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China’s Third Plenum, an important five-yearly meeting traditionally associated with major economic reforms, concluded on 18 July in Beijing.

Observers have been eagerly anticipating signals from the meeting about the leadership’s plans for economic growth and wider development, including on climate action.

The official readout from the meeting of the Central Committee of the Chinese Communist Party calls on policymakers to pursue a range of relevant reforms.

These include a focus on “high-quality economic development” (高质量发展), as well as “supporting all-around innovation” (支持全面创新) and “deepening reform in ecological conservation systems” (深化生态文明体制改革), among other areas.

It also urges officials to “make concerted efforts to cut carbon emissions” and “actively respond to climate change”. This is the first time carbon emissions have been mentioned in a plenum document. 

A key step to achieve this, it adds, is through “improving institutional mechanisms for developing new quality productive forces” (NQPF, 新质生产力).

Since its first appearance in official rhetoric in September last year, this term has featured in Chinese state media in numerous high-level policy documents and commentaries about industrial development and low-carbon growth.

According to Chinese president Xi Jinping, one important element of NQPF is “green development”, which he has described as the “base colour of high-quality development”. In comments made in January 2024, he added that “new quality productivity itself is green productivity” (新质生产力本身就是绿色生产力).

This encapsulates both the development of low-carbon technologies, such as electric vehicles (EVs), and the “green transformation” of the economy.

However, there is significant debate as to whether the concept, which can also be translated as “new productive forces” or “new quality productivity”, will result in concrete policy outcomes and support further development of industries critical to China’s energy transition.

In this article, Carbon Brief unpacks the concepts underpinning new quality productive forces, and what it means for China’s climate, energy and industrial policy.

What does ‘new quality productive forces’ mean?

The phrase was first mentioned by Xi during a visit to Heilongjiang province, located in the “rust belt” of northeast China, in 2023. 

In January 2024, he further defined it as innovation-led development that creates “a break with traditional economic growth models and development pathways”, resulting in a “high level of technology, efficiency and quality” (高科技、高效能、高质量) as well as an “in-depth transformation and upgrading of industry” (产业深度转型升级).

This has led to a “ubiquitous” focus on innovation across official discussions about NQPF, according to the University of Cambridge-affiliated thinktank Cambridge Industrial Innovation Policy.

Unleashing this innovation, according to official interpretations, will lead to a cascade of changes across China’s industrial system – “both technological and institutional” – that will improve China’s advanced manufacturing capabilities.

Nevertheless, innovation and advanced technology are not the only focus. Analysis by the Council on Geostrategy says the framing of NQPF “suggests that, while scientific and technological innovation is essential, [China recognises there] needs also to be deeper reforms of the…economic model”.

Chinese president Xi Jinping inspects a forest farm in Mohe in the Dahinggan Mountains, northeast China's Heilongjiang Province on 6 September 2023.
Chinese president Xi Jinping inspects a forest farm in Mohe in the Dahinggan Mountains, northeast China’s Heilongjiang Province on 6 September 2023. Credit: Yin Bogu / Alamy Stock Photo

Priority areas for reform include the market-based economy; state owned enterprises (SOE); and China’s fiscal, household registration and healthcare systems.

These economic reforms, driven both by “the government’s ‘visible hand’ and the market’s ‘invisible hand’”, are necessary for China’s continuous prosperity, according to the Xinhua Institute, a thinktank affiliated with state news agency Xinhua.

The institute links NQPF with Marxism, arguing this is in line with improving “means of production” – an important force in Marxist theory for production, reform and human development. 

Most official explanations of the concept are relatively broad and unspecific. However, low-carbon development is one of the few named priorities. 

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How significant is this for low-carbon development? 

NQPF will provide an “important support for green development”, according to a commentary in the Communist party-affiliated People’s Daily, which was reposted on the website of China’s National Energy Administration

“Protecting the ecological environment is to protect productivity and improving the ecological environment is to develop productivity,” it adds.

Some analysis takes this further. Prof Zhang Yunfei, from the Marxism studies department at Renmin University in Beijing and researcher at its National Institute of Development and Strategy, tells the government-affiliated newspaper China Environment News that NQPF represents a development model specific to China.

This contrasts with “traditional productive forces in Western societies”, or “black productivity” (黑色生产力), which saw “high consumption of resources and energy, and high pollution of the ecological environment”, he says.

Instead, NQPF signifies “green productivity”, which will help China “shift from conforming to leading globalisation, and promote the country’s healthy and green development”.

“Green productivity”, Zhang adds, is sustainable productivity that focuses both on increasingly productive “ecologicalisation” (生态化) and increasingly ecological productive forces driving wider development. 

These forces are fundamentally provided by and rooted in nature, he explains. Driving forces include “sustainable resources such as information”, a “new generation of workers” that understand the concept of ecological civilisation and an enhanced “level of sustainable development” based on “green science and technology”.

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Why is the concept important?

This concept of NQPF is a holistic approach “designed to address complex, interrelated challenges faced by China and to create a more resilient and dynamic economy that will bring long-term prosperity”, Dr Muyi Yang, senior electricity policy analyst for China from the thinktank Ember, tells Carbon Brief. 

Arthur Kroeber, founding partner and head of research at research firm Gavekal Dragonomics, tells Carbon Brief that NQPF is “the latest iteration of a long-running trend towards industrial policy, technology and intensive growth”.

This is “essentially a new bottle for old wine”, Kroeber adds. “I think what it does do is emphasise the point that there is a national mission” to build China into a technological superpower.

“It is a big deal”, Bill Bishop, author of the Sinocism newsletter, told Bloomberg, as Xi “putting a stamp” on the idea will “send a powerful signal” to stakeholders across the system.

The idea addresses specific anxieties facing China’s leadership. As well as supporting economic growth, some argue that strengthening the country’s ability to innovate provides China with a greater sense of security. 

Workers inspect battery products at a lithium battery factory in Tangshan, China.
Workers inspect battery products at a lithium battery factory in Tangshan, China. Credit: Yang Shiyao / Alamy Stock Photo

According to the Chinese Communist party’s leading theoretical journal Qiushi, for example, Xi believes that China is “still reliant on others for some core technologies…our industry is still not strong enough in spite of its size and falls short of excellence…and we face significant pressure in making the transition to green and low-carbon production modes”. 

Prof Yao Yang, liberal arts chair professor at the China Center for Economic Research and the National School of Development at Peking University in Beijing, echoes this, writing in a comment for China Daily that the “significance” of the concept is the overarching aim of “laying a solid foundation for the future of the Chinese economy”.

Kroeber tells Carbon Brief that this is also driven, in part, by historical parallels between China’s fear of being cut off from US technological advancements and the rupture with the Soviet Union in the Mao era. He says:

“After the Sino-Soviet split, Soviet advisors who went [to China] to help build steel plants and develop the petrochemical industry, for example, all left. China was left [to develop its economy] on its own…Xi Jinping has drawn a specific connection [to that].”

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What does this mean for China’s low-carbon technology industries?

A primary aim of NQPF is to expand “strategic emerging industries” and “nurture future industries”, Deng Zhou, associate research fellow at the Institute of Industrial Economics of the Chinese Academy of Social Sciences, writes in the state-run newspaper China Daily

“Strategic industries” include “new energy”, “new energy vehicles” and “energy conservation and environmental protection”. Recent analysis for Carbon Brief found that “clean energy” sectors contributed 11.4tn yuan ($1.6tn) to China’s economy in 2023.

“Future industries”, according to a policy document issued in January, include nuclear energy, nuclear fusion, hydrogen, biomass, crystalline silicon solar cells, thin-film solar cells and new energy storage such as batteries, among other areas.

These are “implied to be the major sectoral targets” for the NQPF, according to Kroeber.

In his January speech, Xi said that successful deployment of NQPF requires “accelerating green science and technology innovation…promoting application of advanced green technology…strengthening the green manufacturing industry…growing the green energy industry…[and] developing green and low-carbon industrial and supply chains”.

Much of this will be driven by state-coordinated efforts. China Daily says that efforts to cultivate NQPF “will encourage its centrally administered state-owned enterprises [SOEs] to deploy more resources toward developing strategic emerging industries”.

Kroeber believes that this will lead to “national resources [being] mobilised through a ‘new national system’ (新型举国体制)”.

He tells Carbon Brief that the system is an attempt to “create better coordination mechanisms” between the central and local governments in order to better achieve policy goals, such as through research consortiums focused on technological innovations.

This is inspired by the success of China’s electric vehicle (EV) industry, which benefited both from significant state support and from the emergence of innovative and intensely competitive businesses.

Several commentaries and articles highlight EVs as a key example of NQPF working in practice.

Wang Yiming, vice chairman of the China Center for International Economic Exchanges and former vice minister of the Development Research Center of the State Council, wrote in the state-sponsored Guangming Daily that “the rapid development of China’s EVs is a vivid case of NQPF, formed by the deep transformation and upgrading of industry”.

Using innovation to foster leading expertise across different industries, China hopes, will allow the country to replicate its achievements in the EV sector in other industries.

For example, a blog post on Yuyuan Tantian, a WeChat account affiliated with state broadcaster CCTV, draws a link between China’s experience in manufacturing LCD televisions and its later success in developing solar technologies, which require similar manufacturing technologies and processes.   

Prof Zhang tells China Environment News:

“New quality productive forces are not simply a process of transformation from old productivity to new productivity…It is a qualitative leap in productivity based on the achievements of the new round of scientific and technological revolution and industrial transformation, which is characterised by green, intelligent and ubiquitous (绿色、智能、泛在) trends.”

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What are the concerns over NQPF? 

China’s use of state resources to support strategically important industries, such as EVs, has recently fuelled anxieties about “overcapacity” in some countries.

Both the US and the EU have imposed tariffs on China-made EV imports. The EU’s tariff rate for individual automakers is based on the amount of state subsidies, including R&D grants, that the bloc determined those companies to have received. 

There are also concerns around overcapacity domestically. A March Reuters article quoted an anonymous Chinese policy adviser saying: “The direction of promoting tech innovation is right, but my worry is how to achieve it – what path and what institutional mechanisms should we rely on?”

To a point, these concerns are also shared by the leadership. In an article translated by the Pekingology newsletter, Han Wenxiu, a top economic policy planner, cautioned against “campaign-style” implementation of NQPF policies that lead to “neglecting or abandoning traditional industries”, as well as “blind conformity and bubbles”.

Some analysts have linked NQPF to a broader push for faster economic growth and challenges tackling “deep-seated difficulties” in economic reform, which has led to a “lack of more radical action on consumption”.

Michael Pettis, senior fellow at the Carnegie Endowment, is quoted by the Financial Times saying that “the exit strategy has to be, at the end of the day, consumption – there’s no point producing all this stuff if no one’s going to buy it”. 

But given current tensions with the US, Kroeber tells Carbon Brief, China “can’t rely on imports of technology in the same way…It must have an all-of-nation effort to develop its own alternatives for the technologies it used to import.”

France's President Emmanuel Macron, Chinese President Xi Jinping and European Commission President Ursula von der Leyen at the Elysee Palace in Paris, on 6 May 2024.
France’s President Emmanuel Macron, Chinese President Xi Jinping and European Commission President Ursula von der Leyen at the Elysee Palace in Paris, on 6 May 2024. Credit: Eliot Blondet / Alamy Stock Photo

In his view, efforts to foster NQPF “could” lead to the creation of more capacity – although he finds concerns around overcapacity to be overly “politicised”.

He says that any spikes in capacity may be “unintentional” as “the Europeans and Chinese are actually starting discussions on [resolving concerns around] EVs”.

Yang tells Carbon Brief that “innovative technologies are often not commercially viable and struggle to compete with mature technologies in the market”, highlighting the need for government support to make the EV industry viable. He adds:

“The world needs to achieve rapid and deep decarbonisation within a very short timeframe. The market often drives incremental change. But what is required now is more radical, fundamental change.”

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Will NQPF translate into concrete climate policy?

At a press conference on 24 June, the Ministry of Ecology and Environment (MEE) announced that it will release a ‘1+N’ policy on NQPF, which will “promote the accelerated development of NQPF” and “thicken” the “green-ness” of high-quality development (​​厚植高质量发展的绿色底色).

This followed an article in Qiushi by MEE minister Huang Runqiu and party secretary Sun Jinlong, who wrote that “ecology is itself the economy – if you protect ecology, ecology will give you returns”.

The ‘1+N’ framework is well-established in Chinese environmental policymaking, forming the basis for China’s climate policy. 

It refers to “1” policy setting overarching objectives, which guides numerous (“N”) action plans and policy measures that include more concrete targets.

The MEE said that NQPF “can help promote the significant decline of pollutants and carbon emissions, and radically improve the quality of the ecological environment”.

An article on 'green productive forces' by MEE minister Huang Runqiu and party secretary Sun Jinlong.
An article on ‘green productive forces’ by MEE minister Huang Runqiu and party secretary Sun Jinlong. Source: Qiushi

On 11 July, it released one of the first “N” policies in the system – regulations to update “management of ecological environment zoning control”.

Analysis by consulting firm Trivium China questions whether this “will directly contribute” to development of NQPF, but adds that it could signal the MEE “leveraging” the concept to “push through reforms that might otherwise be stymied” by other stakeholders.

Meanwhile, the Ministry of Science and Technology (MOST) announced on 17 July that it will establish a centre for promoting NQPF. This may improve MOST’s “autonomy” in policy planning for science and technology innovation, an analyst told finance newspaper 21st Century Business Herald

Kroeber says that “every document the government comes out with now has to have some reference to NQPF. It’s just a way for bureaucrats to say ‘we have heard the signal [from Beijing] and we are pursuing [those goals]’”.

He adds that one area in which China may issue more concrete policies is power market reform.

China has been trying to “introduce more competition” into its power market to address a range of challenges inherent to the old grid system, including increasing the share of renewable power in overall power generation. 

It is “an area where this idea of coordination and the state playing a more leading role in getting everyone to move together” is crucial, Kroeber says, given the importance of access to abundant, low-cost electricity to power development of more technology.

Seeing further progress “would be the litmus test of whether the government is pursuing its aims [around NQPF] in an effective way”, he adds.

However, Yang tells Carbon Brief that while NQPF “has theoretical underpinnings, it is far from being purely conceptual”.

He says: “I believe more actions in various sectors will come soon to translate it into concrete initiatives and programs.” 

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The Senate makes some improvements, but our defense work continues

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The Senate makes some improvements, but our defense work continues

By Flannery Winchester

On Monday, the Senate Finance Committee released its portion of the big budget bill that’s working its way through Congress. 

After the House passed a version of this bill that drastically cuts America’s clean energy tax credits, we’ve been pushing hard on the Senate — and the Senate Finance Committee in particular — to do a better job protecting these important measures.

So, how did this Senate committee do? Indeed, a bit better than the House!

As Heatmap reported, “Senate Republicans widened the aperture slightly compared to the House version of the bill, extending tax credits for geothermal energy, batteries, and hydropower, and preserving ‘transferability’ — a crucial rule that allows companies to sell their tax credits for cash — for years to come.”

These shifts are worth acknowledging and appreciating. These shifts mean that our advocacy work to defend these tax credits is making a meaningful difference in what members of Congress are willing to support. Our engagement is leading to better outcomes for climate and clean energy than there would be if we weren’t engaging on this. 

We’re grateful to all of our volunteers who sent emails, made calls, and published local media over the last few weeks as we pushed hard to show Senators the value of these tax credits.

‘Better’ still isn’t ‘best’ 

Now, that said — even with these improvements from the House version of the bill, the Senate’s bill “would still slash many of the signature programs of the Inflation Reduction Act,” Heatmap reports

We still prefer the clean energy tax credits to be left intact. CCL doesn’t endorse this bill and won’t encourage members of Congress to vote for it. 

But we’re proud of all the ways we’ve helped push for a better outcome than full repeal of these clean energy tax credits, which many Republican lawmakers campaigned on last fall. 

And, crucially, our defense work is not over yet. The chair of the Senate Finance Committee, Sen. Mike Crapo (R-ID), recently told Politico that Republicans are “not done writing the bill” and there are “all kinds of issues that are still being evaluated.”

That means we have another window to continue to advocate for better protection of the clean energy tax credits as negotiations continue. That’s why today we launched a new action for CCLers to email their Republican Senators with a message tailored to this moment, using data that we know makes an impact on these lawmakers. If you’re represented by at least one Republican Senator, send them a message today.

After you’ve contacted your Republican Senators, the next best opportunity to make a difference on this issue is to plan to join us in D.C. for our Summer Conference and Lobby Day next month. Negotiations are ongoing, and we’ll be pushing for the best results possible for climate and clean energy every step of the way. Learn more and register now to secure your lobby spot and bring the discussion from your hometown right to Capitol Hill.

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Guest post: How the world’s rivers are releasing billions of tonnes of ‘ancient’ carbon

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The perception of how the land surface releases carbon dioxide (CO2) typically conjures up images of large-scale deforestation or farmers churning up the soil.

However, there is an intriguing – and underappreciated – role played by the world’s rivers.

Right now, plants and soils absorb about one-third of the CO2 released by human activity, similar to how much the oceans take up.

Over thousands to millions of years, some of this land-fixed carbon can end up being buried in sediments, where it eventually forms rocks.

The waters that feed rivers flow through plants, soils and rocks in landscapes, picking up and releasing carbon as they go.

This process is generally considered to be a sideways “leakage” of the carbon that is being taken up by recent plant growth.

However, the age of this carbon – how long it resided in plants and soils before it made it into rivers and then to the atmosphere – has remained a mystery.

If the carbon being released by rivers is young, then it can be considered a component of relatively quick carbon cycling.

However, if the carbon is old, then it is coming from landscape carbon stores that we thought were stable – and, therefore, represents a way these old carbon stores can be destabilised.

In our new study, published in Nature, we show that almost 60% of the carbon being released to the atmosphere by rivers is from these older sources.

In total, this means the world’s rivers emit more than 7bn tonnes of CO2 to the atmosphere each year – more than the annual fossil-fuel emissions from North America.

This means that there is a significant leak of carbon from old stores that we thought were safely locked away.

Previous work has shown that local land-use change, such as deforestation and climate-driven permafrost thaw, will directly release old carbon into rivers. Whether this is happening at the global scale remains a significant unknown for now.

Who are you calling old?

How do you tell how old carbon is? We employ the same technique that is used to determine the age of an archaeological relic or to verify the age of a vintage wine – that is, radiocarbon dating.

Radiocarbon is the radioactive isotope of carbon, which decays at a known rate. This enables us to determine the age of carbon-based materials dating back to a maximum age of about 60,000 years old.

We know that some of the carbon that rivers release is very young, a product of recent CO2 uptake by plants.

We also know that rivers can receive carbon from much older sources, such as the decomposition of deep soils by microbes and soil organisms or the weathering and erosion of ancient carbon in rocks.

Soil decomposition can release carbon ranging from a few years to tens of thousands of years. An example of very old soil carbon release is from thawing permafrost.

Rock weathering and erosion releases carbon that is millions of years old. This is sometimes referred to as “radiocarbon-dead” because it is so old all the radiocarbon has decayed.

Rivers are emitting old carbon

In our new study, we compile new and existing radiocarbon dates of the CO2 emissions from around 700 stretches of river around the world.

We find that almost 60% of the carbon being released to the atmosphere by rivers is from older sources (hundreds to thousands of years old, or older), such as old soil and ancient rock carbon.

In the figure below, we suggest how different processes taking place within a landscape can release carbon of different ages into rivers, driving its direct emission to the atmosphere.

Diagram representing the processes that drive young (decadal) and old (millennial and petrogenic) CO2 emissions from rivers. Values are given as petagrams of carbon, equivalent to billions of tonnes. Credit: Dean et al. (2025)
Diagram representing the processes that drive young (decadal) and old (millennial and petrogenic) CO2 emissions from rivers. Values are given as petagrams of carbon, equivalent to billions of tonnes. Credit: Dean et al. (2025)

So, while rivers are leaking some modern carbon from plants and soils as part of the landscape processes that remove CO2 from the atmosphere, rivers are also leaking carbon from much older landscape carbon stores.

One major implication of this finding is that modern plants and soils are leaking less carbon back to the atmosphere than previously thought, making them more important for mitigating human-caused climate change.

We find that the proportion of old carbon contributing to river emissions varies across different ecosystems and the underlying geology of the landscapes they drain.

In the figure below, we show that landscapes underlain by sedimentary rocks, which are the most likely to contain substantial ancient (or “petrogenic”) carbon, also had the oldest river emissions. We also show that the type of ecosystem (biome) was also important, although the patterns were less clear.

Radiocarbon content (age) of river carbon emissions in different ecosystems (“Biome”) and in landscapes underlain by different geology (“Lithology”). The lower the amount of radiocarbon (F14Catm), the older the age. Credit: Dean et al. (2025)
Radiocarbon content (age) of river carbon emissions in different ecosystems (“Biome”) and in landscapes underlain by different geology (“Lithology”). The lower the amount of radiocarbon (F14Catm), the older the age. Credit: Dean et al. (2025)

What is obvious is that at least some old carbon was common across most of the rivers we observed, regardless of size and location.

We provide evidence that there is a geological control on river emissions. And the variability in the ecosystem also indicates important controlling factors, such as soil characteristics, vegetation type and climate – especially rainfall patterns and temperature which are known to impact the rate of carbon release from soils and rock weathering.

Are old carbon stores stable?

Long-term carbon storage in soils and rocks is an important process regulating global climate.

For example, the UK’s peatlands are important for regulating climate because they can store carbon for thousands of years. That is why restoring peatlands is such a great climate solution.

Rivers emit more than 7bn tonnes of CO2 to the atmosphere each year – that’s equivalent to about 10-20% of the global emissions from fossil fuel burning annually.

If 60% of river carbon emissions are coming from old carbon stores, then this constitutes a significant leak of carbon from old stores we thought were safely locked away.

Another major implication of our study is that these old carbon stores can be mobilised and routed directly to the atmosphere by rivers, which would exacerbate climate change if these stores are further destabilised.

As can be seen in the figure below, we found that river carbon emissions appeared to be getting older since measurements first began in the 1990s (lower F14Catm means older radiocarbon ages).

We found that river carbon emissions appeared to be getting older since measurements first began in the 1990s.

While there are several caveats to interpreting this trend, it is a warning sign that human activities, especially climate change, could intensify the release of carbon to the atmosphere via rivers.

Given the strong link between soil carbon and river emissions, if this trend is a sign of human activity disturbing the global carbon cycle, it is likely due to landscape disturbance mobilising soil carbon.

The age of carbon emissions from rivers appears to be getting older since measurements began in the early 1990s. Icons show dissolved inorganic carbon (grey dots), CO2 (orange squares) and methane (grey crosses). The dashed horizontal line indicates F14Catm = 1.0, for which F14C content is in equilibrium with atmospheric levels in the year of sample collection. Credit: Dean et al. (2025)
The age of carbon emissions from rivers appears to be getting older since measurements began in the early 1990s. Icons show dissolved inorganic carbon (grey dots), CO2 (orange squares) and methane (grey crosses). The dashed horizontal line indicates F14Catm = 1.0, for which F14C content is in equilibrium with atmospheric levels in the year of sample collection. Credit: Dean et al. (2025)

Using rivers to monitor global soil carbon storage

Rivers collect waters from across the landscapes they flow through and therefore provide a tool to track processes happening out of sight.

A drop of water landing in a landscape travels through soils and rock before reaching the river, and its chemistry, including its radiocarbon age, reflects the processes occurring within the landscape.

Monitoring the age of carbon in rivers can therefore tell you a lot about whether their landscapes are storing or releasing carbon.

This has been shown to help identify carbon loss in degraded tropical peatlands, thawing Arctic permafrost and due to deforestation.

River radiocarbon is sensitive to environmental change and could therefore be a powerful monitoring tool for detecting the onset of climate tipping points or the success of landscape restoration projects, for example.

While we present data spread out across the world, there are quite a few gaps for important regions, notably where glacier change is happening and others where droughts and flood frequencies are changing.

These include areas with low amounts of data in Greenland, the African continent, the Arctic and Boreal zones, the Middle East, eastern Europe, western Russia, Central Asia, Australasia and South America outside of the Amazon.

All these regions have the potential to store carbon in the long-term and we do not yet know if these carbon stores are stable or not under present and future climate change.

River radiocarbon offers a powerful method to keep tabs on the health of global ecosystems both now and into the future.

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Guest post: Why 2024’s global temperatures were unprecedented, but not surprising

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Human-caused greenhouse gas (GHG) emissions in 2024 continued to drive global warming to record levels.

This is the stark picture that emerges in the third edition of the “Indicators of Global Climate Change” (IGCC) report, published in Earth System Science Data.

IGCC tracks changes in the climate system between Intergovernmental Panel on Climate Change (IPCC) science reports.

In doing so, the IGCC fills the gap between the IPCC’s sixth assessment (AR6) in 2021 and the seventh assessment, expected in 2028.

Following IPCC methods, this year’s assessment brings together a team of over 60 international scientists, including former IPCC authors and curators of vital global datasets.

As in previous years, it is accompanied by a user-friendly data dashboard focusing on the main policy-relevant climate indicators, including GHG emissions, human-caused warming, the rate of temperature change and the remaining global carbon budget.

Below, we explain this year’s findings, highlighting the role that humans are playing in some of the fundamental changes the global climate has seen in recent years.

Headline results from an analysis of key climate indicators in 2024, compared to the IPCC AR6 climate science report. Source: Forster et al. (2025)

(For previous IGCC reports, see Carbon Brief’s detailed coverage in 2023 and 2024.)

An ‘unexceptional’ record high

Last year likely saw global average surface temperatures hit at least 1.5C above pre-industrial levels. This aligns with other major assessments of the Earth’s climate.

Our best estimate is a rise of 1.52C (with a range of 1.39-1.65C), of which human activity contributed around 1.36C. The rest is the result of natural variability in the climate system, which also plays a role in shaping global temperatures from one year to the next.

Our estimate of 1.52C differs slightly from the 1.55C given by the World Meteorological Organisation (WMO) state of the global climate 2024 report, published earlier this year. This is because they make slightly different selections on which of the available global land and ocean temperature datasets to include. (The warming estimate has varied by similar amounts in past years and future work will aim to harmonise the approaches.)

The height of 2024’s temperatures, while unprecedented in at least the last 2,000 years, is not surprising. Given the high level of human-induced warming, we might currently expect to see annual temperatures above 1.5C on average one year in six.

However, with 2024 following an El Niño year, waters in the North Atlantic were warmer than average. These conditions raise this likelihood to an expectation that 1.5C is surpassed every other year.

From now on, we should regard 2024’s observed temperatures as unexceptional. Temperature records will continue to be broken as human-caused temperature rise also increases.

Longer-term temperature change

Despite observed global temperatures likely rising by more than 1.5C in 2024, this does not equate to a breach of the Paris Agreement’s temperature goal, which refers to long-term temperature change caused by human activity.

IGCC also looks at how temperatures are changing over the most recent decade, in line with IPCC assessments.

Over 2015-24, global average temperatures were 1.24C higher than pre-industrial levels. Of this, 1.22C was caused by human activity. So, essentially, all the global warming seen over the past decade was caused by humans.

Observed global average temperatures over 2015-24 were also 0.31C warmer than the previous decade (2005-14). This is unsurprising given the high rates of human-caused warming over the same period, reaching a best estimate of 0.27C per decade.

This rate of warming is large and unprecedented. Over land, where people live, temperatures are rising even faster than the global average, leading to record extreme temperatures.

But every fraction of a degree matters, increasing climate impacts and loss and damage that is already affecting billions of people.

Driven by emissions

Undoubtedly, these changes are being caused by GHG emissions remaining at an all-time high.

Over the last decade, human activities have released, on average, the equivalent of around 53bn tonnes of CO2 into the atmosphere each year. (The figure of 53bn tonnes expresses the total warming effect of CO2 and other greenhouse gases, such as methane and nitrous oxide, using CO2 as a reference point.)

Emissions have shown no sign of the peak by 2025 and rapid decline to net-zero required to limit global warming to 1.5C with no or limitedovershoot”.

Most of these emissions were from fossil fuels and industry. There are signs that energy use and emissions are rising due to air conditioning use during summer heatwaves. Last year also saw high levels of emissions from tropical deforestation due to forest fires, partly related to dry conditions caused by El Niño.

Notably, emissions from international aviation – the sector with the steepest drop in emissions during the Covid-19 pandemic – returned to pre-pandemic levels.

The amount of CO2 in the atmosphere, alongside the other major GHGs of methane (CH4) and nitrous oxide (N2O), is continuing to build up to record levels. Their concentrations have increased by 3.1, 3.4 and 1.7%, respectively, since the 2019 values reported in the last IPCC assessment.

At the same time, aerosol emissions, which have a cooling effect, are continuing to fall as a result of important efforts to tackle air pollution. This is currently adding to the rate of GHG warming.

Notably, cutting CH4 emissions, which are also short-lived in the atmosphere, could offset this rise. But, again, there is no real sign of a fall – despite major initiatives such as the Global Methane Pledge.

The effect of all human drivers of climate change on the Earth’s energy balance is measured as “radiative forcing”. Our estimate of this radiative forcing in 2024 is 2.97 Watts per square metre (W/m2), 9% above the value recorded in 2019 that was quoted in the last IPCC assessment.

This is shown in the figure below, which illustrates the percentage change in an array of climate indicators since the data update given in the last IPCC climate science report.

Bar chart: Key Indicators of Global Climate Change: Percentage change since IPCC Sixth Assessment Report
Percentage changes in key climate indicators in 2024, compared to the IPCC AR6 climate science report. The remaining carbon budget given on the right is the only indicator to show a reduction and is the change since IPCC AR6, presented as a shrinking box. Source: Forster et al. (2025)

Continued emissions and rising temperatures are meanwhile rapidly eating into the remaining carbon budget, the total amount of CO2 that can be emitted if global warming is to be kept below 1.5C.

Our central estimate of the remaining carbon budget from the start of 2025 is 130bn tonnes of CO2.

This has fallen by almost three-quarters since the start of 2020. It would be exhausted in a little more than three years of global emissions, at current levels.

However, given the uncertainties involved in calculating the remaining carbon budget, the actual value could lie between 30 and 320bn tonnes, meaning that it could also be exhausted sooner – or later than expected.

Beyond global temperatures

Our assessment also shows how surplus heat is accumulating in the Earth’s system at an accelerating rate, becoming increasingly out of balance and driving changes around the world.

The data and their changes are displayed on a dedicated Climate Change Tracker platform, shown below.

Webpage screenshot: Indicators of Global Climate Change 2024
Snapshot of Climate Change Tracker

The radiative forcing of 2.97 W/m2 adds heat to the climate system. As the world warms in response, much of this excess heat radiates to space, until a new balance is restored. The residual level of heating is termed the Earth’s “energy imbalance” and is an indication of how far out of balance the climate system is and the warming still to come.

This residual rate of heat entering the Earth system has now approximately doubled from levels seen in the 1970s and 1980s, to around 1W/m2 on average during the period 2012-24.

Although the ocean is storing an estimated 91% of this excess heat, mitigating some of the warming we would otherwise see at the Earth’s surface, it brings other impacts, including sea level rise and marine heatwaves.

Global average sea level rise, from both the melting of ice sheets and thermal expansion due to deep ocean warming, is included in the IGCC assessment for the first time.

We find that it has increased by around 26mm over the last six years (2019-24), more than double the long-term rate. This is the indicator that shows the clearest evidence of an acceleration.

Sea level rise is making storm surges more damaging and causing more coastal erosion, having the greatest impact on low-lying coastal areas. The 2019 IPCC special report on the oceans and cryosphere estimated that more than one billion people would be living in such low-lying coastal zones by 2050.

Multiple indicators

Overall, our indicators provide multiple lines of evidence all pointing in the same direction to provide a clear and consistent – but unsurprising and worsening – picture of the climate system.

It is also now inevitable that global temperatures will reach 1.5C of long-term warming in the next few years unless society takes drastic, transformative action – both in cutting GHG emissions and stopping deforestation.

Every year of delay brings reaching 1.5C – or even higher temperatures – closer.

This year, countries are unveiling new “nationally determined contributions” (NDCs), the national climate commitments aimed at collectively reducing GHG emissions and tackling climate change in line with the Paris Agreement.

While the plans put forward so far represent a step in the right direction, they still fall far short of what is needed to significantly reduce, let alone stop, the rate of warming.

At the same time, evidence-based decision-making relies on international expertise, collaboration and global datasets.

Our annual update relies on data from NASA and the National Oceanic and Atmospheric Administration (NOAA) and input from many of their highly respected scientists. It is this type of collaboration that allows scientists to generate well-calibrated global datasets that can be used to produce trusted data on changes in the Earth system.

It would not be possible to maintain the consistent long-term datasets employed in our study if their work is interrupted.

At a time when the planet is changing at the fastest rate since records began, we are at risk of failing to track key indicators – such as greenhouse gas concentrations or deep ocean temperatures – and losing core expertise that is vital for understanding the data.

The post Guest post: Why 2024’s global temperatures were unprecedented, but not surprising appeared first on Carbon Brief.

Guest post: Why 2024’s global temperatures were unprecedented, but not surprising

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