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In an extraordinary year for the Earth’s climate – which is now virtually certain to be hottest on record – global warming has combined with the El Niño weather phenomenon and other factors to cause “crazy” weather across the globe, including in Africa.

The continent has faced a run of deadly and, in many cases, unprecedented extreme weather events this year.

By far the most lethal was Libya’s “medicane”-fuelled floods, which killed more than 11,300 people in September.

But while Libya’s floods made global headlines, many other deadly extreme events in Africa failed to make international news.

Carbon Brief has combined disaster data, humanitarian reports and local news stories to create a more complete picture of the scale of extreme weather impacts in Africa in 2023 to date.

The investigation shows that at least 15,700 people have so far been killed in extreme weather disasters in Africa in 2023. A further 34 million people have been affected by extremes.

It also shows that:

  • More than 3,000 people were killed in flash floods in the Democratic Republic of the Congo and Rwanda in May. Scientists were unable to assess the role of climate change in the disaster because of a lack of functioning weather stations recording data in the region.
  • At least 860 people were killed in floods and mudslides in February during Tropical Cyclone Freddy, the longest lasting cyclone on record affecting Madagascar, Mozambique, Mauritius, Malawi, Réunion and Zimbabwe.
  • More than 29 million people continue to face unrelenting drought conditions across Ethiopia, Somalia, Kenya, Djibouti, Mauritania and Niger.
  • Southern African countries have sweltered in a months-long winter heatwave, leaving many facing summer-like conditions for a continuous year.

Carbon Brief also spoke to scientists about how these events could be linked to climate change and other factors, including high vulnerability and a lack of preparedness – and why so many of Africa’s extreme weather events go unrecorded and unreported.

In addition, Carbon Brief analysis shows that Africa has the lowest density of weather stations out of any continent – making it difficult to know the extent to which extreme weather is happening and how it might be shifting because of climate change. A climate scientist from Kenya describes this as “extremely worrying”.

She adds that the toll of extreme weather on Africa’s people in 2023 is a stark reminder of why the developed world must take responsibility for the “loss and damage” caused by climate change.

Extremes mapped

Africa is one of the most vulnerable continents in the world to climate change, according to the Intergovernmental Panel on Climate Change (IPCC).

Seven of the 10 countries most vulnerable to climate disasters are in Africa, according to an analysis from the International Rescue Committee (IRC) and the World Resources Institute (WRI).

According to this analysis, the countries most vulnerable to climate disasters are those that have low “climate readiness” – measured by examining the threats that climate change poses to a country and that country’s ability to protect its citizens – and high levels of “fragility” – the likelihood that a country will experience societal collapse in the event of a disaster.

The threats posed by climate change are rising with greenhouse gas emissions, of which Africa is responsible for just 2-3%.

In 2023, every part of the continent was affected by extreme weather disasters, ranging from catastrophic flooding in Libya to intense heat in Malawi.

To study these events, Carbon Brief has combined UN humanitarian reports and local news stories with data from the Emergency Events Database (EM-DAT), which was launched in 1988 by the Centre for Research on the Epidemiology of Disasters (CRED) in Belgium.

The map below shows extreme weather disasters affecting Africa in 2023 to date, according to the EM-DAT database and further analysis by Carbon Brief. On the map, the size of the circles correspond to the number of people affected by the event, while a colour key indicates the event type.

For an extreme event to be featured on the EM-DAT database, it must fulfil one of the following criteria:

  • 10 or more people killed.
  • 100 or more people affected.
  • The declaration of a state of emergency.
  • A call for international assistance.

(It is worth noting that the EM-DAT is the largest disaster database available, but is still not exhaustive, particularly for African nations.)

Extreme weather events in Africa in January-October 2023.

Carbon Brief’s analysis of EM-DAT data, humanitarian reports and local news reports shows that at least 15,700 people have been killed in extreme weather disasters in Africa in 2023 to date.

This is a major jump from the 4,000 people killed by extreme weather disasters in 2022 – but it is worth noting the vast majority of deaths (11,300) occurred during Libya’s record floods.

The analysis also shows that at least 34 million people were affected by extreme weather disasters in 2023. This compares to 19 million people in 2022.

Overall, weather events in Africa this year fit into a global picture of record and, in some cases, uncharted extremes, climate scientists tell Carbon Brief.

The reasons why 2023 has seen such extreme heat and unusual weather events are still being debated by scientists. However, known contributors include the 1.3C of temperature rise already caused by humans and El Niño, a natural phenomenon that tends to drive up global temperatures and affect weather in many parts of the world, including Africa.

Dr Izidine Pinto, a climate scientist from Mozambique currently working at the Royal Netherlands Meteorological Institute, tells Carbon Brief:

“This year is very unusual worldwide. In Africa, almost every month, there were record monthly temperatures. And we know that El Niño is associated with below average rainfall in many parts of Africa, especially in southern Africa.”

Some of the weather events in Africa this year have left scientists scratching their heads, adds Dr Joyce Kimutai, a climate scientist from Kenya currently working at the Grantham Institute – Climate Change and the Environment at Imperial College London. She tells Carbon Brief:

“Climate change is really disrupting the climate system. To me, I think it’s challenging, it’s difficult and it’s also dangerous in a way because as climate scientists we don’t know exactly what’s happening. Every time we think we’ve understood the system, things keep changing. So we would think that we can inform the public about the risks that they can anticipate and how they need to prepare, but then the system is also playing games with us.”

Kimutai adds that the toll of extreme weather events on African lives in 2023 is a stark example of “loss and damage” – a term to describe how climate change is already harming people, especially the world’s most vulnerable. She says:

“We are not on track to limiting warming to 1.5C. That means we will continue to experience these extreme events and that is going to cause more damage to communities. At the same time, people in these countries will have to continually dig deeper into their pockets to deal with these recurring events. What that means is the loss and damages that we know will continue to grow.”

Loss and damage is expected to be a major talking point at the COP28 climate summit in Dubai starting in late November, after a historic fund for such damages was agreed at COP27 in Egypt.

Floods

Floods affected every corner of the African continent in 2023.

Carbon Brief analysis shows at least 23 flood disasters occurred, with countries affected including Angola, Burundi, the Democratic Republic of the Congo, Ghana, Guinea, Ethiopia, Kenya, Liberia, Libya, Mauritania, Mozambique, Namibia, Niger, Rwanda, Somalia, South Africa, Tanzania, Uganda and Zambia.

By far the most deadly were Libya’s floods. In September, a highly unusual cyclone called Storm Daniel dropped a torrent of rainfall over the coast of Libya.

The water quickly overwhelmed two old and damaged dams in the coastal city of Derna, resulting in tsunami-like waves that swept people and houses out to sea. The disaster killed more than 11,300 people.

A rapid analysis released in the storm’s wake found the extreme rainfall was made up to 50 times more likely and 50% more intense by climate change.

Libyan Red Crescent members work on opening roads engulfed in floods.
Libyan Red Crescent members work on opening roads engulfed in floods. Credit: Zuma Press / Alamy Stock Photo.

Storm Daniel was a “medicane”, the name given to a storm originating in the Mediterranean Sea that has the physical features of a hurricane.

Scientists told Carbon Brief that medicanes are currently rare, but there is evidence that they are becoming more intense because of climate change.

One reason for this is when sea surface temperatures are extremely high, it allows storms to gather up more “fuel” as they travel over the ocean – making them stronger when they eventually make landfall.

As well as climate change, the disaster in Libya was worsened by other factors, such as the age of the dams that became overwhelmed with water and an incoherent system for warning the public of the dangers posed by the storms, experts told Carbon Brief.

Another deadly flood to strike Africa in 2023 took place in May, when severe flooding around Lake Kivu devastated communities in the Democratic Republic of the Congo and Rwanda.

According to Carbon Brief analysis, these flash floods killed 2,970 people in the Democratic Republic of the Congo and 131 people in Rwanda.

Many families living in the region had escaped conflict and were living in temporary accommodation, leaving them extremely vulnerable.

Kimutai led a team of scientists who tried to understand how climate change influenced the likelihood and severity of these floods.

However, the researchers were unable to carry out their analysis because they were not able to find reliable rainfall data from weather stations in the region, she explains:

“From the DRC side, we couldn’t find any observational data to use. There have been issues with conflict for a long time and when a country’s at war, almost everything is dysfunctional. What you find with instability is that government employees are not likely to be able to constantly man weather stations and ensure their day-to-day running.”

She adds that the researchers also tried to use satellite information in the place of weather station data. However, data obtained from different satellites did not match up, making it impossible to tell exactly how much rainfall fell during the deadly flash floods.

More on the impact of low weather station coverage in Africa is included in: Why do African extremes go ‘unreported’?

Cyclones

Southern Africa was on the receiving end of a record-breaking – and highly unusual – storm this year called Tropical Cyclone Freddy.

Tropical Cyclone Freddy began as a disturbance near Australia in February and crossed the entire Indian Ocean to make landfall on Madagascar.

The storm then crossed the Mozambican channel to hit Mozambique and surrounding countries. It then returned to the Mozambican channel for several days, before striking Mozambique for a second time. It then proceeded inland towards Malawi.

Overall, the storm persisted for 34 days – making it the longest-lasting tropical cyclone on record. (This record is awaiting verification from the World Meteorological Organization (WMO).)

It also covered a distance exceeding 8,000km. Pinto, who is originally from Mozambique, tells Carbon Brief:

“It made landfall in Mozambique twice, which is very unusual for a tropical cyclone in my living experience. I have never seen a tropical cyclone make landfall and then go back to the ocean before returning again. And this one travelled northwards, which is also unusual because tropical cyclones usually travel from north to south.”

The remarkable path of Tropical Cyclone Freddy is outlined in the diagram below, which was produced by the UN’s Office for the Coordination of Humanitarian Affairs (OCHA).

(The diagram also uses blue shading to show what areas experienced the most flooding and bubbles indicating where the most people were affected.)

The path of Tropical Cyclone Freddy in southern Africa in February. Credit: UN OCHA
The path of Tropical Cyclone Freddy in southern Africa in February. Credit: UN OCHA.

According to Carbon Brief analysis, at least 860 people were killed in floods and landslides associated with the storm across Madagascar, Mozambique, Mauritius, Malawi, Réunion and Zimbabwe.

The storm also destroyed 408,000 houses and 6,600 square kilometres (km2) of cropland across Malawi, Mozambique and Madagascar, according to OCHA. Floodwaters from the storm also assisted several outbreaks of the deadly waterborne disease cholera (indicated with hazard signs on the diagram above).

There has been no analysis into the role of climate change in intensifying Tropical Cyclone Freddy.

However, according to Pinto – who, along with Kimutai, works to analyse the role of climate change in Africa’s extremes with the World Weather Attribution group of scientists – it can be assumed that warming did have an impact on the storm. He explains:

“We did not do a study because previously we’ve done two studies on Tropical Cyclone Batsirai and storm Ana [which affected southern Africa in 2022], and we found that climate change played a role in the amount of rainfall caused by these two tropical cyclones. If we analysed Tropical Cyclone Freddy we would probably find the same answer.”

He adds that the latest findings from the world’s authority on climate science, the Intergovernmental Panel on Climate Change (IPCC), show that eastern southern Africa is likely to see an increase in average tropical cyclone wind speeds and rainfall, as well as a higher proportion of category 4 and 5 (the most severe) storms, as climate change worsens.

“From the scientific literature, it is clear that climate change played a role,” he says.

Tropical Cyclone Freddy crossing the Mozambique Channel.
Tropical Cyclone Freddy crossing the Mozambique Channel. Credit: ZUMA Press, Inc. / Alamy Stock Photo.

Heatwaves

Many parts of Africa faced extreme heat this year.

The north of the continent saw record temperatures during an extreme summer heatwave that affected each of Earth’s seven continents in July.

During this heatwave, Algeria hit 48C, while Morocco faced 47.5C heat.

Adrar in Algeria also experienced Africa’s hottest night on record in July, when night-time temperatures did not fall below 39.6C.

Al Jazeera reported that the extreme temperatures particularly affected migrant workers in Tunisia, who typically sleep rough in tents in the nation’s capital, Tunis.

All Africa reported that 47C heat had a “profound impact” on humans and livestock in Niger.

An analysis by the World Weather Attribution team found that the heat observed across the northern hemisphere in July would have been “virtually impossible” without climate change.

The south of the continent, meanwhile, endured prolonged high temperatures in what were meant to be the winter months.

In August, the Washington Post reported that Southern Africa was in “the midst of a major heatwave” delivering temperatures close to 40C to Botswana, South Africa, Namibia and Mozambique.

In October, the Guardian reported that Malawi was experiencing temperatures 20C above the seasonal average. (Malawi’s cool season typically runs from May to October.)

The prolonged winter heat meant that many southern African countries effectively faced a 12-month long summer, Kimutai says:

“We witnessed for the first time a winter heatwave in southern Africa. People say it didn’t get cold at all this time. It was just like one long back-to-back summer.”

Despite these record events, the Emergency Events Database (EM-DAT) did not register any heatwave disasters in Africa this year (see map above). More explanation of why Africa’s heatwaves often go untracked is included in: Why do African extremes go ‘unreported’?

Wildfires

The extreme heat in northern Africa this year fuelled deadly wildfires.

Reuters reported that wildfires swept across Algeria in July, requiring a response from 8,000 firefighters. The flames killed 34 people, including 10 soldiers.

The newswire added that blazes also ripped across Tunisia, forcing hundreds of households to flee.

A man walks past a house burned down in a wildfire Algeria.
A man walks past a house burned down in a wildfire Algeria. Credit: Xinhua / Alamy Stock Photo.

Drought and famine

Numerous African countries continued to be gripped by severe drought this year. Many of these droughts have spanned several years.

According to Carbon Brief analysis, more than 29 million people faced unrelenting drought conditions across countries including Djibouti, Ethiopia, Kenya, Mauritania, Niger and Somalia in 2023.

According to a report from the UN World Food Programme (WFP) in July, drought in the Horn of Africa has left more than 23 million people facing food insecurity and more than five million children facing acute malnutrition.

The report says:

“The drought affected livestock body conditions and decimated herds, which, in turn, curbed livestock production. Successive below-average harvests, coupled with high production and transport costs, reduced local agricultural produce. All this led to food price spikes that still persist, which reduced household purchasing power and access to nutrient-rich foods.”

An analysis released by the World Weather Attribution service in April found that persistent drought in Ethiopia, Kenya and Somalia “would not have [happened] at all” without human-caused climate change.

People transporting water along a highway in northern Kenya as climate change causes the worst drought in East Africa.
People transporting water along a highway in northern Kenya as climate change causes the worst drought in East Africa. Credit: SOPA Images Limited / Alamy Stock Photo.

A “conservative estimate” from the scientists said that the drought conditions seen in the Horn of Africa over 2020-22 were made at least 100 times more likely by climate change.

In July, the WFP said the impacts of drought conditions in this period are “likely to persist for a long time” despite some improvements in rains in recent months.

Reacting to the analysis in April, Mohamed Adow, director of the Power Shift Africa thinktank in Kenya, said the findings reinforce why climate change is “the world’s biggest and gravest injustice issue”. He told Carbon Brief:

“As someone from East Africa it’s painful to see the impact of climate change wreaking so much suffering on people that have done nothing to cause this.”

Why do African extremes go unreported?

African activists, scientists and policymakers have warned for years that African extreme weather events often go “unreported” when compared to those in North America and Europe.

Understanding the extent to which African extreme weather events are unreported is complicated.

One way to do this is to consider all the ways that extreme weather events are recorded and reported.

Primarily, extreme heat, rainfall and wind speeds – the ingredients of most extreme weather events – are monitored by weather stations.

Carbon Brief’s analysis of WMO weather stations reveals that Africa has the lowest density of operational stations out of any continent.

Africa has the lowest density of weather stations of any continent
Weather station density (number of weather stations per million km2) per continent. Data source: WMO data analysed by Verner Viisainen for Carbon Brief.

Pinto tells Carbon Brief that a lack of weather stations in Africa has limited the tracking of extreme weather events for decades:

“The low density of weather stations is something that limits research and also monitoring of extreme events.”

Without adequate data from weather stations, scientists are not only struggling to track when extreme weather events happen, but they are also left without the historical records needed to understand how events have shifted over time because of climate change, he says.

Kimutai – who was prevented from assessing the role of climate change in deadly floods in the DRC this year by a lack of weather station data – tells Carbon Brief that the lack of weather station data from Africa is “extremely worrying”:

“The reason why I’m extremely worried is because we’ve seen the planet continuing to warm with increasing magnitudes of extreme events – this means the continent is likely to be battered more by these extremes. Without observations, we have a minimal understanding of the climate system so we can’t anticipate how the risks are changing. This means that we can’t adequately prepare.”

As well as having the lowest density of meteorological weather stations, the African continent also has by far the fewest radar weather stations. These kind of stations are needed to warn people about upcoming rainfall, Pinto says:

“If you have a radar, you can see rain coming into the region – and then you can tell people that rain is coming and you can plan. In many parts of Africa, that’s not available because radars are very expensive.”

Even when weather data is recorded, there are other ways that extreme weather disasters can be missed.

In Africa, the most potent example of this occurs with heatwaves.

Human-caused climate change has led to an increase in the intensity and frequency of heatwaves in every region of the world, according to the IPCC.

However, according to the EM-DAT database (see map above), there were no recorded heatwave disasters anywhere in Africa this year. (In fact, EM-DAT lists no more than two heatwaves in sub-Saharan Africa since the beginning of the 20th century.)

This is despite the fact that many parts of Africa did experience record-breaking heat in 2023 (see: Heatwaves). So, why did these events go unrecorded in the EM-DAT database?

The reason is that, for EM-DAT to record a “disaster”, it requires there to be some record of an impact on people.

In Africa, the impacts of extreme heat on people are not routinely recorded as they are in other continents. For example, there are few reliable records of how heatwaves drive up hospital admissions or lead to cropland being destroyed in Africa, Pinto says:

“Some people call heatwaves the ‘silent killer’ because we can’t see the impacts. It is easy to see flooding and people drowning and to record their deaths. But when it’s a heatwave and we don’t see the impact with our eyes, it’s difficult to record.

“So, if a heatwave happens in, say, October and kills 10 people. We don’t know what caused the death of those people. Probably, it was the increase in temperature, which caused them to go to the hospital and suffer heart failures or strokes, but the people responsible for recording the deaths do not make the association with high temperatures.”

Even when observational data and the impacts on people are recorded for an extreme weather event in Africa, there is a good chance that people living outside of the region or country affected will never hear about it.

This is because there is generally less media reporting on African extreme weather events when compared to events in North America or Europe. (Libya’s deadly floods in September were a noticeable exception to this.)

Understanding the reasons behind this are extremely complex.

One survey of 38 African editors by the nonprofit Africa No Filter in 2021 found that shrinking newsrooms and lack of funds prevented deeper reporting and the positioning of correspondents across multiple countries.

Western media has been criticised by young climate activists for giving more priority to extreme weather events in the global north than in Africa.

The post Analysis: Africa’s extreme weather has killed at least 15,000 people in 2023 appeared first on Carbon Brief.

Analysis: Africa’s extreme weather has killed at least 15,000 people in 2023

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Climate Change

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.”

The post Q&A: What can – and cannot – be said about global warming’s role in the 2026 Himalayan floods appeared first on Carbon Brief.

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Climate Change

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”.

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    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.

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    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.

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      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.”

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