failure of a glacier to the bedrock underneath, some climate sceptics seized on the development to falsely claim that climate change had not played any role in the disaster.

These include Dr Matthew Wielicki, recently appointed by the Trump administration to lead the US Global Change Research Program, on Twitter, as well as former Conservative peer and climate-sceptic commentator Matt Ridley in the Spectator.

However, scientists have highlighted the likely contribution of rapid warming in the region. These factors include the thawing of permafrost and glacier retreat. (For more, see sections below).

Fundamentally, “this would have been a much less significant tragedy if it had been just a rock-slope failure”, notes Davies.

The initial landslide took a mixture of rock and ice into a valley that “contains buried ice” as well, she says, providing the water that “resulted in the hyperconcentrated flow, which took so many lives”.

How have temperatures risen in the affected region?

Global temperatures have risen by roughly 1.4C since the pre-industrial period. However, this increase is not uniform across the planet, with some regions warming faster than others.

A study published in Global and Planetary Change in June 2026 investigated changes in the Langtang catchment – a river basin in central Nepal, in which the Langtang-Lirung mountain is located, which eventually drains into the Ganges. Around one-quarter of the area is made up of glaciers.

The paper found that glacial areas of the catchment – found at 4,000 metres above sea level – warmed at 0.31C per decade over 1960-2023. This was “more than three times” the rate observed at a lower elevation weather station, the authors said.

Looking in more detail at the site of the glacial collapse, Dr Robert Rohde, chief scientist for Berkeley Earth, used ERA5 reanalysis data to show how temperature has changed at the 5,200-metre elevation site where the mass of ice and rock broke loose.

Rohde’s analysis found that June-to-August temperatures have been rising at the site of the glacier collapse since the year 1940, with 2026’s summer the fourth warmest on record, behind 2024, 2025 and 2022. This is shown in the graph below.

Average summer (June-August) temperature at the ice-rock avalanche site over 1940-2026.
Average summer (June-August) temperature at the ice-rock avalanche site over 1940-2026. Data source: Rohde, Bluesky (2026)

Rohde also found that the days leading up to the disaster recorded the hottest August temperatures ever experienced at the site. This is shown in the graph below.

Daily average temperature, from 1 June-1 September, at the glacier collapse site.
Daily average temperature, from 1 June-1 September, at the ice-rock avalanche site. 2026, 2025 and 2024 are shown in dark, mid and light blue. All other years from 1940-2023 are shown in grey. Source: Rohde, Bluesky (2026)

On social media, Rohde stated:

“Given the warming trend, this Nepali glacier had probably been thinning and weakening for years, or even decades. But it ultimately failed during the warmest week in one of its warmest years on record. It would be a hell of a coincidence if global warming wasn’t at least partially to blame.”

How have rising temperatures affected mountain stability?

Many experts have linked warming temperatures in the region to thawing permafrost – ground that has been frozen for at least two consecutive years, whose thickness ranges from less than one metre to more than a kilometre.

Steiner is part of a research team that has been using sensors to monitor permafrost in the region since 2014. He tells Carbon Brief that it is “pretty clear” the permafrost has been thawing “very actively” at elevations as high as 5,200 metres above sea level “for many years”. He adds:

“This means that the ground has, over the last decades, moved from being in a solid state into – at least, periodically during the warm season – patchy ground where some is frozen and some isn’t…

“If you have frozen ground next to non-frozen ground, you have dynamics happening between that because there are different densities and there’s movement happening, which is conducive to interventional failure – and that we know from many other cases.”

Davies also points to the “degradation” of perennially frozen ground as a factor in the disaster:

“This permafrost acts as a glue to hold together the rocks and, as it melts, the rock can become weakened.”

Permafrost thaw can also result in saturated ground, says Davies, which adds “pressure in the joints” of rock and can “facilitate” failure. She continues:

“Sources of the water include melting permafrost and meltwater from the overlying glacier. We know that this event happened during a period of warmth, but in the absence of heavy precipitation, pointing to ice melt as the source of water.”

A 2025 study of rock and ice avalanches in High Mountain Asia found that more than two-thirds started in areas “where permafrost is probable”.

How have glaciers retreated in the affected region?

Glaciers – frozen rivers of ice holding three-quarters of the global freshwater supply – are extremely vulnerable to climate change.

In the Himalaya, the rate of glacier retreat has doubled since the late 20th century, according to a 2019 study in Science Advances.

The Global and Planetary Change study found that glacier area loss rates in the Langtang catchment increased more than fourfold from 1964 to 2023 – with melting accelerating after 2000.

It added that glaciers in the region also experienced “fragmentation” and “widespread thinning” over this period.

The study noted that this loss “coincided with elevation dependent warming”.

The figure below provides an overview of glacier loss in the Langtang catchment over 1964-2023, with orange, red and dark red indicating areas of retreat.

In addition, green dots note points of glacier fragmentation, while blue dots show separation and pink show disconnection.

Glacier loss in the Langtang catchment over 1964-2023.
Glacier loss in the Langtang catchment over 1964-2023. Orange, red and dark red indicate areas of retreat. Green dots note points of glacier fragmentation, while blue dots show separation and pink show disconnection. Credit: Silwal et al. (2026)

In comments released by the University of Reading, Prof Maria Shahgedanova, a climate scientist researching climate impacts on mountain glaciers, said that the glacier involved in the floods had “retreated by approximately 450 metres between 1990 and 2020”.

She adds that this “potentially reduce[d] the mechanical support provided by the glacier to the underlying rock slope”.

Speaking to Carbon Brief, Davies reiterates that the retreat of the glacier is “potentially a contributing factor” to the bedrock collapse and subsequent disaster.

This is because the removal of the glacier from the lower slopes leaves the “upper rock slopes less stable”, she says.

The most recent assessment by the International Centre for Integrated Mountain Development said that glaciers in the Hindu Kush Himalaya region are “rapidly shrinking” as a result of climate change. (This region extends 3,500km over Afghanistan, Bangladesh, Bhutan, China, India, Myanmar, Nepal and Pakistan.)

It said this loss is threatening the safety of the nearly two billion people, including by increasing the risk of “glacial lake outburst floods” (GLOFs). A GLOF is a sudden and catastrophic release of meltwater from a glacial lake.

Although this disaster was not caused by a GLOF, it is known that climate change is making such events more likely.

Can the event be attributed to climate change?

In the wake of the flash floods, climate campaigners, media outlets and Nepalese politicians have linked them to human-caused climate change.

However, many climate scientists have cautioned that it is too early to say precisely how climate change impacted the disaster.

Davies tells Carbon Brief:

“These events happen so quickly that the exact causes and drivers can take a little time to uncover, especially if the event was a surprise and there had been no monitoring system in place.”

When trying to determine the role human-caused climate change played in the intensity or likelihood of extreme weather, scientists turn to the field of “attribution science”.

To date, no formal rapid attribution study has been produced that attempts to quantify whether – and how – climate change contributed to the event.

Scientists have noted that climate attribution of ice-rock avalanches – which are typically driven by a variety of factors – remains limited, in part because of the lack of a long-term observational record of previous collapses in high mountain areas.

Meanwhile, the studies that do exist stop short of directly linking such disasters to climate change. For example, the authors of a 2021 study into the Chamoli ice-rock avalanche concluded that “we cannot attribute this individual disaster specifically to climate change”.

However, they added, the “possibly increasing frequency of high-mountain slope instabilities can likely be related to observed atmospheric warming and corresponding long-term changes in cryospheric conditions (glaciers and permafrost)”.

In the aftermath of the disaster, many researchers have similarly highlighted that climate change could not be singled out as the cause of the disaster, even if warming likely increased the probability of its occurrence.

On the Climate Brink substack, Carbon Brief’s climate science contributor Dr Zeke Hausfather noted that a “definitive single-event attribution” of the more recent disaster “may never be possible” due to the “messy causality of rock-ice avalanches”.

However, he added that both the existing scientific literature and “essentially every scientist working on these hazards point in the same direction” – namely, that warming is making such events more likely in the Himalaya.

Steiner tells Carbon Brief it might be possible to attribute different factors that played a role in the disasters to climate change – for instance, the recession of the glacier – but it would be more difficult to do so for the event as a whole.

Part of the reason for this, he says, is that rock failures in this region of the Himalaya have occurred for millennia, well before humans started altering the climate.

However, he continues:

“The physics of it is not something that has been made possible by climate change. This could have happened without it. But the chance of it happening – and the likelihood of it happening five years after a previous, similar event [in Chamoli] – we, as the scientific community, can be pretty confident about that [being increased because of a changing climate].

“This is because so many of the changes that we know are related to climate change can potentially drive the build-up to eventual failure.”

Ultimately, says Davies, a “careful attribution study is needed, but it is hard to argue that the rapidly warming climate is not having an effect in these regions”. She adds:

“A single event may have multiple drivers, but we are seeing an increase in these events and are likely to see more as the permafrost and glacier melt continues.”

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Q&A: What can – and cannot – be said about global warming’s role in the 2026 Himalayan floods
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China’s industrial engine starts to break its fossil fuel habit

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Chinese industry is beginning to shift from fossil fuels to clean electricity, with wind, solar and batteries progressively displacing coal, oil and gas across the industrial sectors that made the country the world’s factory and largest carbon emitter, a new analysis shows.

Clean electricity met all of China’s demand growth in 2025 and coal generation fell for the first time in a decade, even as electricity demand rose by 5%, the report found.

Despite a rebound in coal power generation in the first half of 2026, the analysis by global energy think-tank Ember found the growth in clean electricity illustrates a longer-term shift: a massive build-out of wind, solar energy and battery storage and deepening electrification of the economy are starting to make a dent in the fossil-fuel energy system supporting China’s industrial base.

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The research identifies early signs that a structural transformation of China’s industrial economy from coal, oil and gas to clean electricity is underway, even if changes on the ground are not yet reflected in national data.  

“The energy foundation of the Chinese industrial economy is shifting,” Muyi Yang, a senior energy analyst at Ember and the report’s lead author, told Climate Home News.

“Fossil fuels are progressively being replaced in the many functions they have historically assumed. Because of that, fossil fuel peaking is increasingly coming into view,” he said.

Electrifying industry

Coal generation has stopped growing in 17 of the 26 provinces and regions analysed by Ember between 2021 and 2025. This includes industrial centres such as Hunan in southern China and Shandong – home to energy-intensive industries like cement production. Together, these regions are home to more than half of China’s thermal power capacity.

A greater share of the Chinese economy is now running on electricity than in other major economies, accounting for 29% of final energy consumption in 2024, compared with about 23% in Europe and 21% in the US. Less than half of China’s electricity was generated from coal in the first half of the year.

    Meanwhile, fossil fuel use has fallen in eight of 11 tracked industrial sectors, declining between 26% and 71% from peak consumption levels across fossil fuel extraction, manufacturing industries such as textiles, machinery and food and beverages, transport equipment and chemical materials.

    Earlier this year, German company BASF, the world’s largest chemical producer, opened a new facility in southern China, which is fully supplied by renewable energy. The company said emissions from the site could be 50% lower than conventional petrochemical facilities.

    An employee walks near fields of heliostat mirrors at the site of Dunhuang Shouhang 100MW Tower Solar Thermal Power Generation Project, during an organised media tour to Dunhuang Photovoltaic Industrial Park, in Gansu province, China (Photo: REUTERS/Tingshu Wang)

    An employee walks near fields of heliostat mirrors at the site of Dunhuang Shouhang 100MW Tower Solar Thermal Power Generation Project, during an organised media tour to Dunhuang Photovoltaic Industrial Park, in Gansu province, China (Photo: REUTERS/Tingshu Wang)

    In easier-to-electrify sectors such as machinery, electronics and textiles, electricity now supplies about three-quarters of final energy consumption, Ember found.

    Fossil fuel use is also showing signs of flattening in the metals smelting and processing sector – one of the most fossil-intensive parts of the economy – offering “encouraging signs” that the transformation is starting to take hold in harder-to-abate sectors, said Yang.

    “If that is happening in more and more provinces, and more and more economic sectors that means that fossil fuels are progressively being squeezed out of the energy system,” he said.

    “Growing by greening”

    China’s vast cleantech manufacturing power has become an engine for growth in its own right, spurring investment, creating jobs and generating export revenues.

    Yang described this “growing-by-greening” dynamic as “turning each step of the transition into a source of strength for the next”.

    China and Brazil join pledge to triple global nuclear energy capacity

    For Li Shuo, director of China Climate Hub at the Asia Society Policy Institute, this is part of what makes China’s lead in manufacturing clean energy equipment “irreversible”, comparing its growth with that of a rainforest, where different parts of the ecosystem thrive by reinforcing one another.

    The early success of deploying wind and solar helped drive down electricity costs, which created favourable conditions for the rapid adoption of electric vehicles (EVs) and in turn boosted demand for batteries that are now critical to balance the grid.

    A livestreamer promotes coal during a livestreaming session for Huaze Coal Industry on the Douyin app (Photo:REUTERS/Florence Lo/Illustration)

    A livestreamer promotes coal during a livestreaming session for Huaze Coal Industry on the Douyin app (Photo:REUTERS/Florence Lo/Illustration)

    An oversupply of renewable energy incentivised industrial players to benefit from cheap and readily available clean power generation, encouraging innovative solutions to electrify other parts of the economy. In the transport sector, for example, electrification is moving from passenger vehicles to harder-to-electrify trucks.

    This abundance of cheap green energy is also making China competitive in what has long been seen as the anchor of Western competitiveness, Li said.

    Stalling fossil fuel use

    At the same time, China’s huge legacy fossil fuel generation capacity is still expanding, even as coal power plants are being used less intensively.

    China brought 30 GW of new coal power capacity into operation in the first six months of the year and coal-fired generation rose 3% over the same period after local governments fast-tracked coal projects to prevent a repeat of severe power shortages in 2021.

    Solar surge kept fossil electricity flat in 2025 as China and India made ‘historic’ shift

    A further 274 GW of coal capacity is either under construction or has permits to be built while vast amounts of solar and wind power that could not be absorbed by the grid have gone to waste in the first half of the year.

    “This doesn’t mean that the transition is losing steam,” said Yang, arguing that China is now grappling with some of the more complex aspects of the transition.

    A recent analysis by the Centre for Research on Energy and Clean Air (CREA) for Carbon Brief found that China’s CO2 emissions from fossil fuels and cement have plateaued for more than two years following a peak in March 2024. Ember found that on a 12-month moving average, coal generation has been stalling since then, following years of continuous expansion.

      In the second quarter of the year, CO2 emissions fell by 1% after China’s oil consumption plummeted 9% as the US-Iran war prevented the transport of oil cargoes from the Gulf through the Strait of Hormuz.

      The electrification of the transport sector, particularly electric trucks, was the biggest driver in displacing oil demand as the conflict in the Middle East accelerated the transition.

      A lesson in sequencing

      China’s bumpy transition offers a useful lesson for other countries at an earlier stage of their transition, said Xunpeng Shi, president of the Sydney-based International Society of Energy Transition Studies (ISETS), a global network of professionals that shares research and fosters collaborations.

      “Build quickly enough so that clean electricity can start taking over and prepare for the pressure on the fossil system before it arrives, because that is the part nobody has done easily,” he said.

      For countries that are heavily reliant on revenue from fossil fuel exports, a peak in Chinese fossil fuel use weakens the assumption of rising demand on which investments have long been made.

      “For them, the time to plan for that is now, while the revenues are still there,” he said.

      The post China’s industrial engine starts to break its fossil fuel habit appeared first on Climate Home News.

      China’s industrial engine starts to break its fossil fuel habit

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      Industry and NGOs lobby to weaken UN carbon credit rules in “coordinated” push

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      Carbon credit developers, corporate buyers and some leading conservation NGOs are challenging new proposed rules to stop UN carbon credits being wiped out by fire, drought or logging, in what critics have called a “coordinated lobbying campaign” to weaken the nascent market’s push for greater integrity.

      According to documents seen by Climate Home News – including a briefing given to government officials – companies, NGOs and the UN Environment Programme (UNEP) have contested the scientific basis for the move, arguing that stronger protection for carbon reductions could hike project costs and restrict the supply of credits to the market.

      The climate benefit of credits that claim to reduce or avoid greenhouse gas emissions by storing carbon is undone if that carbon is released back into the atmosphere – something known as reversal risk. To protect against such losses and preserve the credibility of the credits’ carbon-offsetting claims, projects are generally required to set aside a reserve of credits that cannot be sold, as a form of insurance.

      How these “buffer pools” are calculated has long been a source of contention, especially in forest conservation projects, which many experts say have historically underestimated the risk of carbon losses.

      In July, the technical UN panel tasked with drafting rules for the Article 6.4 mechanism, which underpins the credits that countries and companies can use to meet their climate goals, proposed a new system. It would require project developers to size these insurance pools of credits based on local risk values derived from new research published by a group of independent scientists.

      UK’s budget juggling trick with rainforest loan for bus-fare cap needs transparency

      Its supporters have hailed it as a more rigorous approach than current practice in the voluntary carbon market, which largely relies on expert guesswork and, in some cases, gives significant leeway for project developers to come up with their own data.

      “The decision on the reversal risk assessment tool will be crucial,” said Federica Dossi, an expert at Brussels-based advocacy group Carbon Market Watch. “It would bring a new paradigm for calculating the number of units forwarded to the buffer pool based on empirical data.”

      The technical panel is due to discuss the reversal risk tool and its application to a specific set of projects at a five-day meeting in Bonn this week. It is then expected to forward new recommendations to the mechanism’s regulator, the Supervisory Body, for a decision on whether to approve them at a meeting in early October.

      The rules are set to be applied initially only to clean cookstove projects, one of the market’s most popular and heavily criticised credit types. They could then be extended to other activities, including programmes to protect forests.

      Copy and paste?

      More than 30 organisations aired their views in lengthy public submissions to the Article 6.4 mechanism, responding to a call from the UN secretariat for external feedback.

      A Climate Home News review of those submissions found that there was significant overlap in their messages and, in several cases, sections of the text, or even entire submissions, were copied and pasted by different organisations. This points to a coordinated effort to flag concerns regarding the new rules.

      In one instance, tech giant Apple, a large buyer of nature-based carbon credits, warned against relying on one scientific model and called for rules that let project developers use a variety of risk mitigation tools, rather than surrendering buffer credits, to cover the risk of carbon losses.

      Apple’s submission is a lightly-edited version of a separate input presented by the Beyond Alliance, a coalition of corporate buyers and NGOs that promote market-based climate investments. In an apparent oversight in one paragraph, the Beyond Alliance’s name appears in Apple’s submission instead of the tech giant’s.

        The Beyond Alliance told Climate Home News that, after receiving input from its members, it shared its final submission, leaving them to decide if and how they wanted to use it. The coalition rejected any characterisation that its submission advocates for a weaker tool and only reflects business concerns.

        The Beyond Alliance added that its members received briefings by UNEP, which Climate Home News understands has played an important role in wider efforts to influence the development of the rules underpinning the UN carbon market.

        Three experts and a European Union diplomat told Climate Home News that the interventions of the UN agency overwhelmingly supported the views of those with a financial interest in carbon markets.

        UNEP’s head of mitigation Gabriel Labbate rejected this accusation. He told Climate Home News that the UN agency contributes technical inputs from a “politically-neutral, science-based perspective” and its positions are grounded in an assessment of environmental integrity and are not shaped by, or aligned with, the financial interests of any market participant. 

        UNEP, NGOs criticise scientific basis

        In mid-July, representatives from UNEP, Conservation International and The Nature Conservancy (TNC) briefed government officials from Canada, the UK, Germany, Costa Rica, Belgium, Nigeria and Peru, according to a webinar readout seen by Climate Home News.

        The online event was organised by the Forest & Climate Leaders Partnership (FCLP), an initiative that brings together 41 countries plus the EU.

        The speakers voiced strong criticism of the new proposed rules. A technical advisor to Conservation International, a US-based NGO that runs several large-scale carbon offsetting programmes, told participants the Article 6 panel’s approach was “based on bad science”. This, he said, is because it relies on a single model that he claimed is not appropriate to determine buffer pool contributions, according to a presentation seen by Climate Home News.

        During a high-level discussion led by UNEP’s Labbate, speakers said the application of measures to manage reversal risk on cookstove projects could “impose disproportionate costs and undermine the financial viability of these activities”, according to the readout.

        Burn company enumerator Teresia Wanjiru checks moisture on firewood at a client’s house using clean cookstoves in Kachoroba village of Kiambu county, Kenya, August 16, 2023. REUTERS/Monicah Mwangi

        Burn company enumerator Teresia Wanjiru checks moisture on firewood at a client’s house using clean cookstoves in Kachoroba village of Kiambu county, Kenya, August 16, 2023. REUTERS/Monicah Mwangi

        Cookstove programmes issue credits by calculating the greenhouse gas emissions prevented by burning less fuel – usually wood or charcoal – through the use of more efficient stoves. With the new reversal risk tool, these activities would be expected to guard against future carbon losses for the first time under the UN carbon market.

        But UNEP, as well as leading NGOs and carbon credit firms, have pushed back against the requirement, arguing this type of credit represents a “flow” of avoided emissions rather than a “stock” of stored carbon that can be released. Scientists reject that distinction, noting that the wood left unburned is still standing in a forest exposed to the same risks as any other.

        At the online briefing, speakers also raised concerns that the tighter approach would be replicated for nature-based carbon projects with a direct impact on the future of large-scale forest conservation credits. The Conservation International advisor called it a “bad precedent”.

        Both Conservation International and TNC run carbon credit programmes that aim to protect trees from being cut down. Labbate leads the UN-REDD programme, which supports countries developing forest protection initiatives including through carbon credits, and is co-chair of the expert panel advising the Integrity Council for the Voluntary Carbon Market (ICVCM).

        After the webinar, the organisers shared by email a series of “key messages” and draft submissions produced by the three organisations, which participants were invited to consider and adapt in their own inputs to the Article 6.4 consultation process.

        Getting the rules ‘right’

        In a statement to Climate Home News, Ghana, Paraguay and the UK – which are FCLP co-leads for its work on forest carbon credits – said members of the coalition welcomed expert views from a range of partners to help them understand the potential impact of Article 6.4 rules on the eligibility of forest carbon credits in international markets.

        They added that the FCLP does not have a common position on the rules and its members are free to choose whether to attend webinars and use any of the materials circulated.

        In a statement to Climate Home News, Conservation International said “getting these rules right is important to the environmental integrity of the carbon market, while ensuring all sectors have a place in it”. It added that the NGO does not dispute the validity of the scientific research underlying the proposed buffer pool, but recommends a broader approach including multiple models and datasets.

        A spokesperson for TNC said the organisation had helped clarify complex materials and their potential implications, while decisions on how to respond remained entirely with participating countries.

        ‘Inconvenient science’

        The scientific basis for the disputed reversal risk tool rests on two pieces of research. A peer-reviewed study, published in Nature in May and led by scientists at several US universities, modelled forest carbon-loss risk across the United States and found existing buffer pools there are undersized by an average factor of six.

        To extend that approach worldwide, the Article 6.4 panel also drew on a second, global analysis by the same research team, which has not yet completed peer review. That study used satellite images, weather records and computer modelling to estimate a 31-42% chance of forests worldwide losing stored carbon within 100 years, depending on the scenario.

        The panel picked one of these scenarios and turned its estimates into fixed risk percentages for individual countries, and in some cases provinces, which projects in those locations would need to apply.

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        Critics say the peer-reviewed portion of the research was calibrated on North American forests, and that applying the same approach to other regions relies on a global study that is still going through academic checks.

        But, for William Anderegg, professor of biological sciences at the University of Utah and one of the authors of that research, it is the best science currently available. He described it as “light-years better” than assumptions underlying the voluntary carbon market, where risk numbers are not generally based on independent evidence and tend to be incredibly low.

        Scientific research, including by Anderegg, has found that buffer pools in forestry projects in the voluntary carbon market are substantially smaller than they should be to adequately protect against future releases of carbon.

        “There really seems to be a fairly coordinated campaign to try to weaken the strength of these [Article 6.4] tools and their scientific underpinning,” he told Climate Home News. “It’s a little dispiriting to see folks attack science that’s inconvenient.”

        Regulators under pressure?

        An EU diplomat told Climate Home News that experts and negotiators working on the Article 6.4 mechanism have faced intense pressure from big carbon credit developers and large parts of the nature-based solutions community.

        “It is very clear that they are lobbying against strong rules, and they want to align the Paris Agreement mechanism with the standards of the voluntary carbon market,” the diplomat said. “They have influence, time and money, even more than some governments, so they can be very effective in their efforts.”

        Last year, the Article 6.4 Supervisory Body, the new market’s regulator, approved rules on the permanence of credits aiming to remove carbon from the atmosphere which critics said were watered down compared to the technical panel’s recommendations. This followed feedback from carbon market firms and conservation NGOs, which submitted dozens of critical views.

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        Carbon Market Watch’s Dossi said decisions that strengthen environmental integrity are targeted in particular as they tend to reduce the number of credits that can be issued.

        Then, as now, those who opposed tighter rules argued that overly strict safeguards would make some projects too expensive to carry out, with a negative impact on local communities and the climate.

        But proponents argue that higher-integrity programmes will drive up market prices, ultimately benefiting everyone.

        “If rules ensuring better-quality credits make them somewhat more expensive than they are today, that’s an acceptable consequence, not a reason to weaken the rules, especially since these credits will be used to offset continued emissions,” said Dossi.

        Efforts to pull the rule-makers in different directions are expected to intensify in the coming weeks as a decision on the new credit protection system nears.

        “I really don’t know how this will turn out in the end,” one veteran carbon market expert said. “What I am sure about is that it will be quite a battle.”

        The post Industry and NGOs lobby to weaken UN carbon credit rules in “coordinated” push appeared first on Climate Home News.

        Industry and NGOs lobby to weaken UN carbon credit rules in “coordinated” push

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