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The past three years have been exceptionally warm globally.

In 2023, global temperatures reached a new high, after they significantly exceeded expectations.

This record was surpassed in 2024 – the first year where average global temperatures were 1.5C above pre-industrial levels.

Now, 2025 is on track to be the second- or third-warmest year on record.

What has caused this apparent acceleration in warming has been subject to a lot of attention in both the media and the scientific community.

Dozens of papers have been published investigating the different factors that could have contributed to these record temperatures.

In 2024, the World Meteorological Organization (WMO) discussed potential drivers for the warmth in a special section of its “state of the global climate” report, while the American Geophysical Union ran a session on the topic at its annual meeting.

In this article, Carbon Brief explores four different factors that have been proposed for the exceptional warmth seen in recent years. These are:

Carbon Brief’s analysis finds that a combination of these factors explains most of the unusual warmth observed in 2024 and half of the difference between observed and expected warming in 2023.

However, natural fluctuations in the Earth’s climate may have also played a role in the exceptional temperatures, alongside signs of declining cloud cover that may have implications for the sensitivity of the climate to human-caused emissions.

An unusually warm three years

Between 1970 and 2014, average surface temperatures rose at a fairly steady rate of around 0.18C per decade.

Set against this long-term trend, temperature increases during the period from 2015 to 2022 were on the upper end of what would be expected.

The increases seen in 2023, 2024 and 2025 were well outside of that range.

The high temperatures of the past three years reflect a broader acceleration in the rate of warming over the past decade.

However, the past three years were unusually warm, even when compared to other years in the 2010s and 2020s.

Record-breaking warmth in 2023 meant that it beat the prior warmest year of 2016 by 0.17C – the largest magnitude of a new record in the past 140 years.

The year 2024 then swiftly broke 2023’s record, becoming the first year where average global temperatures exceeded 1.5C above pre-industrial levels.

The 10 months of data available for 2025 indicates that the year is likely to be slightly cooler than 2023 – though it is possible it may tie or be slightly warmer.

The figure below shows global surface temperatures between 1970 and 2025. (The figures for 2025 include uncertainty based on the remaining three months of the year.)

It includes a smoothed average based on temperature data for 1970-2022 that takes into account some acceleration of warming – and then extrapolates that smoothed average forward to 2023-25 to determine what the expected temperature for those years would have been. (This follows the approach used in the WMO’s “state of the global climate 2024” report.)

Chart showing annual global surface temperatures and the long-term average warming
Global average surface temperature changes between 1970 and 2024 using the WMO average of six groups that report global surface temperature records (dark blue), estimated 2025 temperatures and uncertainties (red) based on the first nine months of the year and a long-term average locally linear smooth (light blue).

This approach calculates how much warmer the past three years were than would be expected given the long-term trend in temperatures.

It shows that 2023 was around 0.18C warmer than expected, 2024 was a massive 0.25C warmer and 2025 is likely to be 0.11C warmer.

Researchers have identified a number of potential drivers of unexpected warmth over 2023-25. Here, Carbon Brief looks at the evidence for each one.

A weirdly behaving El Niño event

El Niño is a climate pattern of unusually warm sea surface temperatures (SSTs) in the tropical Pacific that naturally occurs every two to seven years. Strong El Niño years generally have warmer global temperatures, with the largest effect generally occurring in the months after El Niño conditions peak (when SSTs reach their highest levels in the tropical Pacific).

A relatively strong El Niño event developed in the latter half of 2023, peaking around November before fading in the spring of 2024.

This event was the fourth-strongest El Niño ever recorded, as measured according to SSTs in the Niño 3.4 region in the central tropical Pacific. However, it was notably weaker than the El Niño events in both 1998 and 2016.

This can be seen in the chart below, which shows the strength of El Niño events (red shading) since the 1980s. (The blue shading indicates La Niña events – the opposite part of the cycle to El Niño, which results in cooler SSTs in the tropical Pacific.)

Char showing El Niño and La Niña Index (Niño 3.4 region)
NOAA’s Niño 3.4 region Oceanic Niño Index using detrended data from ERSSTv5.

(It is worth noting that measuring the strength of El Niño events is not entirely straightforward. Other tools used by scientists to monitor changes to El Niño – such as the US National Oceanic and Atmospheric Administration’s (NOAA’s) multivariate ENSO index – show the 2023-24 event was much weaker than indicated in the Niño 3.4 dataset.)

Global surface air temperatures tend to be elevated by around 0.1-0.2C in the six months after the peak of a strong El Niño event – defined here as when SSTs in the Niño 3.4 region reach 1.5C above normal.

The figure below shows the range of global temperature change for the 12 months before and 22 months after the peak of all 10 strong El Niño events since 1950. The light line represents the average of past strong El Niño events, the dark blue line the temperature change observed during the 2023-24 event and the shaded blue area the 5-95th percentile range.

Chart showing that the recent El Niño was unusual compared with strong El Niño events
Global mean surface temperatures for the 12 months prior to peak El Niño conditions and the 22 months following for strong El Niño events. Calculations by Carbon Brief using data from Copernicus/ECMWF’s ERA5 and NOAA’s Oceanic Niño Index.

The figure shows the 2023-24 El Niño was quite unusual compared to other strong El Niño events since 1970. Global temperatures rose to around 0.4C above expected levels – which is on the high side of previous El Niños.

The heat also came early, with high temperatures showing up around four months before the El Niño event peaked. This early heat is unlike any other El Niño event in modern history and is one of the reasons why 2023’s global temperatures were so unexpectedly warm.

Global temperatures remained elevated for a full 18 months after the El Niño peaked, well after conditions in the tropical Pacific shifted into neutral conditions – and even after mild La Niña conditions developed at the end of 2024 and into early 2025.

This figure does not explain how much of this unusual heat was actually caused by El Niño, compared to other factors, but it does suggest that El Niño behaviour alone does not fully explain unusually high temperatures in recent years.

Based on the historical relationship between El Niño and global temperatures, Carbon Brief estimates that El Niño contributed a modest 0.013C to 2023 temperatures and a more substantial 0.128C to 2024 temperatures, albeit with large uncertainties. (See “methodology” section at the end for details.)

However, it is possible that this 2023 estimate is too low. There are some suggestions in the literature that 2023-24 El Niño’s early warmth may have been caused by the rapid transition out of a particularly extended La Niña event. There are indications that temperatures have spiked in similar situations further back in the historical temperature record.

Falling sulphur dioxide emissions

Sulphur dioxide (SO2) is an aerosol that is emitted into the lower atmosphere by the burning of coal and oil. It has a powerful climate cooling effect – Carbon Brief analysis shows that global emissions of SO2 have masked about one-third of historical warming.

Global SO2 emissions have declined around 40% over the past 18 years, as countries have increasingly prioritised reducing air pollution, including through the installation of scrubbers at coal plants.

These declines have been particularly concentrated in China, which has seen a 70% decline in SO2 emissions since 2007. In addition, a rule introduced for international shipping in 2020 by the International Maritime Organization (IMO) has resulted in an 80% decline in the sulphur content of shipping fuel used around the world.

The decline of SO2 emissions is shown in the figure below.

Chart showing that China and international shipping are large drivers of recent SO2 emissions decline
Annual SO2 emissions from China, international shipping and the rest of the world. Data from the Community Earth atmospheric Data System (CEDS).

Shipping in particular has been suggested as a potential culprit for recent temperatures, given that ships emit SO2 over oceans where the air tends to be cleaner and so emissions have a bigger effect.

Seven of the eight studies that have explored the temperature impact of the IMO regulations have suggested a relatively modest effect, in the range of 0.03-0.08C. However, one study – led by former NASA scientist Dr James Hansen – calculated a much stronger effect of 0.2C that would explain virtually all the unusual warmth of recent years.

The figure below shows Carbon Brief’s estimate of the global average surface temperature changes caused by the low-sulphur shipping fuel rules, using the estimates produced by all eight studies. The central estimate (dark blue line) is relatively low, at around 0.05C, but the uncertainty range (light blue shading) across the studies remains large.

Chart showing the range of estimated warming effects of the IMO 202 low sulphur shipping rules
Range (5th to 95th percentile) and central estimate (50th percentile) of simulated global average surface temperature responses to the IMO 2020 regulations across the radiative forcing estimates in the literature. Analysis by Carbon Brief using the FaIR model.

Overall, Carbon Brief’s analysis finds that around 0.04C of warming over 2020-23 and 0.05C of warming over 2020-24 can be attributed to SO2 declines from shipping and other sources.

However, this approach might slightly overstate the effects of SO2 on the exceptional temperatures of the past three years, as shipping and other SO2 declines would have had some effect on 2021 and 2022 as well.

It is also worth noting that the total effects of SO2 declines on global temperatures have been considerably larger and are estimated to be responsible for around one-quarter of all warming since 2007.

However, these SO2 decreases occurred over a long period of time and do not clearly explain the recent spike in temperatures.

An unusual volcanic eruption in Tonga

In early 2022, the Hunga Tonga-Hunga Ha’apai underwater volcano erupted spectacularly, sending a plume 55km into the atmosphere. This was by far the most explosive volcanic eruption since Mount Pinatubo erupted in 1991.

This was a highly unusual volcanic eruption, which vaporised vast amounts of sea water and lofted it high into the atmosphere. Overall, around 146m metric tonnes of water vapour ended up in the stratosphere, which is the layer of the atmosphere above the troposphere.

Water vapour is a powerful greenhouse gas. While it is short-lived in the lower atmosphere, it can stick around for years in the stratosphere, where it has a significant warming effect on the climate.

The figure below shows the concentration of water vapour in the stratosphere between 2005 and mid-2025. It shows how the 2022 eruption increased atmospheric concentrations of the greenhouse gas by around 15%. More than half the added water vapour has subsequently fallen out of the upper atmosphere.

Chart showing upper atmosphere water vapour content
Upper atmosphere water vapor content from NASA’s Aura MLS satellite. Figure from Dr Robert Rohde.

Most early studies of the Hunga Tonga-Hunga Ha’apai volcano focused specifically on the effects of stratospheric water vapour. These tended to show strong warming in the lower stratosphere and cooling in the middle-to-upper stratosphere, but only a slight warming effect on global surface temperatures of around 0.05C.

Hunga Tonga-Hunga Ha’apai had much lower sulphur emissions than prior explosive eruptions, such as Pinatubo and El Chichon. However it put 0.51.5m tonnes of sulphur into the stratosphere – the most from an eruption since Pinatubo.

Studies that included both sulphur and water vapour effects tend to find that the net effect of the eruption on surface temperatures was slight global cooling, concentrated in the southern hemisphere.

By using the estimates published in a 2024 study published in Geophysical Research Letters, which used the FaIR climate emulator model, Carbon Brief estimates that the Hunga Tonga-Hunga Ha’apai eruption cooled global surface temperatures by -0.01C in 2023 and -0.02C in 2024.

This suggests that the eruption was likely only a minor contributor to recent global surface temperatures.

A stronger-than-expected solar cycle

The source of almost all energy on Earth is the sun. Over hundreds of millions of years, variations in solar output have a big impact on the global climate.

Thankfully, over shorter periods of time the sun is remarkably stable, helping keep the Earth’s climate habitable for life. (Big changes – such as ice ages – have more to do with variations in the Earth’s orbit than changes in solar output.)

However, slight changes in solar output do occur – and when they do, they can influence climate change over shorter periods of time. The most important of these is the roughly 11-year solar cycle, which is linked with the sun’s magnetic field and results in changes in the number of sunspots and amount of solar energy reaching Earth.

The figure below shows a best-estimate of changes in total solar irradiance since 1980, based on satellite observations. Total solar irradiance is a measure of the overall amount of solar energy that reaches the top of the Earth’s atmosphere and is measured in watts per metre squared.

Chart showing the recent solar cycle has been relatively strong
Total solar irradiance from the PMOD composite (blue) along with a smoothed average (red) from 1980 to 2025.

The 11-year solar cycle is relatively modest compared to the sun’s total output, varying only a few watts per metre squared between peak and trough – amounting to around 0.01% of solar output. However, these changes can result in variations of up to 0.1C in global temperatures within a decade.

The most recent solar cycle – solar cycle 25 – began around 2020 and has been the strongest solar cycle measured since 1980. It was stronger than most models had anticipated and likely contributed to around 0.04C global warming in 2023 and 0.07C in 2024.

Putting together the drivers

By combining earlier estimates of different factors contributing to 2023 and 2024 global surface temperatures, about half of 2023’s unusual warmth and almost all of 2024’s unusual warmth can be effectively explained.

This is illustrated in the figure below, which shows the five different factors discussed earlier – El Niño, shipping SO2, Chinese SO2, the Hunga Tonga-Hunga Ha’apai volcano and solar cycle changes – along with their respective uncertainties.

The sum of all the factors is shown in the “combined” bar, while the actual warming compared to expectations is shown in red.

The upper chart shows 2023, while the lower one shows 2024.

Charts showing the components of 2023 and 2024's above-expected warmth
Attribution of 2023 and 2024 anomalous warmth. Blue bars show individual factors and their uncertainties, the orange bar shows the combined effects and combination of uncertainties and the green bar shows the actual warming compared with expectations. Adapted from Figure 12 in WMO’s state of the global climate 2024 report.

It is important to note that the first bar includes both El Niño and natural year-to-year variability; the height of the bar reflects the best estimate of El Niño’s effects, while the uncertainty range encompasses year-to-year variability in global temperatures that may be – at least in part – unrelated to El Niño.

The role of natural climate variability

Large natural variability to the Earth’s climate is one of the main reasons why the combined value of the different drivers of expected warmth in 2023 has an uncertainty range that exceeds the observed warming – even though the best-estimate of combined factors only explains half of temperatures.

Or, to put it another way, there is up 0.15C difference in global temperatures year-on-year that cannot be explained solely by El Niño, human-driven global warming, or natural “forcings” – such as volcanoes or variations in solar output.

The figure below shows the difference between actual and expected warming in the global temperature record for every year in the form of a histogram. The vertical zero line represents the expectation given long-term global warming and the other vertical lines indicate the warming seen in 2023, 2024 and 2025.

The height of each blue bar represents the number of years over 1850-2024 when the average global temperature was that far (above or below) the expected level of warming. 

Chart showing that the difference from expected warming shows year-to-year variability
Histogram of residuals between actual and expected warming for all years since 1850, with the values for the past three years highlighted. Expected warming based on a 20-year locally linear smooth of the data.

Based on the range of year-to-year variability, temperatures would be expected to spike as far above the long-term trend as they did in 2023 once every 25 years, on average. The year 2024 would be a one-in-88 year event, whereas 2025 would be a less-unusual, one-in-seven year event.

These likelihoods for the past three years are sensitive to the approach used to determine what the longer-term warming level should be.

In this analysis, Carbon Brief used a local smoothing approach (known as locally estimated scatterplot smoothing) to determine the expected temperatures, following the approach used in the WMO “state of the climate 2024” report.

This approach results in a warming of 1.28C in 2023 and 1.30C in 2024, against which observed temperatures are compared.

Other published estimates put the longer-term warming in 2024 notably higher.

Earlier this year, the scientists behind the “Indicators of Global Climate Change” (IGCC) report estimated that human activity caused 1.36C of recent warming in 2024. They also found a slightly lower overall warming level for 2024 – 1.52C, as opposed to the WMO’s 1.55C – because they looked exclusively at datasets used by IPCC AR6. (This meant estimates from the Copernicus/ECMWF’s ERA5 dataset were not included.)

Based on climate simulations, the IGCC report finds the likelihood of 2024’s warmth to be a one-in-six year event and 2023’s a one-in-four event.

Using the same assumptions as the IGCC, Carbon Brief’s approach calculates that 2024 would be a less-common, one-in-18 year event.

However, the IGCC estimate of current human-induced warming is based on the latest estimates of human and natural factors warming the climate. That means that it already accounts for additional warming from low-sulphur shipping fuel, East Asian aerosols and other factors discussed above.

Therefore, the results from these two analyses are not necessarily inconsistent: natural climate variability (including El Niño) played a key role – but this came in addition to other factors. Natural fluctuations in the Earth’s climate alone would have been unlikely to result in the extreme global temperatures seen in 2023, 2024 and 2025.

A cloudy picture

Even if unusual recent global warmth can be mostly attributed to a combination of El Niño, falling SO2 emissions, the Hunga Tonga-Hunga Ha’apai volcano, solar cycle changes and natural climate variability, there are a number of questions that remain unanswered.

Most important is what the record warmth means for the climate going forward. Is it likely to revert to the long-term average warming level, or does it reflect an acceleration in the underlying rate of warming – and, if so, what might its causes be?

As explained by Carbon Brief in a 2023 article, climate models have suggested that warming will speed up. Some of this acceleration is built into the analysis presented here, which includes a slightly faster rate of warming in recent years than has characterised the period since 1970.

But there are broader questions about what – beyond declining SO2 and other aerosols – is driving this acceleration.

Research recently published in the journal Science offered some potential clues. It found a significant decline in planetary reflectivity – known as albedo – over the past decade, associated with a reduced low-level cloud cover that is unprecedented in the satellite record.

The authors suggest it could be due to a combination of three different factors: natural climate variability, changing SO2 and other aerosol emissions and the effects of global warming on cloud reflectivity.

Natural climate variability seems unlikely to have played a major role in reduced cloud cover, given that it was relatively stable until 2015. However, it is hard to fully rule it out given the relatively short satellite record.

Reductions in SO2 emissions are expected to reduce cloud reflectivity, but the magnitude of the observed cloud reflectivity changes are much larger than models simulate.

Models might be underestimating the impact of aerosols on the climate. But, if this were the case, it would indicate that climate sensitivity might be on the higher end of the range of model estimates, because models that simulate stronger aerosol cooling effects tend to have higher climate sensitivity.

Finally, cloud cover might be changing and becoming less reflective as a result of warming. Cloud responses to climate change are one of the largest drivers of uncertainty in future warming. One of the main reasons that some climate models find a higher climate sensitivity is due to their simulation of less-reflective clouds in a warming world.

The Science study concludes that the 2023 heat “may be here to stay” if the cloud-related albedo decline was not “solely” caused by natural variability. This would also suggest the Earth’s climate sensitivity may be closer to the upper range of current estimates, it notes.

Methodology

Carbon Brief built on work previously published in the IGCC 2024 and WMO state of the global climate 2024 reports that explores the role of different factors in the extreme temperatures in 2023, 2024 and 2025.

The impact of El Niño Southern Oscillation (ENSO) on the temperatures was estimated using a linear regression of the annual mean global temperature anomaly on the Feb/Mar Niño 3.4 index. This resulted in an impact of −0.07C, 0.01C and 0.13C for 2022, 2023 and 2024 respectively (with a 95% confidence interval of ±0.13 ºC).

It is important to note that the uncertainties in the ENSO response estimated here also incorporate other sources of unforced internal (modes of variability in other basins such as AMV), and potentially some forced variability. The bar in the combined figure is labelled “El Niño and variability” to reflect this.

For details on calculations of the temperature impact of shipping and Chinese SO2 declines, see Carbon Brief’s explainer on the climate impact of changing aerosol emissions.

Solar cycle 25 was both slightly earlier and slightly stronger than prior expectations with a total solar irradiance anomaly of 0.97 watts per metre squared in 2023 relative to the mean of the prior 20 years. This resulted in an estimated radiative forcing of approximately 0.17 watts per metre squared and an estimated global surface temperature increase of 0.07C (0.05C to 0.10C) with a one- to two-year lag based on a 2015 study. Thus, the impact on 2023 and 2024 is around 0.04C and 0.07C, respectively (+/- 0.025C). This is a bit higher warming than is given by the FaIR model, as the 2015 study is based on global models that have ozone responses to the UV changes, which amplifies the temperature effects a bit.

The Hunga Tonga-Hunga Haʻapai volcanic eruption added both SO2 and water vapour to the stratosphere (up to 55km in altitude). The rapid oxidation of SO2 to sulphate aerosol dominated the radiative forcing for the first two years after the eruption. As a result, the net radiative forcing at the tropopause was likely negative; −0.04 watts per metre squared and −0.15 watts per metre squared in 2022 and 2023, respectively, implying a temperature impact of -0.02C (-0.01C to -0.03C) calculated using the FaIR model.

The post Analysis: What are the causes of recent record-high global temperatures? appeared first on Carbon Brief.

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The world doesn’t need a Paris Agreement for plastics

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Amy Youngman is a legal and policy specialist at the campaigning group Environmental Investigation Agency (EIA).

The chair’s August Aid to Negotiations is being sold as a pragmatic way to rescue the global plastics treaty. However, the text is starting to resemble the architecture of a Paris Agreement-style framework: a patchwork of vague commitments, nationally determined action and reporting, with the hardest substantive decisions left to a future that, my experience following these negotiations tells me, would never arrive.

In March 2022, governments adopted UNEA Resolution 5/14 by consensus, launching negotiations for a legally binding international instrument to end plastic pollution. I joined the global plastics treaty process in Paris in 2023, where hopes of drafting a treaty capable of confronting one of the defining environmental and human health threats of our time were first derailed by procedural warfare.

    Five months later, in Nairobi, I watched the chair close a meeting while delegates still negotiated -allegedly to catch a flight. In 2024 and 2025, in Ottawa, Busan and Geneva, the same small group of blocking states grew bolder, cloaking opposition in language about defending the vulnerable while subsidising a system that fuels the pollution crisis. Offended by ambition, ashamed of nothing.

    A year after the last formal attempt to negotiate a treaty, we are tasked with protecting a fragile process. And despite long-standing support, including legal, policy and technical expertise from my own Environmental Investigation Agency, the chair has excluded observers from the rooms where the treaty’s fate is being decided.

    In that orchestrated quiet, the loudest proposal emerged: the suggestion that the instrument be a “framework convention.” The new Aid, intended to shape the late-September Heads of Delegation meeting, never uses the word “framework”. It does not need to. It strips back substantive obligations and presupposes future action.

    A framework is no match for this crisis

    Framework conventions outline broad principles and leave each country to develop its own plan, often delaying tough decisions to future negotiations that may never happen. This tactic is a political shell game: persuading states that want action now to give up meaningful, binding measures to reach agreement.

    The Chair’s Aid arrives at a framework by subtraction rather than by proposal, which makes it harder to name and potentially easier to accept. Using the Aid, effectively the rejected text from Geneva, as a basis for the next informal meeting in Bangkok will be sold as a way to preserve a distressed UN system and reach consensus in a fractured geopolitical environment.

    This is diplomacy drowning in wishful thinking that the countries fighting binding rules today will approve tougher ones tomorrow. Four years of negotiations and decades of climate diplomacy taught us that this is not a bridge to ambition – this is how ambition dies.

    Modou Fall, 45, head of Senegal Propre (“Clean Senegal”) Association is covered with plastic cups and bags to raise awareness of the damage on the environment caused by waste as he cleans a beach during World Cleanup Day in Dakar, Senegal September 15, 2018. REUTERS/Zohra Bensemra

    Modou Fall, 45, head of Senegal Propre (“Clean Senegal”) Association is covered with plastic cups and bags to raise awareness of the damage on the environment caused by waste as he cleans a beach during World Cleanup Day in Dakar, Senegal September 15, 2018. REUTERS/Zohra Bensemra

    Production is driven by global oil, gas and chemical markets, while products and waste travel across borders. No singular government can regulate its way out of a problem created and amplified by a globalised system.

    Countries have tried, and production kept rising. Now there is plastic everywhere we look, and the cost falls hardest on the people least responsible.

    That failure is why there was consensus to negotiate a treaty, because this crisis requires global action. The purpose was never to list national efforts and call that progress but to create common global rules to address pollution.

    The most politically sensitive issues cannot simply be postponed. How much plastic is produced, which toxic chemicals are allowed in it, which throwaway products are banned, and how future decisions are made are precisely the issues that require global answers. An instrument that refuses to negotiate them will be easier to adopt but useless on arrival.

    Learn from climate governance

    Supporters of a framework approach may point to the ozone treaty as proof that it can work. But the Vienna Convention succeeded for one reason: governments quickly adopted binding upstream controls on ozone-depleting substances.

    Climate offers the opposite warning: a framework followed by contested, delayed and insufficient measures, while emissions keep rising.

    The new chair not only deleted a direct reference to “production and consumption” and bracketed similar preambular language copied from the original mandate. The article on reporting borrows language from the Paris Agreement. Another summer of record heat, fires and floods offers a glimpse of how well that model is working.

    Nothing suggests that the states blocking binding rules today will suddenly accept them tomorrow, and the exponential rise in unchecked plastic production will not pause while governments wait for courage. Blockage is not being resolved, but just pushed forward.

    A framework would lock in the wrong response: unlimited upstream growth with waste management attempting to handle it downstream. No waste system can keep pace with a material engineered for endless growth.

    Keeping to 1.5C of warming is no longer possible – but we must still limit the overshoot

    After four years of INC negotiations, governments know this. States must reject the false choice that the only path to agreement is an instrument too weak to solve the problem it was created to address. Compromise is part of diplomacy. Surrender is not.

    And if the UN keeps pushing that choice, the countries prepared to act must be willing to pursue alternative pathways. Groups of willing governments have built effective agreements before, and existing environmental regimes can deliver new rules without inventing a new empty instrument.

    This process was never meant to find a lowest common denominator. It was to create the rules necessary to change our direction. Bangkok in September will be where the second iteration of this text is shaped. If ambitious countries do not push back, the argument about a framework convention will already be lost by default.

    Negotiations cannot end with governments accepting the crisis rather than solving it. The science is clear and the damage is accelerating. The world does not need another promise to act later. It needs the treaty governments promised to deliver in 2022. 

    The post The world doesn’t need a Paris Agreement for plastics appeared first on Climate Home News.

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    As science comes under attack at UN talks, climate movement splits over how to respond

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    With June’s UN climate talks inching towards gridlock, a group of diplomats calling themselves “Friends of Science” issued a stark warning: climate science was under attack in Bonn.

    The coalition, spanning the world’s richest to its most vulnerable nations, pointed the finger primarily at those who think “science threatens their economic prospects” – a thinly-veiled reference to fossil fuel-dependent states accused of casting doubt on long-held scientific tenets in the UN climate process.

    Fiji’s lead negotiator, Sivendra Michael, went still further. He denounced what he called “a very polluted narrative” taking hold outside the negotiating rooms and singled out ECO, a daily newsletter on the talks produced by Climate Action Network (CAN) International, for overlooking the issue.

    “They are representing developing countries, but they are not representing us,” Michael said. His words hinted at how a rift between governments over the science of global warming has created tensions inside the climate movement.

    Watchers of the UN climate talks have told Climate Home News there is growing unease over where the world’s most influential coalition of climate NGOs stands in an increasingly heated debate about how scientific messages produced by the Intergovernmental Panel on Climate Change (IPCC) are crafted and turned into global climate policy.

    UN sets out narrow path back to 1.5C warming after inevitable overshoot

    CAN’s international leadership has publicly backed a line of argument, championed by some big emerging economies including India, that questions how fair and equitable the models underpinning the work of the IPCC – the UN’s climate science body – are because they are dominated by research from the Global North.

    But some climate activists, including from nations on the frontline of the climate crisis in the Pacific, are increasingly disappointed by CAN’s silence in a connected row over whether the IPCC’s forthcoming assessment report should be finished in time to inform the next UN scorecard of global climate action.

    Over the last two years, India, Saudi Arabia, China, Russia and Kenya have pushed back against attempts by a large coalition of nations to align the IPCC’s AR7 report timeline with the second stocktake of national climate plans under the UN climate process. They claim this would put a burden on developing countries with limited resources and restrict their ability to provide scientific input into the process.

    India flags bias in IPCC assumptions

    CAN International Executive Director Tasneem Essop spoke at an online event last month in which panelists challenged the “Friends of Science” campaign launched at the Bonn talks.

    During the webinar, an Indian scientist and government negotiator set out her view that the IPCC’s way of working and scientific assumptions perpetuate inequity between developed and developing countries – and yet its reports have come to be treated as “scripture” that cannot be questioned.

    In her intervention, Essop did not comment directly on the Bonn science campaign nor on the IPCC timeline issue. But the participation of CAN’s leadership in an event where such criticism of the IPCC was aired has sparked concern in some parts of the NGO community.

    “The way in which CAN International is playing into what could be the destruction of the IPCC inputs into the climate process is very concerning,” said Bill Hare, who was involved in CAN’s establishment nearly four decades ago and now runs think-tank Climate Analytics.

    Science ‘under attack’ from fossil fuel interests at UN climate talks

    He added that it was a mistake for CAN International to align itself with arguments made by India and Saudi Arabia, when those countries are blocking the conclusion of the IPCC’s next key report on cutting emissions in time for it to feed into the next global stocktake, which is due to conclude in 2028.

    Like other insiders Climate Home News spoke to, the veteran Australian climate scientist fears these tensions could hamper CAN’s widely recognised power to influence the talks.

    “The CAN International voice has been very, very important in the process. That voice doesn’t need to be diluted at this moment in history – that would be a really bad move,” Hare said.

    Dialogue to reconcile differing views

    Over the last decade, CAN has been working to transform itself into an organisation that is more representative of, and responsive to, voices and needs in the Global South. In 2019, it appointed Essop – a South African expert on climate, energy, poverty and social justice – as executive director, shifting further away from its European and North American roots.

    CAN International, which functions as the broader network’s secretariat, says it is discussing how to reconcile varying views on the IPCC and the science and equity question among its hundreds of member groups spread across 130 countries.

    “We acknowledge that there are different perspectives within a global network of over 2,000 members on these issues,” CAN International’s Essop said in response to questions from Climate Home News. “Given this diversity, we have democratic processes to build internal agreements.”

    “Science and equity are both fundamental principles for effective climate action and are firmly embedded in CAN’s work,” she added in a written statement. “Putting these principles into practice in a painfully unjust world is not always straightforward, which is why we need continued dialogue across the network.”

    Calls for “fair share” approach

    The webinar in late August – which aimed to untangle what organisers described as “a growing narrative” that “treats science and equity as opposing priorities” – opened with a presentation by Tejal Kanitkar, a prominent Indian climate scientist who also serves on her government’s delegations at the IPCC and UN climate talks.

    Outlining the findings of a paper she co-authored, Kanitkar argued that the IPCC had used scenarios for future emission reduction trajectories based primarily on assumptions put forward by Global North researchers that are skewed against the world’s poorest nations. These, she noted, were then incorporated into the first UN review of global climate action in 2023 and turned into widely cited emissions-cutting targets for limiting warming to 1.5C – a goal the UN has now conceded will be breached, at least temporarily.

    Tejal Kanitkar speaking at a meeting of the IPCC in March 2026. Photo: IPCC Secretariat | Melissa Walsh

    Tejal Kanitkar speaking at a meeting of the IPCC in March 2026. Photo: IPCC Secretariat | Melissa Walsh

    Kanitkar said the “Friends of Science” group included “some of the people who have over-consumed the carbon budget and now use science as a slogan”. When Climate Home News raised the participation of diplomats from vulnerable countries, she said they should be asked why they “accept outcomes that burden the poorest the most”.

    Commenting on Kanitkar’s presentation, CAN’s Essop said everyone knows that “imbalances of power dictate who sits at the table, who designs the models and who determines the assumptions underlying them”.

    Her wider intervention focused more generally on the need to ensure that emissions-reduction pathways follow an equitable approach and account for the “fair share” of action countries need to take based on their historical responsibilities for climate change.

    IPCC working to update models

    Hare later acknowledged that most of the IPCC models used for 1.5C scenarios fail to account for the higher cost of capital and transition financing faced by developing countries. But as this is a “well-known” limitation, the IPCC gives a nuanced reading of the scenarios, and the next generation of models it uses is expected to include more consideration of equity, he added.

    Echoing this, a climate scientist from a developing country currently involved in the IPCC process, who did not want to be identified, told Climate Home News that economic models inevitably contain biases and IPCC authors are already working to identify and correct them.

      Despite criticisms of how IPCC scientific reports have been produced, all governments must sign off on every line of a key “summary for policy-makers” at a dedicated meeting. In 2023, the approved summary included the emissions reduction figures in question that informed the UN’s first global stocktake.

      Irrespective of this wider debate, Hare said the “Friends of Science” campaign, which he supports, is focused on the timing of the IPCC’s next assessment cycle rather than the equity of its models.

      Unresolved row over IPCC report timeline

      A political battle over that time-frame has dragged on for more than two years at successive meetings of the science panel, with governments repeatedly failing to find a solution.

      A large majority of nations have been pushing for a timeline that would ensure the next round of AR7 reports can feed into the UN’s global stocktake. But a group of countries, including Saudi Arabia, India, China, Russia and Kenya, have said at previous IPCC meetings that this would put a burden on developing countries with limited resources and have lobbied for a longer process.

      Member of the “Friends of Science” campaign wears a pin in Bonn. Photo: IISD/ENB – Kiara Worth

      Member of the “Friends of Science” campaign wears a pin in Bonn. Photo: IISD/ENB – Kiara Worth

      In Bonn this summer, the coalition that wants to align AR7 with the 2028 stocktake – which includes diplomats from Fiji, Nepal, the European Union, Switzerland, Sierra Leone and Panama – vowed to ensure that decision-making in the UN climate process remains based on the “best available science”, including the IPCC assessment reports.

      They pointed the finger at “the usual suspects” but stopped short of singling out any countries at the public press conference. Discussions in the previous week had seen Saudi Arabia and India play down the centrality of IPCC reports in the UN stocktake and oppose calls in draft texts to encourage scientific work on scenarios to limit an overshoot of the 1.5C warming goal.

      Bonn upset fuels further tension

      A campaigner with knowledge of internal discussions told Climate Home News that many civil society groups from some of the world’s most vulnerable nations, including the Pacific islands, had expected CAN International to back calls in Bonn defending the centrality of the IPCC in UN climate policy-making.

      Despite this, a day before the “Friends of Science” press conference, CAN published an ECO newsletter that did not mention the issue. Instead, it voiced surprise over the claims of an attack on science happening in the negotiations and accused some of the IPCC’s loudest-defending governments of hypocrisy for continuing to expand fossil fuels and not delivering “fair shares” of emissions cuts and finance to the developing world.

      “We were really shocked we could not find a common position and then this jarring narrative was being pushed,” the campaigner added.

      After divisions hardened in Bonn, Hare said his organisation was approached by “very upset” CAN members from various regions about the stance taken by the network’s international leadership on the issue.

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

      While Climate Home News understands that internal discussions have continued during the summer, including at a CAN leadership meeting in Nairobi in recent days, the campaigner said that CAN International’s endorsement of the recent webinar that directly challenged the “Friends of Science” coalition did not send a reassuring signal.

      Some observers said they feared it would inflame tensions over how climate science is defined and utilised for policy purposes, with consequences reaching well beyond Bonn.

      In a statement to Climate Home News, Essop said that “at a time when communities are experiencing the most horrific impacts of climate chaos, our collective energy must turn to solutions such as filling the Loss and Damage Fund, the phasing out of fossil fuels led by the Global North, and justice for people who are least responsible for this climate emergency”.

      The post As science comes under attack at UN talks, climate movement splits over how to respond appeared first on Climate Home News.

      As science comes under attack at UN talks, climate movement splits over how to respond

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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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