This month marks 10 years since the UK recorded its first named storm.

Storm Abigail struck in November 2015, bringing high winds, lightning and snow and causing power cuts and school closures in northern Scotland.

In the decade that has passed, storm naming has become a key part of how the Met Office warns the public about impending storms.

Storm naming is a public safety tool that makes severe weather easier to remember, talk about and follow.

The success of the scheme offers lessons for how clear communication can help communities prepare, adapt and build resilience in a changing climate.

Here, we look back at a decade of naming storms in the UK and some of the most notable events.

Storms in the UK

Storms in the UK typically take place during the autumn and winter months and last for between two and three days.

The number of named storms varies from year to year. Some storm seasons – for example, 2023–24 – are exceptionally active, while others are much quieter.

The UK owes its stormy climate in large part due to the jet stream – fast-moving winds that blow from west to east high in the atmosphere and push low-pressure weather systems across the Atlantic.

These low-pressure systems can bring heavy rain and strong winds to the UK, which, in turn, causes storms.

Storms in the UK can cause serious damage, felling trees, destroying infrastructure and causing travel disruptions.

Some have resulted in widespread flooding – and others, tragically, in loss of life.

Over the last decade, the UK has seen a number of storms with extreme wind speeds and heavy rainfall.

The table below sets out a list of records set by storms between November 2015 and October 2025.

UK storm records for the period November 2015–October 2025. Source: Met Office

Storm naming

Storm naming was introduced in the UK and Ireland at the start of the 2015 storm season.

Launched by the Met Office and Ireland’s weather service, Met Éireann, Dutch weather service the Royal Netherlands Meteorological Institute (KNMI) joined the storm-naming scheme in 2019.

This collaboration between the UK, Ireland and Netherlands is one of three storm-naming groups in Europe. Each group releases a new alphabetical list of storm names in September.

The graphic below highlights the storm names picked by the Western European storm-naming group for 2025-26.

Not all storms are named. A storm will be named if the Met Office anticipates it having potential to cause disruption or damage.

This is often linked to whether strong winds are expected, but impacts caused by other weather types – for instance, heavy rain, hail or snow – are also considered.

Once named, the storm is referred to consistently by weather services and other authorities in Ireland, Netherlands and the UK.

Storm naming was introduced to improve communication of the weather forecast to the public and help people stay safe during severe weather.

Using a single, authoritative name for a storm allows government and media outlets to deliver a consistent message about approaching severe weather.

In this way, the public will be better placed to keep themselves, their homes and businesses safe.

There have typically been around half a dozen named storms each year since November 2015, although this varies on a year-to-year basis.

The 2023-24 storm season saw the most named storms to date. In August 2024, Storm Lillian became the 12th named storm of that season.

Below is a table of all the storms that have been named since 2015.

Storms named between November 2015 and October 2025. Source: Met Office.

Notable named storms

While every year since the scheme began has seen storms strong enough to be named, some storms have been particularly significant.

Storm Desmond, December 2015

Storm Desmond brought extreme rainfall to north-west England. The weather station in Honister Pass in Cumbria recorded 34.1cm of rainfall in just 24 hours in a new UK record. Another record was set when 405mm of rain fell at Thirlmere in Cumbria over two consecutive days.

The subsequent floods affected thousands of homes and businesses across Cumbria and other parts of northern England, sweeping away several bridges and cutting road and rail links.

Storm Desmond led to the government launching the National Flood Resilience Review.

Storm Arwen, November 2021

Storm Arwen is an example of how the damages caused by a storm depends on more than its overall strength. A storm’s location, duration and wind direction also plays a role.

This storm occurred after an area of pressure in the North Sea drove very strong northerly winds across north-eastern parts of the UK. Winds gusted at up to 98mph at Brizlee Wood in Northumberland.

The unusual wind direction of Storm Arwen resulted in the felling of thousands of trees and left more than a million homes without power. Parts of the Pennines also saw significant disruption from lying snow.

Storms, like Arwen, that have a wind direction different to the prevailing south-westerly direction are less frequent, but are nevertheless a key part of the UK’s climate.

Storm Eunice, February 2022

In February 2022, three named storms affected the UK within the space of a week. The second of these storms was Storm Eunice.

Storms in close succession can cause particular problems because clean-up efforts can be hampered by further severe weather.

Storm Eunice was the most severe and damaging storm to affect England and Wales since February 2014. Gusts reached 122mph at Needles on the Isle of Wight – the highest on record for England at a low-level station.

The storm caused deaths, widespread damage to buildings and major travel disruption, including the temporary closure of the Port of Dover.

Storm Babet, October 2023

Storm Babet was notable for prolonged and intense rainfall which led to severe flooding, evacuations and sadly, deaths. In eastern Scotland, particularly in the county of Angus, rainfall totals reached 150-200mm, with some areas experiencing their wettest day on record since 1891.

A key factor with this storm was its unusual track, or path. The storm moved south to north, picking up additional moisture as it crossed the Bay of Biscay. A high-pressure “blocking” weather system over Scandinavia prevented Babet clearing the UK eastwards into the North Sea. As a result, high wind speeds were sustained across north-east England and much of Scotland for a prolonged period.

Storm Éowyn, January 2025

Storm Éowyn was the UK’s most powerful windstorm in more than decade, with the brunt of impacts felt in Northern Ireland and Scotland’s populous Central Belt.

Gusts exceeded 90mph in Northern Ireland – where this was the most severe wind storm since 1998 – while a 100mph gust was recorded at Drumalbin in Lanarkshire.

Roads were closed, flights, ferries and trains were cancelled and more than a million homes were reported to be without power at the peak of the storm. Scotland’s national botanical collection at the Royal Botanic Garden in Edinburgh saw several dozen felled or badly damaged trees.

Storm Éowyn’s intensity and geographic reach made it a standout event in recent years.

The timeline below shows how the Met Office worked with Met Éireann and KNMI to alert the public about Storm Éowyn.

Climate change and storms

There is no evidence of positive or negative trends in windstorm number or intensity in the UK’s recent climate.

Trends in windstorm frequency are difficult to detect, because numbers vary year-to-year and decade-to-decade.

Most climate projections indicate that winter windstorms will increase slightly in number and intensity over the UK, including disproportionately more severe storms. However, scientists have “medium confidence” in these projections – because a few climate models indicate differently.

This uncertainty highlights the need for ongoing research into how climate change may influence the severity and frequency of windstorms in northern Europe.

On the other hand, scientists are confident that climate change is making rainfall during storms more intense.

A 2024 attribution study involving Met Office scientists showed that climate change has made rainfall during storms more intense through autumn and winter in the UK. The researchers noted that this trend is set to increase as the planet warms.

Recent increases in flooding in the UK have also been linked to climate change.

Other research, meanwhile, has found that sea level rise caused by climate change will worsen storm surges and high waves during windstorms.

The continuing unpredictability of UK storms – combined with projections of increased rainfall and heightened coastal damage under climate change – means that being prepared for, and adapting to, the future weather is crucial.

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The post Met Office: Ten years of naming UK storms to warn the public appeared first on Carbon Brief.

Met Office: Ten years of naming UK storms to warn the public

Reflections on Community at CCL’s 4th Annual Inclusion Conference

By Phalika Oum, CCL Inclusion Fellow

Maybe it was Karina’s plumeria hair clip, paying homage to the land and the native peoples of Hawaii; she humbles us with a reminder that we are merely guests here. Perhaps it was Wanda’s Elsa doll or Karis’ worn-out, well-loved book. Or perhaps it was Mike’s gentle tone, swiftly dancing to the music of multiplicity: We contain multitudes and our identities cannot be distilled into words. Words that we too often take for granted.  

What’s it like to choose stillness in times of great civil unrest and mounting ecological turmoil? What’s it like to choose to love in the face of disjuncture? How do we keep moving forward, despite it all?

____

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From Friday, Sept. 26, to Saturday, Sept. 27, Citizen Climate Lobby’s People of the Global Majority and members of the Inclusion team hosted their 4th annual virtual Inclusion Conference, “Rooted in Care, Growing in Community,” dedicated to sharing stories from CCL’s Affinity Action Teams and practical tools for managing anxiety at the intersections of climate and inclusion. With 77 community members attending the Friday reception and 181 members attending the Saturday conference, this year’s event demonstrates the power of convening as a community.

The event kicked off with a show and tell reception, where community members shared stories about an object of their choosing. This created room for cultural, familial, and personal reflections and storytelling, setting the stage for a weekend of intention and belonging. In this space, we saw the coming together of difference, with attendees ranging in age, race, profession, gender orientation, and more.

The Saturday conference was supported by Spanish interpretation from Gabriela and ASL interpretation from Jessy and Joe. Kendyl, a leader from our Persons with Disability affinity group, encouraged the usage of visual descriptions—an accessibility tool used by the speaker to identify themselves in a presentation. Karina also shared a playlist to celebrate the songs of difference, submitted by the People of the Global Majority (PGM) Caucus. 

Jacob Shores-Argüello, Costa Rican-American environmental humanist, writer, and author of Paraíso and In Absence of Clocks, started the day off by reading poetry from his new book “Grief for the green that was.” Jacob challenged concepts of geographical boundaries and reminisced about his late mother, exploring how grieving for his mother translated to grieving for his motherland. The “grief for the green that was,” as he so eloquently stated it, is a deep longing to come home. Hear Jacob read his poetry here:

Then Julian Cauzae, a seminary student at Harvard Divinity School interested in conversations around climate change and the apocalypse, created space for attendees to share their experiences conversing about the climate question. From conversations about inductive gas stoves and the restoration of democracy to the question of human extinction, Julian patiently listened and responded by weaving in themes of time and agency. 

Mayor Ukeme Awakessian Jeter

Mayor Ukeme Awakessien Jeter of Upper Arlington, Ohio, joined the conversation to share her understanding of cultural competency. While recognizing the importance of data in storytelling and advocacy, Jeter encouraged us to use a different and more qualitative method for gathering information: going directly to the people most impacted by the crisis. She walked us through how to effectively integrate cultural competency into our walk as the “connector” of community, pointing to three key steps: access your own cultural awareness, invest in your own cultural development, and foster a culture of curiosity. Ukeme challenged us to have the integrity to say, “I have some work to do here, and I am going to do the work to get there.”

The next hour of the conference included breakout sessions on various topics, led by CCL community members and members of the People of the Global Majority Caucus. The sessions included:

• “Faith, Stewardship, and the Climate Crisis: How Religion Shapes Environmental Action,” led by Mike Roman, a member of CCL’s Peace Corps Action Team
• “Our Water and Climate Change,” led by Manolo Matos, CCL’s Kentucky State Coordinator
• “Resistance is Edible: The Poetics of Food and the Teachings of Ancestors,” led by Phalika Oum, a 2025 Inclusion Fellow
• “Putting Partisan in the Past: Changing our perspectives during engagements from ‘you and I’ to ‘we’ to truly embrace our value of nonpartisanship,” led by Drew Eyerly, CCL’s Action Teams Director
• “Building Community Resilience with Educational Gardens,” led by Lucy Xue, a member of CCL’s Asian Pacific Action Team
• “At the Intersection: Gender, Justice, and the Climate Crisis,” led by Allison Fabrizio, a member of CCL’s People of the Global Majority Action Team

After, we rejoined the main conference room to hear from Clara Fang, Founder of Green Tara Consulting. Clara shared strategies for preventing burnout and productivity, as well as the value of dismantling oppression and colonial regimes through self-care, a radical form of resisting the culture of white supremacy, patriarchy, and capitalism. Clara recognized the work of CCL’s Personal Resilience Action Team, which seeks to strengthen group and personal resilience through trainings and workshops. She also encouraged attendees to join her Activism Hour, held every Tuesday at 6 p.m. ET, as a coworking meeting for activists. 

Pamela Benson Owens

Vanessa Nakate sent along a video message for conference attendees, urging us to join people in the frontlines of the climate crisis with a spirit of one-ness, community, and care. Vanessa spoke about a world without oppression where nature is recognized and treated as the source of life.

Our final speaker, Pamela Benson Owens of Edge of Your Seat Consulting, Inc., shared a powerful message about the importance of integrating inclusion into every organizational standard. Using her experience training other organizations, including like-minded groups and disagreeing parties, she urged us to create space for relationship-building and communication by seeing each other as humans first, anchored in the common experience. Pamela held the truth that to build on inclusion, we need to have respectful communication, which includes active listening, inclusive language, and curiosity without judgement. 

_____

It’s times like this I feel the most connected with the world, with humanity, and with my body. Historians, anthropologists, and all other scientists alike say there was a time before written language, following the language of gestures. It was in these times that our ancestors passed down knowledge and wisdom through the practice of oral storytelling and share outs. How incredible it is to return to our roots and dance with words together in the blight of monoculture and during the age of erosion! 

Conferences, such as this one, leaves us feeling empowered and ready to act. But what comes next? What do you do the day after? The month? The year? 

Many attendees shared that their motivation for engaging in climate work are their children, grandchildren, neighbors, friends, and even strangers—this is the heart of inclusion in climate work, for we cannot sufficiently address climate justice without addressing the ones currently most impacted and will be most impacted by what’s to come if we do not act. 

Phalika Oum, CCL 2025 Inclusion Fellow

Over the years, I’ve placed my hope in places and rhythms that leave me feeling more helpless. For reasons I’m still piecing together, this multicultural and intergenerational space that the CCL Inclusion team has cultivated left me with security. I am one of the lucky ones to stand alongside veterans, retirees, high school students, college students, academics, climate professionals, and more to discuss the very pressing issues in our climate and celebrate the beauties of inclusion. 

For all the attendees who chose to use their weekend to attend CCL’s 4th Inclusion Conference, thank you. Thank you for your presence and solidarity. Thank you for sharing your thoughts and experiences. And thank you for being open-minded and choosing to listen to difficult conversations. I feel forever grateful.

As for me, I sit with wonder. My chest fills with gravity and eagerness. And somehow, the air feels lighter knowing that I have a whole community to reflect alongside. I continue to meditate on the praxis of holding space for people and communities. I’m walking a tightrope held together by tensions and truths. This, I know, will be a lifetime of reflection and endurance.

Phalika Oum has served as CCL’s Inclusion Fellow since January 2025.

The post Reflections on Community at CCL’s 4th Annual Inclusion Conference appeared first on Citizens' Climate Lobby.

Reflections on Community at CCL’s 4th Annual Inclusion Conference

Carbon dioxide (CO2) emissions from fossil fuels and cement will rise around 1.1% in 2025, reaching a record 38.1bn tonnes of CO2 (GtCO2), according to the latest figures from the Global Carbon Project. 

However, falling land-use emissions means that global CO2 emissions in 2025 will remain relatively unchanged compared to 2024 levels.

The 20th edition of the annual Global Carbon Budget report, published today, also finds that the land carbon sink – the portion of human-caused CO2 emissions absorbed by plants and soils – appears to have recovered to its pre-El Niño strength after two unusually weak years. 

However, research published alongside the report by the same team also suggests that climate change has caused a long-term decline in land and ocean carbon sinks, with sinks being about 15% weaker over the past decade than they would have been without climate impacts.

The study, published in Nature, finds that the decline of carbon sinks has contributed about 8% to the rise in atmospheric CO2 concentration since 1960.

The 2025 Global Carbon Budget report also estimates that:

• Emissions in China and India are projected to grow much less in 2025 compared to the past decade, while emissions in the US and EU are projected to grow this year after years of decline.
• Global CO2 emissions from land-use change are expected to decrease by nearly 10% in 2025, driven by reductions in deforestation and forest degradation in South America. 
• Total CO2 emissions – fossil and land use – have grown more slowly over the past decade (0.3% per year on average) compared to the previous decade (1.9% per year). 
• The remaining carbon budget to limit global warming to 1.5C is virtually exhausted and is equivalent to only four years of current emissions. Carbon budgets to limit warming to 1.7C and 2C would similarly be used up in 12 and 25 years, respectively.
• The concentration of CO2 in the atmosphere is set to reach 425.7 parts per million (ppm) in 2025, 2.3ppm above 2023 and 52% above pre-industrial levels.

(For detailed coverage of previous editions of the report, see Carbon Brief’s coverage for 2024, 2023 and 2022.)

Global emissions remain flat

The Global Carbon Budget (GCB) finds that total global CO2 emissions in 2025 – including those from fossil fuels and land use – are projected to remain approximately flat at 42.2GtCO2, falling by a negligible -0.04% compared to last year. 

This means 2025 is effectively tied with 2024 as the highest global CO2 emissions on record.

Flat total CO2 emissions in 2025 reflect a combination of continued rising emissions from fossil fuel and industry and declining emissions from land-use change. Fossil CO2 emissions rose 1.1% to 38.1GtCO2, while land-use emissions declined by -9.8% to 4.1GtCO2 (albeit with large uncertainties).

The figure below shows the 2025 global CO2 emissions update (red solid line) alongside 2024 (dark blue dotted), 2023 (mid blue dotted) 2022 (light blue dotted), 2021 (light grey dotted) and 2020 (dark grey dotted). The shaded area indicates the uncertainty around the new 2025 budget. 

(Each year, the GCB is updated to include the latest data as well as improvements to modelling sources and sinks, resulting in some year-to-year revisions to the historical record.)

The 2025 figures are notably higher than those in the prior five GCB reports, reflecting an upward revision in historical land-use emissions. (This is discussed in more detail in the land-use emissions section below.)

Total global CO2 emissions have notably flattened in the past decade (2014-25), growing at only 0.3% per year compared to the 1.9% rate of growth during the prior decade (2004-13) and the longer-term average growth rate of 1.6% over 1959-2014.

This apparent flattening is due to declining land-use emissions compensating for continued – but slow – increases in fossil CO2 emissions. Fossil emissions grew around 0.2GtCO2 per year over the past decade, while land-use emissions decreased by a comparable amount.

However, despite the emissions plateau, there is still no sign of the rapid and deep decrease in CO2 emissions needed to reach net-zero and stabilise global temperatures in-line with the Paris Agreement temperature goal.

If global emissions remain at current levels, the remaining carbon budget to limit warming to 1.5C (with a 50% chance) will be rapidly exhausted.

(The carbon budget is the total amount of CO2 that scientists estimate can be emitted if warming is to be kept below a particular temperature threshold. Earlier this year, the Indicators of Global Climate Change report estimated the remaining carbon budget had declined by three-quarters between the start of 2020 and the start of 2025.)

With human-caused global warming sitting at around 1.36C above pre-industrial levels in 2024, the remaining budget for 1.5C is 170GtCO2, equivalent to four years of current emissions. 

The GCB report finds that the remaining carbon budgets to limit warming to 1.7C and 2C have been reduced to 525GtCO2 (12 years at current emissions levels) and 1,055GtCO2 (25 years), respectively.

Global fossil CO2 emissions also grew more slowly in the past decade (0.8% per year) compared to the previous decade (2.1%). This was driven by the continued decarbonisation of energy systems – including a shift from burning coal to gas and replacing fossil fuels with renewables – as well as slightly weaker global economic growth during the past decade.

The figure below breaks down global emissions (dark blue line) in the 2025 budget into fossil (mid blue) and land-use (light blue) components. Fossil CO2 emissions represent the bulk of total global emissions in recent years, accounting for approximately 90% of emissions in 2025 (compared to 10% for land use). This represents a large change from the first half of the 20th century, when land-use emissions were approximately the same as fossil emissions.

Global fossil emissions include CO2 emitted from burning coal, oil and gas, as well as the production of cement. However, to determine total fossil emissions, the Global Carbon Budget also subtracts the cement carbonation sink – CO2 slowly absorbed by cement once it is exposed to the air – from fossil emissions.

Global emissions can also be expressed on a per-capita basis, as shown in the figure below.

While it is ultimately total global emissions that matter for the Earth’s climate – and a global per-capita figure glosses over a lot of variation among, and within, countries – it is noteworthy that global per-capita fossil emissions peaked in 2012 and have been slightly declining in the years since.

Land-use emissions continue downward trend

Global land-use emissions stem from deforestation, forest degradation, loss of peatlands and harvesting trees for wood. They averaged around 5.0GtCO2 over the past decade (2015-24) and the Global Carbon Budget provides an initial projection for 2025 of 4.1GtCO2.

This represents a 0.5GtCO2 decrease in land-use emissions relative to 2024. The GCB report suggests that this was largely driven by a combination of reductions in deforestation and forest degradation in South America and by the end of the dry 2023-24 El Niño conditions.

Overall, land-use emissions have decreased by around 32% compared to their average in the 2000s, with a particularly large drop in the past decade. This decline is statistically significant and is due both to decreasing deforestation and increasing levels of reforestation and afforestation globally.

Three countries – Brazil, Indonesia and the Democratic Republic of the Congo (DRC) – collectively contribute approximately 57% of the global land-use emissions. In the past, China has been a meaningful contributor to land-use emissions, but in recent years its land-use emissions have turned net-negative as more trees have been planted than cut down.

The figure below shows changes in emissions over time in these countries, as well as land-use emissions in the rest of the world (grey).

Historical land-use emissions have been revised upward in the 2025 GCB report compared to prior estimates. This reflects a combination of two factors:

• The discontinuation of one of the four bookkeeping models that GCB has historically relied on for land-use emissions estimates. This model tended to show lower land-use emissions than the others.
• The inclusion of the impacts from CO2 fertilisation on global biomass densities. Because forests have higher biomass densities now than in the past, due to increasing CO2, this tends to increase the estimate of land-use emissions for recent years.

Fossil-fuel CO2 hits record highs

Global emissions of fossil CO2 – including coal, oil, gas and cement – increased by around 1.1% in 2025, relative to 2024, with an uncertainty range of 0.2-2.2%. This represents a new record high and surpasses the prior record set in 2024.

The figure below shows global CO2 emissions from fossil fuels, divided into emissions from major emitting countries including China (dark blue shading), the US (mid blue), the EU (light blue), India (light blue) and the remainder of the world (grey).

China represents 32% of global CO2 emissions today. Its 2025 emissions are projected to increase by a relatively small 0.4% (with an uncertainty range of -0.9% to 2%), driven by a small rise in emissions from coal (0.3%), a modest rise in gas (1.3%) and a larger rise in oil (2.1%).

Given the uncertainty range, a decrease in Chinese emissions is also a possibility, but this will not be confirmed until the full 2025 data is available.

Similarly, recent analysis for Carbon Brief found that China’s emissions were “finely balanced between a small fall or rise” in 2025. However, it said that a drop in the full-year total became more likely after a 3% decline in September. (The Global Carbon Project estimates are based on data covering January through to August, which point towards a small rise in 2025.)

Whether China’s emissions see small rise or fall in 2025, the outcome will be due to moderate growth in energy consumption combined with an extraordinary growth in renewable power generation. This would represent the second year in a row where Chinese emissions growth was well below the average rate over the past decade.

The US represents 13% of global emissions and emissions in 2025 are projected to increase by 1.9% (-0.2 to +4.1%) compared with 2024. This marks a reversal from recent trends in declining CO2 emissions. 

The projected growth of emissions in the US is likely driven by a combination of three factors: a colder start to the year after a mild 2024, which led to greater heating requirements, higher gas prices, which led to more coal being used in power generation, as well as an increase in total demand for electricity.

US emissions from coal are expected to increase by a substantial 7.5% in 2025, emissions from both oil and gas by a more modest 1.1% and emissions from cement to fall by -8.0%.

While policies enacted by the current US administration may increase CO2 emissions going forward, their impact on national emissions levels in 2025 were likely relatively modest compared to other factors.

India represents 8% of global emissions. In 2025, its emissions are projected to increase by 1.4% (-0.3% to +3.1%) on 2024 levels, significantly below recent trends.

An early monsoon with the highest-ever May rainfall substantially reduced cooling requirements in May and June, the hottest months of the year. Strong growth or renewables – particularly solar – has also helped limit the growth of Indian emissions. 

Indian emissions from coal are expected to grow 1.7%, with oil growing 0.1%, gas shrinking by -6.4% and cement growing by 9.9%.

The EU represents 6% of global emissions. Its emissions are projected to increase by 0.4% in 2025, with an uncertainty range of -2.1 to +2.8%. This represents a divergence from a past decline in emissions (albeit with large uncertainties).

EU emissions from coal are expected to decline by -0.3%, whereas emissions from oil and gas are projected to increase by 0.6% and 0.9%, respectively. Cement emissions are expected to fall by -4.1%.

The increase in EU emissions is in part from weather-related low hydropower and wind generation which – despite increases in solar – have led to an increase in electricity generation from gas. In addition, a relatively cold February led to increased use of natural gas for space heating.

International aviation and shipping (included in the “rest of world” in the chart above) are responsible for 3% of global emissions. They are projected to increase by 6.8% for aviation, but remain flat for international shipping. This year will be the first time that aviation emissions have exceeded pre-Covid levels.

The rest of the world (excluding aviation) represents 38% of global emissions. Emissions are expected to grow by 1.1% in 2025 (ranging from -1.1% to +3.3%), with increases in emissions from coal (1%), oil (0.5%), gas (1.8%) and cement (2.4%).

The total emissions for each year over 2022-25, as well as the countries and regions that were responsible for the changes in absolute emissions, are shown in the figure below.

Annual emissions for 2022, 2023, 2024 and estimates for 2025 are shown by the black bars. The smaller bars show the change in emissions between each set of years, broken down by country or region – the US (dark blue), EU (mid blue), China (light blue), India (pale blue) and the rest of the world (grey). Negative values show reductions in emissions, while positive values reflect emission increases.

The US represented a large part of the rise in global fossil-fuel emissions in 2025. US emissions increases over 2024-25 contributed about 40% of the total global increase – more than the EU, China and India contributions combined.

The Global Carbon Project notes that emissions have declined over the past decade (2015-24) in 35 nations, which collectively account for 27% of global emissions. This is up from 18 countries during the prior decade (2005-14).

The decrease in emissions in those countries comes despite continued domestic economic growth and represents a long-term “decoupling” of CO2 emissions and the economy.

The carbon intensity of energy has consistently decreased over the past decade in China, the US, the EU – and, to a lesser extent, globally.

However, peaking CO2 emissions requires that the rate of decarbonisation exceeds the growth in energy demand. This has happened in some regions, including the US and EU, but not yet globally.

Modest growth in emissions from coal, oil, gas and cement

Global fossil-fuel emissions primarily result from the combustion of coal, oil and gas.

In 2025, coal is responsible for more emissions than any other fossil fuel, representing approximately 42% of global fossil-fuel CO2 emissions. Oil is the second largest contributor at 33% of fossil CO2, while gas comes in at 21%.

The production of cement is responsible for around 3.8% of global emissions, but this is reduced to 1.9% once the carbonation sink – the drawdown of atmospheric CO2 by concrete – is taken into account.

These percentages reflect both the amount of each fossil fuel consumed globally, but also differences in CO2 intensities. Coal results in the most CO2 emitted per unit of heat or energy produced, followed by oil and gas.

The figure below shows global CO2 emissions from different fuels over time, covering coal (dark blue), oil (mid blue) and gas (light blue), as well as cement production (pale blue) and other sources (grey).

While coal emissions increased rapidly in the mid-2000s, they have largely flattened since 2013. However, coal use increased significantly in 2021 and then more modestly in the subsequent four years.

Global emissions from coal increased by 0.8% in 2025 compared to 2024, while oil emissions increased 1.0% and gas emissions increased by 1.3%.

Despite setting a new record this year, global coal use is only 6% above 2013 levels – a full 13 years ago. By contrast, during the 2000s, global coal use grew at a rate of around 4% every single year.

The figure below shows the total emissions for each year over 2022-25 (black bars), as well as the absolute change in emissions for each fuel between years.

Global oil emissions were suppressed for a few years after the 2020, but rebounded to pre-pandemic levels as of 2024 and have continued to grow in 2025.

This reflects that, despite falling sales of internal combustion engine vehicles, not enough electric vehicles (EVs) have yet been sold to result in peak oil demand.

The global carbon budget

Every year, the Global Carbon Project provides an estimate of the overall “global carbon budget”. This is based on estimates of the release of CO2 through human activity and its uptake by the oceans and land, with the remainder adding to atmospheric concentrations of the gas.

(This differs from the commonly used term “remaining carbon budget”, which refers to the amount of CO2 that can be released while keeping warming below global limits of 1.5 or 2C.)

The most recent budget, including estimated values for 2025, is shown in the figure below.

Values above zero represent sources of CO2 – from fossil fuels and industry (dark blue shading) and land use (mid blue) – while values below zero represent carbon sinks that remove CO2 from the atmosphere. Any CO2 emissions that are not absorbed by the oceans (light grey) or land vegetation (mid grey) accumulate in the atmosphere (dark grey). In addition, a dashed black line is shown to represent the expected sum of sinks based on estimated emissions.

Over the past decade (2015-24), the world’s oceans have taken up approximately 29% of total human-caused emissions, or around 11.8GtCO2 per year.

The ocean CO2 sink has been relatively flat since 2014 after growing rapidly over the prior decades, reflecting the flattening of global emissions during that period.

This estimate for carbon sinks has been revised up from 26% in prior versions of the GCB, reflecting a major update to carbon budgets driven by new data and modelling of carbon sink behavior.

The land sink takes up around 21% of global emissions, or 8.7GtCO2 per year on average over the past decade – discussed in more detail in the section below. This is down from 29% in prior budgets.

The atmosphere continues to accumulate the bulk of human-caused CO2 emissions, with about 49% going into the atmosphere on average over the past decade – a rate of 20.4GtCO2 per year.

The growth rate of atmospheric CO2 in 2025 is expected to be around 2.3ppm, which is a bit below the decadal average rate of 2.6ppm over the past decade (2015-24). This is well below the record-setting rise of 3.7ppm in 2024, which was primarily driven by the effect of the 2023-24 El Niño conditions weakening the land sink.

Atmospheric CO2 concentrations are set to reach an annual average of 425.7ppm in 2025, representing an increase of 52% above pre-industrial levels of 280ppm.

There remains an unusual imbalance in the carbon budget in 2024, where the sum of the sinks is notably larger than estimated emissions. This can be seen in the figure above, where the dashed line is below the shaded area.

Budget imbalances are not unprecedented – there are large uncertainties in both emissions data and sink estimates. But the rise in the amount of CO2 accumulating in the atmosphere in 2024 is larger than would be expected based on emissions.

There are a number of potential explanations for this 2024 imbalance. The land cover data for 2024 is not yet complete and it is possible that some fire emissions data might be missing from the record. This might result in either higher land-use emissions or lower land sinks than currently estimated.

Alternatively, it could be due to the CO2 growth rate – captured by surface stations managed by the US National Atmospheric and Oceanic Administration (NOAA) – being slightly high. CO2 records for 2024 from these stations are higher than those obtained from satellite-based sensors, though it remains unclear which provides the most accurate measurement.

A declining, but not collapsing, land sink

After an usually weak land carbon sink in 2023, there were a number of media articles about its potential collapse.

For example, in October 2024, the Guardian wrote that “the sudden collapse of carbon sinks was not factored into climate models – and could rapidly accelerate global heating”. 

The truth is a bit more complicated. While the impending collapse of the land carbon sink has been greatly exaggerated, there is growing evidence of a long-term weakening of both the land and ocean carbon sinks due to human activity. 

And while the land sink has recovered to its pre-El Niño strength in 2025, aided by relatively low global fire CO2 emissions, it will continue to gradually weaken as global temperatures rise. This is not unexpected – scientists have long foreseen a weaker carbon sink in a warmer world.

A weaker land sink will contribute to higher global temperatures in the future as more CO2 emissions from burning fossil fuels and land use change will accumulate in the atmosphere.

The figure below shows the percentage of human emissions absorbed by the land sink in every year since 1959, with a recovery upwards in 2025 after two relatively low years.

In a study published in Nature alongside the release of the 2025 Global Carbon Budget, the same team of researchers provide a detailed estimate of exactly how the land and ocean sinks have changed as a result of human activity.

The research finds that the land and ocean sinks are 25% smaller and 7% smaller, respectively, than they would have been without the effects of climate change over 2015-24.

This amounts to a nearly 20% reduction in the efficacy of current global carbon sinks – that is, both the land and ocean – and a 15% reduction compared to how large they would be without the effects of climate change.

The figure below, from the new paper, shows the impact of climate change on the ocean sink (blue), the land sink (green) and atmospheric CO2 concentrations (grey) since 1960.

The weakening of carbon sinks due to human activity has led to an increase of atmospheric CO2 of more than 8ppm since 1960. The combined effects of climate change and deforestation have turned tropical forests in south-east Asia and in large parts of South America from CO2 sinks to sources.

And these sinks will likely continue to weaken as long as atmospheric CO2 concentrations continue to rise and the world continues to warm. There are a wide range of estimates of carbon cycle feedbacks among climate models, but a large carbon cycle feedback could result in a few tenths of a degree of future warming.

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The post Analysis: Fossil-fuel CO2 emissions to set new record in 2025, as land sink ‘recovers’ appeared first on Carbon Brief.

Analysis: Fossil-fuel CO2 emissions to set new record in 2025, as land sink ‘recovers’