This year marks a decade since nations successfully negotiated the Paris Agreement, a landmark treaty that has been the guiding force for international climate politics ever since.
Yet, with another round of negotiations looming at COP30 in November, there has been growing discontent with the UN climate process.
Critics say the talks are not doing enough to accelerate emissions cuts, tackle fossil fuels or raise climate funds for developing countries, among other concerns.
Influential figures in climate politics and civil society groups say COPs are in need of an “urgent overhaul” and have launched various manifestos for change.
This has been recognised by the Brazilian COP30 presidency, which has acknowledged the “growing calls for change” and asked parties to “reflect on the future of the process itself”.
All of this comes amid concerns about a “crisis” of multilateralism, widespread conflict and escalating climate hazards.
Carbon Brief asked 16 leading experts about how they think the UN climate talks could be reformed, including Christiana Figueres, Todd Stern, Prof Navroz K Dubash, Bernice Lee, Paul Watkinson, Dr Joanna Depledge, Dr Jennifer Allan, Sandrine Dixson-Declève and Li Shuo.
The contributors’ answers are presented via the thematic sections below.
- Has the Paris Agreement been a success?
- How could the negotiations themselves be improved?
- Can UN climate talks drive faster emissions cuts?
- How could COPs ensure broader accountability?
- Do UN climate talks need majority voting?
- What should the role of the COP presidency be?
- Do fossil-fuel companies have too much influence?
- Are COPs too big?
- How could COP participation be improved?
- How can COPs drive change outside the UN process?
Has the Paris Agreement been a success?
Todd Stern, former US special envoy for climate change: Paris has performed well in some respects, including strengthening both its temperature and emission goals in light of evolving science. It also led to a first global stocktake that called for tripling renewable energy and doubling energy efficiency by 2030 – and transitioning away from fossil fuels – in order to achieve net-zero emissions by 2050.
Bernice Lee, distinguished fellow and senior advisor at Chatham House: It can be hard to remember that the process remains one of the most successful multilateral endeavours in recent history. It has delivered what few thought possible: agreement among nearly 200 countries on a global issue that cuts to the core of national sovereignty, economic models and domestic politics. That the COP process delivered the Paris Agreement – and more recently, an agreement to transition away from fossil fuels – is no small feat. It is also easy to forget that, prior to Paris, the world was on track for a catastrophic 4-5C of warming. Today’s pledges, while still inadequate, have bent that curve closer to 2.5-3C – still unsafe, but a meaningful shift…Rather than dwelling on the system’s imperfections, the question is whether it can evolve, realistically and politically. Dismantling the current system is unlikely to yield a stronger or more equitable one with the authority to override national decisions. The current process, after all, emerged from the ruins of earlier failures.
Kaveh Guilanpour, vice president for international strategies at the Centre for Climate and Energy Solutions: In the aftermath of every COP, there are calls to reform the UNFCCC. But we should be aiming for an evolution, not a revolution, for three reasons. Firstly, a revolution would almost certainly not result in something stronger than we already have. It is hard to imagine that it would be possible to adopt the Paris Agreement in the current geopolitical and economic context. Secondly, the Paris Agreement is working, albeit not fast enough. Thirdly, and most importantly, the biggest barriers to the effective functioning of the UNFCCC and delivering on the Paris Agreement are deficiencies in the underlying politics. No amount of tweaking of the UNFCCC process can make up for that.
How could the negotiations themselves be improved?
Dr Monserrat Madariaga Gomez de Cuenca, environmental lawyer at Legal Response International: It is time to fully acknowledge that there is a crisis of trust in the UN climate process and take appropriate measures to limit it. Parties mistrust each other and stakeholders mistrust the limited results emerging from 30 years of climate talks.
Paul Watkinson, former EU climate negotiator: Whilst the negotiating process can be frustrating, it remains essential. I would focus on making the workload more manageable, for example by grouping items on agendas and organising work on a multiannual basis. The aim should be to give enough time to every item – rather than addressing everything together each time – and develop the understanding that not every item needs a negotiated outcome at each meeting.
Kaveh Guilanpour: [We should] embrace the role of multilateral negotiations at the core – and recognise that this is what attracts world leaders and non-parties to COPs – but work towards contextualising the negotiations in a wider ecosystem of climate action, to which they are clearly linked. Do not place all expectations only on the negotiated outcomes.
Christiana Figueres, former executive secretary of the UNFCCC: We could…streamline repetitive and overloaded agendas – and elevate the accountability of COP presidents through a public oath of office, potentially administered by the UNFCCC bureau, that reminds the COP presidency of its role.
Dr Joanna Depledge, research fellow at the University of Cambridge and former UNFCCC secretariat staff member: Overall, the negotiations have proved resistant to anything but very limited reform. Why so? The fact is that many of the perceived inefficiencies are not flaws as such, but inherent to a global process where all nations are sovereign and equal – and all want a say. They are also inherent to the very issue of climate change, which, because it is so multifaceted…inevitably spawns an ever-expanding agenda, while attracting ever more government and civil society participants. And process is politics: moves to restructure the negotiations inevitably come up against powerful forces who know how to maximise their influence in the existing system and far prefer the status quo.
Dr Monserrat Madariaga Gomez de Cuenca: [COPs should] avoid rushed, closed-door negotiations without party consultations, which make implementation impossible. When draft text appears in the eleventh hour and is forwarded to the closing plenary without proper discussion, the possibilities of parties gaslighting each other on the actual “meaning” and “intention” of the text multiply. Language such as “transitioning away from fossil fuels” or the path towards the “Baku to Belém Roadmap to $1.3tn” – where the wording is not clear – allows parties to cherry-pick the most favourable interpretation, undermining the implementation of decisions that were already difficult to achieve.
Dr Joanna Depledge: Streamlining agendas and limiting government delegation size are worth fighting for, but imposing criteria for selecting COP hosts and excluding private companies involved in high-carbon activities are non-starters. If the real problem is that the COP is not taking decisions in line with the science, then the answer is not tinkering around the edges of procedure and process. What is needed is a major strategic rethink and more fundamental reforms – notably to decision-making practices and voting – as I argue elsewhere.
Harjeet Singh, founding director at the Satat Sampada Climate Foundation: The process must change: streamline negotiations, review consensus rules and ban fossil-fuel lobbyists from influencing texts. Centre the voices of Indigenous peoples, frontline communities and civil society. And scale up public climate finance to enable a just transition and real support for adaptation and addressing loss and damage – by making polluters pay. The recent International Court of Justice advisory opinion has reinforced the demand for climate reparations. COP30 must open a new era of accountability and justice.
Can UN climate talks drive faster emissions cuts?
Dr Jennifer Allan, senior lecturer in international relations, Cardiff University: The UNFCCC is only as effective as parties allow it to be. The Paris Agreement is working precisely how some feared and how some major emitting countries hoped. It is premised on the promise of transparency: that national reports and the global stocktake, coupled with principles of progression, will – somehow – inspire climate ambition. But transparency is not the same as accountability.
Todd Stern: The Paris regime itself has an important role to play. For starters, the regime needs to develop much more of a broad partnership in the spirit of the 2015 High Ambition Coalition. Part of such a shift will depend on considering whether country emission targets are adequate. Of course, Paris was built on the principle of “nationally determined contributions” and that principle cannot be thrown overboard. But Paris was also built on the promise that it would strive to prevent dangerous climate change, that new emission targets every five years would reflect countries’ highest possible ambition and that global stocktakes would, in fact, take stock.
Claudio Angelo, head of international policy at the Climate Observatory: The “nationally determined” nature of nationally determined contributions (NDCs), and the fact that no assessment of progress is formally done outside the five-year period of the global stocktake, mean that the ambition gap will become more difficult to close the more urgent it becomes to close it. The irony of it is that the Paris architecture was tailor-made to accommodate the idiosyncrasies of the US, which has pulled out of the agreement anyway.
Prof Navroz K Dubash, professor of public and international affairs at Princeton School of Public and International Affairs: A bumper sticker for reform of the UN climate talks might read: “Less talk of ambition; more action on implementation”. An “ambition-first” approach rests on extracting national statements of emissions reduction intent, leveraging these up through country “naming and shaming” and strengthening compliance through enhanced accountability. But the conditions are not favourable for this approach. National politics rarely privilege emissions reductions over other objectives and global politics is increasingly non-responsive to climate shame. By contrast, the conditions for a “learning-by-doing” approach based on on-the-ground implementation appear brighter. Many countries are experimenting with pragmatic efforts to turn their economies in low-carbon directions.
Todd Stern: There is nothing about the nationally determined character of country pledges that says countries cannot be questioned, prodded and critiqued. Protecting thin skin is not as important as protecting a liveable world.
Prof Navroz K Dubash: How might global talks enable learning by doing, rather than doubling down on ambition-first approaches? NDCs could be liberated to be templates for experimentation rather than rigid bases for accountability alone. Detailed sectoral low-carbon development pathways would highlight country commonalities, reveal productive scope for international cooperation and incentivise finance…A renewed international process should be focused on the hard, detailed work of enabling low-carbon, resilient development transitions and less on extracting statements of intent.
Kaveh Guilanpour: [We should] move to an approach where progress is measured predominantly by the impact of implemented national level policies, not NDCs on paper. Focus as much on enhancing international cooperation to deliver implementation as on increasing formal ambition on paper through NDC target-setting.
How could COPs ensure broader accountability?
Paul Watkinson: The biggest opportunity to support implementation is outside the formal process, putting order and structure into the “action agenda”. It has grown enormously in recent years and there have been many valuable initiatives…But there has been insufficient continuity and not enough follow-up and tracking to ensure that what is announced and promised is delivered. That is why I welcome the proposal of the incoming Brazilian COP30 presidency to structure the action agenda around six broad themes, drawn from the outcomes of the global stocktake, including a cross-cutting theme around enablers including the vital role of finance. They have the power, in close coordination with the high-level champions, to relaunch the action agenda on stronger foundations that could serve for years to come.
Dr Jennifer Allan: Within the negotiations, there is a glaring need to track the many commitments made outside of the regular negotiation process, either in presidency-led declarations or cover decisions. A central, publicly available hub needs to collate these promises and track progress. Presidencies may broker these commitments, but have few incentives to follow up on them.
Bernice Lee: What can – and must – change is how the system functions. Every decade or so, the climate regime has adapted – from Kyoto’s top-down legalism to Paris’s nationally determined flexibility. These shifts were not just philosophical, they also enabled new capacities. The collapse in Copenhagen helped catalyse renewable energy investment plans, while Paris introduced NDCs. The next phase must embed delivery and equity more deeply into the process including, for example, mechanisms aligning corporate transition plans with country transition, national policies and sectoral pathways. The outcomes of any reform process should mean fewer theatrics, earlier decisions and sharper accountability. All of this would enhance not only country but also public engagement, as well as the credibility of the global climate process.
Harjeet Singh: Rather than catalysing ambition, the Paris Agreement has been used by developed countries to shirk their historical responsibilities…It is not the Paris Agreement or the UNFCCC that failed – it is rich countries that undermined the system to protect polluters and preserve an unsustainable growth model. True reform begins with accountability. Wealthy nations must be held responsible for their historical emissions and must pay for the loss and damage they have caused.
Sandrine Dixson-Declève, honorary president at the Club of Rome and executive chair of Earth4All: Strengthen climate target enforcement through scientific oversight, peer review and robust reporting – ensuring governments, COP presidencies and corporations are held accountable. [There should be] a permanent scientific advisory body within the COP. Science must be central to negotiations, with all delegations regularly briefed on the latest data around risks, equity, solutions and scenarios.
Prof Navroz K Dubash: Ambition and implementation can be complementary, but they are not necessarily so. The former is driven by a relentless focus on emissions, comparability in emission pledges and building accountability. The latter is enabled by linking climate to other objectives, seeking country-specific formulations that buy political support and flexible experimentation that allows for learning from failure. Being more, not less, in the sectoral weeds might reveal opportunities not apparent from the stratospheric heights of climate negotiations. Well-developed, home-grown visions of sustainable futures are the most robust basis for developing countries’ legitimate claims for finance and other support.
Do UN climate talks need majority voting?
Erika Lennon, senior climate attorney at the Centre for International Environmental Law: Voting is the elephant in the room. The parties to the UNFCCC have never been able to adopt the “rules of procedure” because they cannot agree on the provision related to voting in the absence of consensus. Instead, they proceed meeting after meeting using them as “draft rules of procedure”. This has created a race to the bottom whereby countries that want to stall progress can do so. For 29 years, other parties have had to agree to the lowest common denominator in the name of consensus.
Claudio Angelo: The decision made in 2023 to “transition away from fossil fuels” needs both fleshing out and monitoring, but it is nowhere to be seen in the formal negotiations towards Belém. Such omissions reflect one fundamental problem of the UNFCCC and one fundamental flaw of the Paris Agreement: the consensus rule. Some countries are now shamelessly backtracking on their previous commitment and saying that any mention of cutting back on fossil fuels anywhere is a red line for them…A handful of countries are holding the future of humanity hostage because they can block whatever they want [due to the consensus rule]. Even COP presidencies that do want to move the agenda forward are afraid to be bold, lest “the process should collapse”. But a process that is unfit for purpose might as well collapse.
Christiana Figueres: In the context of the formal negotiations, we could reconsider our tradition of having to adopt all decisions unanimously. UNFCCC procedures require consensus for the adoption of decisions, not necessarily unanimity. The difference is important and admittedly challenging to manage, but worth examining.
Erika Lennon: The fix would be to adopt the rules of procedure, including the paragraphs on voting. The UNFCCC would then join many other multilateral environmental agreements – and its own financial instruments – that sometimes use majority voting.
Bernice Lee: In recent months, many well-meaning critics have called the UN multilateral climate process broken, arguing it should be dismantled and replaced, but with no viable alternatives waiting in the wings. Reforming core procedures – such as introducing majority voting or amending the convention – would require agreement from three-quarters of countries, followed by domestic ratification. Even without today’s fractured geopolitics, this would be a tall order.
What should the role of the COP presidency be?
Dr Monserrat Madariaga Gomez de Cuenca: [COPs should] avoid adding more pressure by clarifying duties and processes for the COP president. Rules of procedure simply give the COP president the power to formally conduct the negotiations, which should be done in a neutral manner. Increasingly, we see COP presidents setting exceedingly ambitious plans for their respective COPs. Ideas of “success” and “legacy” permeate what should be a facilitative role towards the collective progress of UN climate talks. COPs finish with statements and reports of achievements that do not reflect the actual progress. Reviewing the conduct of negotiations and the role and expectations of COP presidencies could help in restoring some of the damaged trust in the process.
Prof Thomas Hale, professor in public policy at the University of Oxford: The “action agenda” needs to escape the “boom-bust” cycle that shifting presidencies and high-level champions have imposed on it, in which new announcements trump delivery. The COP30 presidency has laid out a positive approach here, but the acid test lies in making it real.
Sandrine Dixson-Declève: Only countries with high climate ambition should be eligible to host COPs.
Li Shuo, director of the China Climate Hub at the Asia Society Policy Institute: Instead of – or alongside – three more paragraphs specifying how the world will “transition away from fossil fuels” or “triple renewable energy”, how about three renewable projects in the COP host country, to be announced in conjunction with the climate summit?…Efforts to advance the implementation agenda through additional multilateral rulemaking and COP decisions risk missing the point. The COP presidency…could showcase a handful of large‑scale renewable energy projects in their own countries, backed by concrete financing. Such a “trade fair” function of the COP would help bridge the widening gap between what is agreed at COPs and what is happening on the ground.
Do fossil-fuel companies have too much influence?
Erika Lennon: The fossil fuel industry’s survival depends on the UNFCCC’s failure, as meeting the goals of the UNFCCC and Paris Agreement undeniably means phasing out fossil fuels. It is therefore no wonder that, since the beginning, fossil-fuel industry lobbyists have been present at COPs and working to undermine ambition.
Dr Jennifer Allan: Presidencies have much to answer for and can be key to raising accountability. COP is becoming the new Davos: a place for billionaires to meet, without scrutiny of their activities or announcements. This must end. Presidencies should revoke invitations to [Amazon chief executive] Jeff Bezos and others who have been offered high-level platforms.
Erika Lennon: Parties could adopt a conflict-of-interest policy to, at the very least, make [fossil-fuel lobbyists’] influence transparent and subsequently exclude those who aim to unduly influence the process. Parties, including the presidency team, could refuse to give them badges…In addition, they could end greenwashing at COPs in the form of corporate sponsorships and pavilions.
Are COPs too big?
Prof Thomas Hale: COP is both too big and too small for an era of implementation. Its cost and complexity eat up scarce resources. Meanwhile, it creates a gravity well that warps the climate community’s work into an annual rush to the end of the year…At the same time, even the biggest COPs are puny compared to the problem. Climate change demands action from all of society…In this complex system, the UNFCCC process plays the critical function of setting agendas and goals. No other body has the multilateral legitimacy to serve as a lighthouse.
Dr Jennifer Allan: Climate summits could shift from a talkshop to a demonstration of leadership if invitations are only extended to countries that have submitted and maintained more progressive NDCs and are implementing them.
Prof Thomas Hale: We need COPs to be everything, everywhere, all at once. Alongside a single, two-week meeting in one place, we need lots of smaller, focused meetings in many places. Instead of an intergovernmental process that talks about action, we need to fully shift the “action agenda” into the heart of the UNFCCC. The good news is that the elements of this shift are already well in motion, with more and more cities hosting “climate weeks”…Regional meetings with more flexible formats reach more people, in a more targeted way, much more cheaply and efficiently than a COP.
Dr Jennifer Allan: I’ve been researching the role of side events, pavilion activities and Global Climate Action Hub panels in the “expo” that now dominates COP space and participation opportunities. There has been a decided shift, from a smaller number of events focused on negotiation and implementation to a huge array of panels showcasing new initiatives or national actions. It is about what is new, not following up on what has been agreed. Side events and Global Climate Action Hub events could shift focus under the secretariat and the high-level champions. Pavilion spaces could be reserved for those who can demonstrate that their presence will advance climate action.
Sandrine Dixson-Declève: COPs must evolve from negotiation-heavy forums to more frequent, smaller, solution-focused meetings centred on progress and implementation, with broad stakeholder participation.
How could COP participation be improved?
Erika Lennon: Civil society, youth, Indigenous peoples, women, local communities and people with disabilities, among others, have increasingly faced shrinking civic space in the UNFCCC process. They have to fight to have their voices heard, to be present in the rooms where decisions happen, for access to information and open decision-making, and to assemble peacefully.
Shreeshan Venkatesh, global policy lead at Climate Action Network International: Structural barriers…undermine inclusivity and equitable participation in UNFCCC meetings, from the high cost of accommodation at COPs to discriminatory visa practices and shrinking civil society quotas. These barriers must be dismantled to ensure all parties and stakeholders can participate fully and on equal terms.
Erika Lennon: Parties should incorporate and support participation not only at COPs, but also in climate action and decisions on the ground. They can do this by creating space across all agenda items to hear from rightsholders and ensuring human rights and civic space are guaranteed during all negotiations.
Shreeshan Venkatesh: Civic space and freedoms are under threat, even at COPs. Host agreements must guarantee freedom of speech, assembly and accessibility, backed by an independent body to address violations.
How can COPs drive change outside the UN process?
Sandrine Dixson-Declève: COP must transform from a forum of negotiation to a platform of delivery, inclusion and accountability, anchoring climate action in the lived realities of people and the demands of science.
Kaveh Guilanpour: There should be a thorough and honest analysis of the value add of the UNFCCC process and what is best left to other fora.
Christiana Figueres: While some negotiations remain necessary, the most urgent action has shifted to implementation in the context of market forces and climate economics. There is no doubt that civil society, businesses, cities and communities are moving faster than governments. These actors, traditionally considered and labelled as mere “observers” in the formal UNFCCC space, have become the true engines of transformation. One could consider the pros and cons of creating a semi-detached “real world” space alongside COP – one that amplifies their progress, showcases innovation and feeds actionable insights back into the formal process.
Todd Stern: The Paris regime has a role to play in encouraging and tracking strong action outside its purview. This includes the public and private sectors working together on rapid decarbonisation and on unlocking the kind of large-scale investment needed for countries in the global south to build sustainable and resilient economies.
Shreeshan Venkatesh: The UNFCCC, and other multilateral fora that have become central to the formulation and implementation of climate policy and international cooperation, must align with international law. This includes the recent advisory opinions from the ICJ and the Inter-American Court of Justice, and the obligations they clearly lay out.
Claudio Angelo: [There is] a final, bigger problem, which no UNFCCC reform can solve: the climate regime is a child of the democratic world order and the lynchpin of that world order has become a rogue state. The rise of the far-right and the erosion of democracy are rendering multilateralism itself useless – a world that is unable to stop genocides in Gaza and Sudan can’t solve the climate crisis.
The post COP experts: How could the UN climate talks be reformed? appeared first on Carbon Brief.
This summer has seen Europe suffer through a series of record-breaking heatwaves.
Amid widespread media coverage of the number of deaths and the influence of climate change, the UK’s Daily Telegraph reported on new research with the incorrect headline: “Heatwaves caused by fall in pollution.”
The article was shared on social media by Richard Tice – deputy leader of the hard-right, climate-sceptic Reform UK party – along with a number of prominent rightwing commentators.
Tice claimed that “net stupid zero is contributing to rising temperatures, not helping”, adding that “we have been gaslit and lied to”.
GB News followed up with its own article, incorrectly headlined: “Britain’s scorching heatwaves caused by falling pollution levels, researchers find.”
Scientists tell Carbon Brief that the framing of heatwaves being “caused” by declining air pollution is “wrong”.
While a drop in pollution has reduced the cooling impact it has had in the past, the scientists say, Europe’s summer heatwaves are primarily becoming more extreme “as a result of greenhouse-gas-induced warming”.
Another scientist adds that “any attempt” to link this research to net-zero policies is “simply wrong”.
Fast warming
The extensive reporting around Europe’s heatwaves in recent months has often mentioned that Europe is the world’s fastest-warming continent.
The new study in question aims to unpack why Europe’s summer temperatures are rising more quickly than other regions of the northern hemisphere’s mid and high latitudes.
The research – published in Geophysical Research Letters – explores the role of air pollution and, specifically, how it affects circulation patterns in the atmosphere.
(The study focuses on long-term trends in European summers and does not include the very recent heatwaves.)
Human-caused emissions of aerosols – tiny, light‑scattering particles produced mainly by burning fossil fuels – have long acted to “mask” global warming. This is largely because they absorb or reflect incoming sunlight and influence the formation and brightness of clouds.
To understand how the climate of Europe – or any region – is changing, scientists need to take into account a whole range of factors, says Prof Bjørn Samset, a research professor at Norway’s Center for International Climate Research (CICERO), who was not involved in the work.
This includes “greenhouse gases, aerosols, land-use change, natural variability and how they all interact”, he says, adding:
“The effects of air pollution on circulation, which is the topic here, has long been difficult to pin down.”
As European countries improved their air quality through the second half of the 20th century, the cooling effect of aerosols has gradually been removed.
This can boost heatwaves in two ways – directly, by letting more sunlight reach the land surface and, indirectly, by influencing the jet stream.
Using hundreds of simulations from nine climate models, the new study finds that a decline in aerosols is resulting in more frequent “quasi-stationary Rossby waves”.
Rossby waves are huge meanders in the jet stream. Occasionally, they become slow-moving – or “quasi-stationary” – which allows weather systems to get stuck over one region, leading to prolonged heatwaves.
These circulation changes have contributed to Europe’s rapidly warming summers.
However, while Europe’s heatwaves are being influenced by declining aerosols, it is “wrong” to say they are being “caused” by them, says Prof Erich Fischer, a climate scientist at ETH Zurich.
Fischer, who was not involved in the study, tells Carbon Brief:
“Heatwaves are caused by high-pressure systems and are now much more frequent and intense because they are happening in a climate that is much warmer than 100 years ago as a result of greenhouse-gas-induced warming.
“The paper shows that the greenhouse-gas-induced summer warming had been temporarily masked by air-polluting aerosols. The full extent for European summers only becomes visible now as the air-polluting aerosols have declined.”
Samset adds:
“Air pollution never causes or removes global warming, it only temporarily moderates it.”
Study lead author Dr Pedro Roldán‐Gómez, an associate researcher at the Barcelona Supercomputer Centre, is quoted in the Daily Telegraph saying that “most” of the “excess warming” in Europe, beyond that of comparable regions in the northern hemisphere, can be linked to declining aerosols.
But, earlier in the article, the newspaper interprets this as, simply, “most of the extra heat experienced in Britain and Europe” is down to air pollution.
GB News uses a similar phrasing, reporting that “much of the additional warming across Britain and western Europe since the 1980s is linked to the sharp decline in airborne particles known as aerosols”.
This is “misleading”, says Fischer, while Roldan-Gomez tells Carbon Brief that this is a “tricky point”, which “could lead to wrong interpretations if not properly explained”. He adds:
“The contribution of greenhouse gases is, in any case, the most important factor.”
Cleaner air
The Daily Telegraph’s article was seized upon by Reform’s Richard Tice to claim that “cleaner air” was causing higher temperatures, rather than CO2.
This continued his position – refuted by long-established climate science – that CO2 does not drive global warming.
Tice also claimed in his post that net-zero policies are “contributing to rising temperatures”. Tice appears to be linking declining air pollution to a shift from fossil fuels to renewable energy.
Samset points out that net-zero became a goal “decades later” than the cumulative efforts to reduce air pollution since the 1980s and that it is “simply wrong” to link it to the study.
“The scientific community will keep working to understand how greenhouse gas warming and air pollution interact,” he says, but “nothing we do will change the fact that the consequences of global warming are due to human-induced CO2 emissions”.
Fischer adds:
“Let us not forget that cleaning up air-polluting aerosols is highly desirable. According to the World Health Organisation, 7 million people still die prematurely every year due to air pollution.”
Clean air legislation
Finally, the Daily Telegraph article and the study itself both attribute Europe’s declining air pollution from the 1980s onwards to the Montreal Protocol.
This is a “glaring error”, Samset says, and it is “surprising that it wasn’t picked up” in the peer-review process for the study. He explains:
“The Montreal Protocol did not deal with air pollution. It dealt with ozone-depleting gases and has been an extremely successful multi-national effort against environmental damage. “
Clean air legislation was already in place in many European countries by the time the Montreal Protocol was signed in 1987, says Samset.
In response, Roldán‐Gómez says that while the protocol did not target aerosols specifically, it “boosted the clean air policies”.
The post Factcheck: No, Europe’s heatwaves are not being ‘caused’ by declining air pollution appeared first on Carbon Brief.
Factcheck: No, Europe’s heatwaves are not being ‘caused’ by declining air pollution
Empowering women through greater access to finance could “strengthen” households’ resilience to “climate shocks”, according to a new study.
Published in Climate Risk Management, it analyses the impact of financial access on “women-headed households” in sub-Saharan Africa.
The study finds that where women had formal financial access – such as through owning a bank account – households were more able to withstand short-term shocks.
It adds that “climate shocks”, such as extreme weather events and the impacts of climate change, can cause economic crises, which destabilise communities and households.
However, the authors say that in order to protect households from long-term climate vulnerabilities – including “droughts, floods and sea-level rise” – financial access would need to be paired with wider efforts to tackle gender inequality.
They add that the findings could have important implications for policy in sub-Saharan Africa, where many countries and households are vulnerable to climate disasters.
Financial inclusion
The study highlights that entrenched gender disparities mean many women still have unequal access to financial services in sub-Saharan Africa
For example, women are still less likely to have their own bank accounts and instead are often dependent on male relatives for access to finance.
The number of women with access to an account in the region had risen to 52% as of 2024, according to data from World Bank Group.
However, as shown in the chart below, the gap between men and women has also increased, rising from just under 5 percentage points in 2011 to 12 in 2024.
Using survey data from Afrobarometer, the new study analyses 25,511 women-headed households across 37 sub-Saharan countries.
The authors use the Organisation for Economic Co-operation and Development’s (OECD) framework to measure “financial inclusion”. This looks at factors such as having a bank account, owning a mobile phone and having internet access.
Francis Anaisie, a co-author on the study, tells Carbon Brief the researchers were motivated by the UN’s sustainable development goals (SDGs). Anaisie, an economist at the University of Cape Coast, Ghana, says the study specifically looked at SDGs five and 13, on gender equality and addressing climate issues. He adds:
“Financial inclusion is one of the key policy tools for empowering women or for empowerment. But as to whether this actually translates into better climate outcomes for women is not known or is limited; this study seeks to address that gap.”
The study finds households with higher levels of financial access for women had higher levels of women’s empowerment, when this is defined as the ability to make choices and have control over economic and social outcomes.
This was checked by cross-comparing financial access against different measures of women’s empowerment, such as financial security, voting rights and connection to communities.
In particular, the study found that “financially included” women had greater political and economic empowerment, such as financial security and voting rights. On some measures of social empowerment, however, the link was weaker – financial access alone was not enough to erase cultural and social barriers to gender equality.
Women and climate change
It has been well documented that women are more vulnerable to the impacts of climate change than men.
Environmental shocks affect women disproportionately due to a range of factors. These include income disparities, higher rates of displacement and unequal access to land.
Financial inequality and barriers to economic resources, such as needing internet access to make digital payments, play a key role in climate vulnerability, says Tracy Kajumba. She is director for the Least Developed Countries initiative for Effective Adaptation and Resilience (LIFE-AR) interim secretariat at the International Institute for Environment and Development (IIED).
Kajumba, who was not involved in the study, explains to Carbon Brief:
“Women are on the front line doing farming, planting, harvesting and these things that are all impacted [by climate change]. If they don’t have the income to invest either in drought-resistant crops or water-saving technologies, it becomes difficult for households to adapt.”
Calculating climate resilience
The new study measures the impact of financial inclusion on women’s empowerment and, in turn, on climate resilience.
It evaluates a household’s ability to withstand and recover from “shocks and stressors” by using a UN Food and Agriculture Organization metric for “resilience index measurement and analysis” (RIMA).
For example, questionnaires are used to gather information about households in certain areas. The data is then used, together with key indicators, to quantify a household’s resilience to food insecurity, climate variability and economic crisis, amongst other risks.
The 25,511 households surveyed across sub-Saharan Africa were found to be relatively resilient overall and had a high capacity to bounce back from climate shocks. However, they had much lower ability to adapt, in order to build protective capacity in advance of extreme events.
In addition, the study finds that women’s financial empowerment had a positive impact on a household’s ability to “absorb” a climate shock, suggesting that financial access is critical for responding to climate change.
Increased empowerment through financial access enables women to make decisions about planting crops, to access credit in emergencies and to buy or sell food at a better price, the study notes.
For example, it says increased financial access and women’s empowerment help households to deal with the immediate consequences of an extreme weather event, such as a drought. This could be through building community mutual-support networks and by enabling access to savings, to keep the household running.
Anaisie says the study shows women’s empowerment has a significant impact on climate resilience. He tells Carbon Brief:
“If we include women in the financial system, in the case of any climate issue they can save, they can be independent, they can rely on investment to absorb these shocks. This empowerment will help them to be more resilient to climate shocks…We can make progress because SDG goals are all about inclusiveness. It’s all about inclusive growth.”
However, the study notes that financial access does not necessarily create long-term change, which would make the household less vulnerable to extreme weather in the first place.
The authors suggest that lasting structural and cultural change is important for bringing about long-term resilience. They say that policies to address gender inequalities would help bring this about.
They say such policies could include gender-sensitive agricultural credit schemes, subsidised climate insurance for women farmers in drought-prone regions, joint land-titling programmes and quotas for women in local climate-adaptation committees.
Such policies would have helped women impacted by recent severe floods in Ghana to protect their savings, Anaisie explains. He tells Carbon Brief:
“Women are engaged in economic activities, especially informal activities. They have resources and money, but when the flood came in, many women lost that. If they had access to insurance, this flood wouldn’t have cost them that much.
“So, if the government comes out with financial initiatives, training, civic education and gender-focused initiatives, leadership training, women will be empowered and this will translate into their resilience with regards to climate change.”
Addressing climate vulnerability in sub-Saharan Africa
The study could have policy implications for sub-Saharan Africa, a region particularly vulnerable to the effects of climate change. The region faces increasingly extreme weather, heatwaves, droughts, wildfires and floods, as well as food scarcity and threats to crops.
The study suggests that policies to address structural and cultural barriers to women’s financial autonomy could be a key way to build climate resilience across the region.
However, it recognises that even where financial access is expanded, gender norms and cultural constraints continue to shape women’s social empowerment. This, in turn, affects their ability to adapt to climate change in the long term.
Ultimately, addressing structural inequalities is needed to minimise climate vulnerability, says Kajumba. She adds that supporting adaptation with financial access can allow households to absorb shocks without falling into poverty – and to rebuild after climate impacts.
Kajumba says that supporting adaptation with women’s financial access can allow households to absorb shocks without falling into poverty – and to rebuild after climate impacts. She adds:
“When they are supported [with] microloans, savings and all that, you will see change in income, change in households, change in health and education for the children as well.”
However, Kajumba notes that structural inequalities still “amplify” women’s vulnerability to climate impacts and make it harder for them to exercise agency and leadership. She adds:
“The tools that are being used are not always favourable for women…When we look at women in leadership and participation, you cannot lead or you cannot participate unless you have some level of income.”
The post Access to finance ‘strengthens climate resilience’ among sub-Saharan women appeared first on Carbon Brief.
Access to finance ‘strengthens climate resilience’ among sub-Saharan women
As 2026 passes its halfway point, the world is watching one of the most rapidly intensifying El Niño events in the modern record take shape in the tropical Pacific.
The developing El Niño is boosting expectations for global temperatures, both this year and next.
El Niño is the warm phase of a recurring climate pattern in the tropical Pacific that releases heat from the ocean into the atmosphere, temporarily raising global temperatures and reshaping rainfall and extreme weather around the world.
Carbon Brief’s “state of the climate” report in April gave 2026 a 19% chance of setting a new global temperature record.
That chance now stands at 35% – a near-doubling in four months – with virtually all of the change driven by ever-stronger El Niño forecasts.
The key findings from the first half of 2026 include:
- The first six months of 2026 were the third-warmest start to a year on record – around 1.4C above pre-industrial levels – behind only 2024 and 2025.
- While the first few months of the year came in as the fourth or fifth warmest, both May and June were the second-warmest ever recorded as El Niño conditions took hold.
- El Niño conditions arrived in April and reached the threshold for a “strong” event by June, when the Niño3.4 index reached 1.6C. Of the 667 model runs Carbon Brief examined, 91% project a peak later this year that is above the strongest El Niño in history.
- The chance that 2026 beats 2024 as the warmest year on record has risen to 35%. Carbon Brief’s central estimate remains that 2026 will be the second-warmest year, at around 1.51C above pre-industrial levels.
- Whether 2026 sets a record will depend on the dataset: the odds range from around two-in-three in NASA and Berkeley Earth data to around two-in-10 in ERA5 and one-in-10 in the JRA-3Q reanalyses.
- June 2026 was western Europe’s hottest June on record, amid a heatwave that set hundreds of individual records. Nearly 9% of the world’s surface saw record June warmth.
- The developing El Niño will have its largest impact on 2027, which Carbon Brief projects to be around 1.7C above pre-industrial levels – this would comfortably set a new record for the warmest year.
- Arctic sea ice has spent 39 days of 2026 so far at, or below, record daily lows following its joint-lowest winter maximum in the satellite era.
Third-warmest start to a year
Carbon Brief analyses records from six different groups that report global surface temperatures: NASA GISTEMP, NOAA GlobalTemp, Hadley/UEA HadCRUT5, Berkeley Earth, Copernicus/ECMWF ERA5 and the JMA JRA-3Q reanalysis.
The first half of 2026 was the third warmest on record in every one of the six datasets, behind only 2024 and 2025. The figure below shows annual temperatures since 1970, along with the 2026 year-to-date average (January-June) for each group.
January 2026 was only the fourth- or fifth-warmest January on record, as lingering weak La Niña conditions suppressed temperatures. Since then, each month has climbed the rankings.
La Niña is the cool phase of the El Niño-Southern Oscillation (ENSO). It typically brings wetter conditions to Australia, Indonesia and equatorial South America and drier conditions to the southern US.
March was second-to-fourth warmest across datasets, April the third and both May and June were the second warmest ever recorded, behind only the corresponding months of 2024.
The chart below shows how June 2026 (thick red line) came in around 0.08C below the June record set in 2024 in the average of the six datasets.
Meanwhile, Copernicus reported that global sea surface temperatures over the ice-free oceans set a new June record.
A record-breaking El Niño
ENSO is the largest source of year-to-year variability in global temperatures.
The most common way to assess the strength of an El Niño or La Niña event is by looking at the sea surface temperature anomaly in the “Niño3.4” region of the tropical Pacific.
El Niño and its sister La Niña occur when temperatures in the tropical Pacific are more than 0.5C (El Niño) or less than 0.5C (La Niña) below normal, where normal is defined by removing the effects of long-term climate change.
The thresholds for defining the strength of an El Niño or La Niña are above/below 1C for “moderate” events, 1.5C for “strong” events and 2C for “very strong” (or “super”) events.
After two years dominated by La Niña conditions, the tropical Pacific flipped decisively in April when the Niño3.4 index crossed the 0.5C El Niño threshold. It subsequently reached 1C in May and hit 1.6C in June, marking one of the fastest onsets in the observational record.
In the first few weeks of July, the index shot above 2C, significantly outpacing the speed at which any prior El Niño events developed.
Forecast models expect even more to come.
An analysis by Carbon Brief of the median of 667 model runs from 14 different modelling groups suggests that sea surface temperatures in theNiño3.4 region could peak at 3.59C between July and December.
More than 91% of runs predict the strongest El Niño event in the modern record. The previous record was set during the event of 2015-16, when temperatures peaked around 2.75C.
This is shown in the chart below, which features a histogram of the likelihood of different possible 2026 El Niño peaks across all the models on the top. The forest plot beneath shows the best estimate and range of outcomes predicted by each individual model.
The median forecast in every one of the 14 models suggests a peak that exceeds the 2C “super” El Niño threshold, with most models peaking in November or December.
Some caution here is warranted, however. Raw model Niño3.4 anomalies are measured against a fixed climatology. Because the entire tropical ocean has warmed due to human-caused greenhouse gas emissions, the models tend to overstate event strength relative to the historical record.
A cleaner comparison uses the relative Niño3.4 index (RONI), which subtracts the average tropical ocean warming.
This relative measure suggests the median forecast peak for El Niño in the latter half of 2026 is 3.1C. The prior record stands at a lower 2.69C, set in 1982-83.
Nevertheless, 77% of model runs still show a new record event occurring. This is shown in the chart below.
In summary, on both indexes, the central expectation is now for the strongest El Niño in the observational record.
Model forecasts made in the spring and early summer have historically shown some bias toward overpredicting event strength. However, forecasts made after the spring are considerably more reliable.
Widespread record warmth and a massive European heatwave
The map below shows the temperature anomaly for the first half of 2026 in the ERA5 dataset, relative to a 1981-2010 baseline period.
It shows how the largest warm anomalies were found across the Arctic – particularly north of Scandinavia and Svalbard – as well as western Europe, the western US, northern Mexico, central Asia, western China, eastern Russia and the Antarctic Peninsula region.
The developing El Niño is clearly visible as a tongue of warm anomalies stretching along the equatorial eastern Pacific. Only a few regions – central Canada, Alaska and parts of the Southern Ocean – saw temperatures below the 1981-2010 average.
Where 2026 ranks against history is even more striking. The map below shows where the period of January-June 2026 ranked among all 87 years in the ERA5 record, which stretches from 1940 to 2026. Grid cells marked in red saw temperatures in the first half of the year that were in the top-five warmest years.
More than 30% of the global surface had a top-five warmest start to the year and 7.1% saw its warmest on record, including much of western Europe, the eastern equatorial Pacific and the seas around Japan.
Not a single grid cell had a top-five coolest start to the year. In June alone, 8.9% of the world’s surface saw record warmth for the month. This is illustrated in the map below, where grid cells marked in red saw temperatures that were in the top-five warmest years and grid cells in blue in the top-five coolest.
The standout regional temperature event was a heatwave that struck Europe in late June.
Western Europe had its hottest June on record, recording an average temperature of 3.05C above the 1991-2020 average and beating the record set only a year earlier, according to Copernicus. A heat dome over 22-30 June broke 10 all-time national heat records and around 400 long-record station records.
France set a new June national record of 44.3C, while the UK broke its June record on three consecutive days, reaching 37.3C. The humid heat drove a death toll estimated in the thousands.
A separate heat dome also brought record June temperatures to parts of North America in late June.
On track to be second warmest, but a real chance at first
Carbon Brief’s updated projection for 2026 as a whole combines the observed January-June temperatures with the latest El Niño forecast. It uses a statistical model trained on the historical relationship between the first half of the year, ENSO conditions and annual temperatures observed over 1950-2025, excluding major volcanic eruption years.
Carbon Brief estimates that 2026 will be around 1.51C above pre-industrial levels, with a 90% range of 1.45C to 1.57C, shown by the yellow dot in the chart below.
This is up from 1.47C in the projection set out in April – and is notably more certain now that half the year has passed.
This central estimate would make 2026 the second-warmest year on record, just below 2024 (1.52C) and ahead of 2023 (1.43C) and 2025 (1.41C).
Carbon Brief’s modelling puts the chance that 2026 beats 2024 as the warmest year on record at 35%, using the average of the six different surface temperature records assessed. It puts the chance that 2026 comes in above 1.5C at around 63%.
If it does, 2026 would be the second calendar year – after 2024 – where warming averaged above 1.5C, in a further sign that the world is rapidly approaching the Paris Agreement’s 1.5C limit.
A single year above 1.5C does not by itself constitute a breach of the goal, which refers to the longer term average temperature of the planet. This is defined as the midpoint of a 20-year period by the Intergovernmental Panel on Climate Change (IPCC).
These likelihood of a record have been climbing rapidly throughout 2026.
Global temperatures so far throughout the year have run well below the record-setting levels of 2024 – around 0.13C cooler over the first six months.
On their own, temperatures observed so far in 2026 would make a new annual record unlikely.
However, rerunning the projection using only the data available at the end of each month since March – including both the year-to-date observations and the El Niño forecast issued that month – shows a shifting picture.
Using March data, 2026 had just a 7% chance of setting a new record. That rose to 16% in April, 24% in May, 27% in June and 35% using the latest data in mid-July.
This is shown in the chart below.
Notably, this rise has little to do with observed temperatures. The year-to-date anomaly has actually drifted slightly down, from 1.41C after March to 1.39C after June.
Observed temperatures and fewer remaining months of the year contributed only around four percentage points of the 28-point rise in the likelihood; the remaining ~84% of the change comes from successive upward revisions to the El Niño forecast for late 2026.
However, whether 2026 ends up becoming the warmest year on record may end up depending on which dataset is used.
Running the same projection gives odds of a 2026 record of around two-in-three for Berkeley Earth (66%) and NASA GISTEMP (65%), but only 35% for HadCRUT5, 24% for NOAA and just 13% and 9% for the ERA5 and JRA-3Q reanalyses, respectively.
This is shown below.
The divergence between projections mostly reflects how exceptional each dataset’s 2024 was.
The reanalysis approaches recorded a particularly warm 2024, leaving 2026 more ground to make up. GISTEMP and Berkeley, on the other hand, project 2026 modestly above their 2024 values.
A repeat of the situation in 2015 where different groups disagreed on record rankings is a real possibility. Headlines in January 2027 may hinge on choices of dataset.
2027 likely to be the warmest year in human history
The biggest climate story of the developing super El Niño may not be 2026 at all.
Global temperatures typically lag in the tropical Pacific by around three months. So, an El Niño event peaking in November and December 2026 will have its largest warming influence on 2027.
We saw this same pattern occur in 1997-98, 2015-16 and 2023-24 – where the year in which the El Niño developed was warm, but the following year was record-smashing.
Carbon Brief has extended its projection into 2027 by using the historical relationship between year-over-year temperature changes and ENSO conditions in the preceding autumn.
This yields a best estimate for 2027 of around 1.71C above pre-industrial levels, with a 90% range of 1.49C to 1.93C. This is shown by a yellow square on the chart below.
That would give 2027 a 92% chance of setting a new global temperature record and a 94% chance of exceeding 1.5C.
Taking 2026 and 2027 together, there is a 93% chance that at least one of the two years sets a new record.
The 2027 estimate is more uncertain than the 2026 one. As with 2026, there are uncertainties in the projection due to unknowns around exactly how strong the El Niño peak proves to be and how quickly it decays.
However, even the low end of the 2027 range would put it among the warmest years on record and the central estimate of 1.71C would exceed 2024 by nearly 0.2C.
If these projections bear out, the 2020s will have delivered new global temperature records in 2023, 2024 and 2027 – and potentially 2026 too – with a number of individual years well above the 1.5C threshold.
The long-term warming trend, driven by human emissions of carbon dioxide and other greenhouse gases, has increased from around 0.18C per decade in the early 2000s to around 0.27C per decade today. El Niño and La Niña play a big role in determining which years along that rising path stand out as records.
Arctic sea ice at record lows
Arctic sea ice has spent much of 2026 in record-low territory.
Following the joint-lowest winter maximum in the satellite record in mid-March, daily extent has set or tied record lows for the date on 39 days so far this year, including extended spells in mid-to-late March and in early-to-mid June.
The most recent record-low days were in early July.
The chart below shows how Arctic sea ice in 2026 (dark red line) has been below the historical range (shaded red).
It also shows how Antarctic sea ice (dark blue), meanwhile, has remained below the 1979-2010 range for almost all of 2026 to date.
As of mid-July, Arctic extent is a bit below the 1979-2010 historical range for the date, though it remains around 0.6m square kilometres (km2) larger than the record low for the date set during 2020’s exceptional summer melt season.
The trajectory over the coming two months will determine whether 2026 challenges 2012’s record September minimum. Early-summer conditions are a poor predictor of the September minimum, which depends heavily on summer weather.
Antarctic sea ice, meanwhile, is currently around 300,000km2 below the historical envelope, but has stayed well clear of the record lows set in 2023 and has not set any new daily records yet this year.
Q&A: Europe’s May and June heatwave deaths – and how they were counted
Guest post: France’s June heatwave caused more than 2,700 heat-related deaths
Guest post: Climate change has caused one-fifth of Pine Island glacier retreat
Media reaction: How climate change intensified Europe’s record-breaking June heat
The post State of the climate: Rapidly developing El Niño raises chance of record-warm 2026 appeared first on Carbon Brief.
State of the climate: Rapidly developing El Niño raises chance of record-warm 2026
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