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The first three months of 2026 have been the fourth warmest on record, with each successive month surpassing historical averages by a greater margin.

While weak La Niña conditions pushed down temperatures at the start of the year, scientists expect the development of a strong – and potentially “super” – El Niño event by early autumn.

El Niño and La Niña are the warm and cool phases of the El Niño-Southern Oscillation (ENSO), a recurring climate pattern in the tropical Pacific that shapes global weather patterns.

Based on temperature datasets from five different research groups, Carbon Brief predicts that 2026 is likely to be the second-warmest year on record.

The year is virtually certain to be one of the four warmest on record and, currently, has a 19% chance of surpassing 2024 as the warmest year on record.

However, the development of a strong El Niño event later this year would substantially increase the chance that 2027 will be the warmest year on record.

In addition to near-record warmth, the start of 2026 has seen record-low sea ice cover in the Arctic, with the year tying with 2025 for the lowest winter peak in the satellite record.

Fourth-warmest start to the year

In this latest quarterly state of the climate assessment, Carbon Brief analyses records from five different research groups that report global surface temperature records: NASA, NOAA, Met Office Hadley Centre/UEA, Berkeley Earth and Copernicus/ECMWF.

The figure below shows the annual temperatures from each of these groups since 1970, along with the average over the first three months of 2026.

Chart showing global surface temperature records from 1970-2025 and 2026 to date
Annual global average surface temperatures from NASA GISTEMP, NOAA GlobalTemp, Hadley/UEA HadCRUT5, Berkeley Earth and Copernicus/ECMWF’s ERA5 (lines), along with 2026 temperatures so far (January-March, coloured dots). Anomalies plotted with respect to the 1981-2010 period and shown relative to pre-industrial based on the average pre-industrial temperatures in the Hadley/UEA, NOAA and Berkeley datasets that extend back to 1850.

(It is worth noting that warming in the first three months may not be representative of the year as a whole, as temperatures relative to pre-industrial levels tend to be larger in the northern hemispheric winter months of December, January and February.)

Carbon Brief provides a best estimate of global temperatures by averaging the different records using a common 1981-2010 baseline period and then adding in the average warming since the pre-industrial period (1850-1900) across the datasets – NOAA, Hadley and Berkeley – that extend back to 1850. (This follows the approach taken by the World Meteorological Organization in its state of the climate reports.)

The figure below shows how global temperature so far in 2026 (black line) compares to each month in different years since 1940 (lines coloured by the decade in which they occurred).

Chart showing monthly global temperature anomalies
Temperatures for each month from 1940 to 2026 from the Carbon Brief average of temperature records. Anomalies plotted with respect to a 1850-1900 baseline.

The first three months of 2026 have been relatively warm, coming in in the top-five warmest on record across all the different scientific groups that report on global surface temperatures. This is despite the presence of weak La Niña conditions in the tropical Pacific at the start of the year, which typically suppress global temperatures.

January 2026 was the fourth- or fifth-warmest January on record across all the groups, February was the fourth- to sixth-warmest and March was between the second and fourth warmest.

Dataset January February March
HadCRUT5 5th 6th Yet To Report
NOAA 5th 5th 2nd
GISTEMP 5th 4th 4th
Berkeley Earth 4th 4th 4th
Copernicus ERA5 5th 5th 4th

Global temperature anomalies have been steadily increasing since their low point in January, as La Niña conditions have faded.

When combined, the first three months of the year in 2026 were the fourth-warmest in the historical record, below only 2024, 2025 and 2016.

Chart showing that 2026 was the forth-hottest start to a year on record
Quarter one temperature anomalies from 1850 through 2026 from Carbon Brief’s average of temperature records. Anomalies plotted with respect to a 1850-1900 baseline.

A potential ‘super’ El Niño

There is reason to expect that global temperatures will continue to increase over the remainder of the year, as a strong – or even “super” – El Niño event is expected to develop later in the year.

Since the start of April, 13 different modelling groups have published estimates of future El Niño strength through at least September. These, in turn, contain 637 different model runs, as each model is run multiple times to better characterise the range of potential El Niño development.

There are a number of different ways to assess the strength of an El Niño or La Niña event.

The most common is the temperature anomaly in the “Niño3.4” region of the tropical Pacific. In addition, these temperatures have the human warming signal removed from changes over time in that part of the Pacific.

There are other approaches to assessing the strength of El Niño, including the newly released relative Oceanic Niño Index (RONI), which may be more accurate. However, RONI data is not readily available from all models today.

The figure below shows a distribution of Niño3.4 temperature anomalies across all of the runs of all of the models (top panel), as well as the range of runs across each of the individual models (bottom panel). Sustained sea surface temperatures in excess of 0.5C indicate an El Niño event, temperatures above 1.5C represent a strong El Niño event and above 2C is often referred to as a “super” El Niño event.

Charts showing the ENSO forecast for September 2026 from 13 modelling groups
Nino3.4 region temperature anomaly forecasts for September 2026 from 637 model runs by 13 modelling groups. The top panel shows a model-weighted density of estimates, where each model is given equal weight regardless of the number of ensemble members. The bottom panel shows the median and ensemble range for each individual model. Data obtained from Copernicus C3S, NOAA’s CFSv2, CanSIPS and NMME.

The latest climate models give a central (median) estimate of 2.2C warming by September – a scenario which would put the world firmly in “super” El Niño territory.

Warming would likely strengthen after September, as El Niño conditions generally peak between November and January.

However, there is still a wide spread among models, with some, such as CanESM5 and DWD, only showing a weak-to-moderate El Niño.

Historically, it has been hard to accurately forecast the development of El Niño during early spring, so it will be a few more months before scientists can be confident that a strong or super El Niño will develop.

Exceptional regional warmth

There were many regions of the planet that saw exceptional warmth in the first quarter of 2026. This includes much of the western US, western China and eastern Russia.

The figure below shows the temperature anomaly in the ERA5 dataset, relative to a more recent 1981-2010 baseline period. (ERA5 does not provide gridded data back to the pre-industrial era.)

Map showing global surface temperature anomalies
Global surface temperature anomalies in ERA5 over the January-March period, relative to a 1981-2010 baseline period.

In addition to temperature anomalies, it is useful to look at where new records have been set. The figure below shows each grid cell that saw one of the top-five warmest first-quarter periods on record, as well as the top-five coolest.

Map showing global temperature records
Global surface temperature records (top five and bottom five) in ERA5 over the January-March period over the 1940-2026 period covered by the dataset.

During the first quarter of 2026, 5.2% of the globe saw record warm temperatures, while virtually no place on earth had record cool temperatures. In addition, 24.3% of the globe was in the top-five warmest on record, whereas only 0.1% was in the bottom-five coolest on record.

On track to be second-warmest year on record

Carbon Brief estimates that the global average temperature in 2026 will be between 1.37C and 1.58C, with a best estimate 1.47C. This puts 2026 on track to likely be the second warmest year on record, though it could potentially be as high as the warmest or as low as the fourth warmest.

This is based on the relationship between the first three months and the annual temperatures for every year since 1970. The estimate also accounts for El Niño and La Niña conditions seen in the first three months of 2026, as well as how El Niño conditions are projected to develop across the rest of the year.

The analysis includes a wide range of possible outcomes in 2026, given that temperatures from only the first quarter of the year are available so far.

The chart below shows the expected range of 2026 temperatures using the Carbon Brief average of groups – including a best-estimate (red) and year-to-date value (yellow). Temperatures are shown with respect to the pre-industrial baseline period (1850-1900).

Chart showing that 2026 is on track to be the second-warmest year
Annual global average surface temperature anomalies from the WMO aggregate plotted with respect to a 1850-1900 baseline. To-date 2026 values include January-March. The estimated 2026 annual value is based on the relationship between the January-March temperatures and annual temperatures between 1970 and 2025. Chart by Carbon Brief.

Carbon Brief’s projection suggests that 2026 is virtually certain to be one of the top-four warmest years, with a best-estimate – a 62% chance – that it ends up between 2024 and 2023 as the second-warmest year on record.

However, there remains a 19% chance that 2026 will be the warmest year on record – beating the prior record set in 2024. There is also a 19% chance that it will end up as the third- or fourth-warmest year.

The chances of a record-breaking year depends on the strength of El Niño, as well as how rapidly global temperatures warm up as El Niño develops.

There is also a roughly 30% chance that 2026 will be the second year that exceeds 1.5C above pre-industrial levels.

While the development of a strong or “super” El Niño will give a boost to 2026 temperatures in the latter part of the year, its largest effects will likely be felt in 2027.

Historically, the year where El Niño develops has been warmer than usual, but the year that follows the phenomenon’s winter peak – for example, in 1998, 2016 and 2024 – is record-setting.

This is because there is an approximately three-month lag between the peak of El Niño conditions in the tropical Pacific and the maximum global surface temperature response. If a super El Niño develops this year, it is likely that 2027 will set a new record.

Record-low winter Arctic sea ice

Earlier this year, Arctic sea ice saw the joint-smallest winter peak in a satellite record going back almost half a century.

Sea ice extent peaked for 2026 at 14.29m square kilometres (km2) on 15 March, marking a “statistical tie” with a record low recorded the year before, according to the US National Snow and Ice Data Center (NSIDC).

The figure below shows both Arctic and Antarctic sea ice extent in 2026 (solid red and blue lines), the historical range in the record between 1979 and 2010 (shaded areas) and the record lows (dotted black line).

(Unlike global temperature records, which only report monthly averages, sea ice data is collected and updated on a daily basis, allowing sea ice extent to be viewed up to the present.)

Chart showing the Artic and Antarctic sea ice in 2026
Arctic and Antarctic daily sea ice extent from the NSIDC. The bold lines show daily 2026 values, the shaded area indicates the two standard deviation range in historical values between 1979 and 2010. The dotted black lines show the record lows for each pole.

Arctic sea ice set new record daily low values during periods of January, March and early April. Antarctic sea ice did not set any new records so far in 2026, but remains on the low end of the historical (1979-2010) range.

The post State of the climate: Strong El Niño puts 2026 on track for second-warmest year appeared first on Carbon Brief.

State of the climate: Strong El Niño puts 2026 on track for second-warmest year

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Colorado River Faces ‘Devastating Consequences’ If Another Dry Winter Lands, Experts Warn

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Even a huge snowpack during the coming winter would only give the river basin states less than two years of storage before reservoirs returned to historic lows.

Another warm, arid winter could leave Colorado River reservoirs nearly dry.

Colorado River Faces ‘Devastating Consequences’ If Another Dry Winter Lands, Experts Warn

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Q&A: The current state of ‘carbon dioxide removal’ around the world

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Carbon dioxide removal (CDR) technologies will need to be deployed at rates even faster than those seen for solar power, if the world is to have a chance of limiting global warming to 1.5C by 2100, says a new report.

Nearly all pathways to meeting the Paris Agreement’s highest ambition of keeping global temperatures to 1.5C above pre-industrial levels in 2100 involve CDR techniques – ranging from tree-planting to sucking CO2 from air with machines.

This is in addition to steep and immediate emissions cuts.

Scientists expect carbon emissions to push warming beyond 1.5C in the decade ahead, meaning that the target can only be achieved “from above” via large-scale CDR that brings down global temperatures.

These temperature trajectories are known as “overshoot” pathways.

The third “state of CDR” report, written by more than 50 scientists, says that countries’ current CDR plans would fall short of what is needed to limit warming to 1.5C by more than 5bn tonnes of CO2 (GtCO2) per year by 2050.

Global CDR would have to increase fourfold – from 2.2GtCO2 in 2026 to 8.75GtCO2 by 2050 – to have a chance of meeting the 1.5C target by 2100, according to the report.

It adds that deploying CDR can be a “gradual process”, making the period 2026-30 “crucial” for “establishing CDR’s role in limiting climate damages” in the future.

Below, Carbon Brief covers the key findings of the third state of CDR report. (This follows from Carbon Brief’s coverage of the first report in 2023 and second report in 2024.)

What is CDR?

According to the report, the definition of CDR is:

“Human activities capturing CO2 from the atmosphere and storing it durably in geological, terrestrial or ocean reservoirs, or in products. This includes human enhancement of natural removal processes but excludes natural uptake not directly caused by anthropogenic [human-caused] activities.”

In addition to this, the report includes “three key principles” for CDR, which are:

  1. The captured CO2 must come from the atmosphere, not from “fossil sources”.
  2. The subsequent storage “must be durable”, so that the CO2 is not soon reintroduced to the atmosphere.
  3. The removal must result from human intervention that is in addition to Earth’s natural processes.

In this report, a CDR method is considered durable if it is able to lock up carbon for “decades or more”.

The report classifies CDR techniques as either “conventional” or “novel”.

“Convential” CDR techniques are “well established, already deployed at scale and widely reported by countries as part of [land-use] activities”.

The methods included in this group are tree-planting, ecosystem restoration, agroforestry (trees in agriculture), improving soil carbon in croplands and natural lands, and durable wood production.

“Novel” CDR techniques have “lower level of readiness for deployment and, as a consequence, are currently deployed at smaller scales”, says the report.

Some examples of different CDR methods are listed on the graphic below.

The graphic also shows whether carbon is captured through biological or chemical processes, as well as how “ready” the method is and for how long it can store carbon, among other features.

CDR techniques and their characteristics. Credit: Edwards et al. (2026)

The report says that CDR is “needed alongside deep and rapid emissions reductions” to give Earth a chance of limiting global warming to 1.5C. It continues:

“It should play a smaller role than emissions reductions given uncertainty around the feasible levels of scaling, sustainability limits, storage availability and the risk of reversal, among other constraints.

“In general, CDR should be seen as a limited resource that will need to be used prudently.”

It adds that CDR can “fulfil three major functions”.

In the near term, CDR can help reduce “net emissions”, it says.

In the medium term, CDR can “counterbalance residual emissions” to achieve net-zero CO2 or net-zero greenhouse gas emissions, the report continues.

(“Residual emissions” are those that cannot be eradicated through technologies or societal changes, such as methane emissions from rice production.)

Research suggests that global warming is likely to stop, more or less, once net-zero is achieved globally.

In the long term, CDR can “help achieve net-negative emissions”, a state where CO2 removal exceeds emissions, says the report.

In this state, humans could lower global temperatures. This may allow the world to limit global warming to 1.5C by 2100, even if the temperature target is surpassed earlier on in the century.

Future trajectories where temperatures exceed the 1.5C limit before being brought back down again through CDR techniques are known as “overshoot” pathways.

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What are current levels of CDR?

The report says that, at present, “99.9%” of existing CDR is conventional, land-based techniques such as tree-planting and ecosystem restoration.

The world currently removes 2.2GtCO2 per year, equivalent to around 5% of gross global CO2 emissions, it continues.

The largest contributors to removing CO2 from the atmosphere are China, the US, the EU, Brazil and Russia.

The chart below shows the amount of CO2 removed each year over 2014-23 by the largest contributors, through tree-planting (afforestation) and forest restoration (reforestation).

Chart showing country-level CDR through afforestation and reforestation
CO2 removed via afforestation and reforestation each year by the world’s largest contributors to current CDR. Credit: Edwards et al. (2026)

“Novel” CDR, such as biochar and direct air capture, currently removes just 2m tonnes of CO2 annually at present, according to the report.

However, these methods have been growing at a rate of 40% per year – “similar to successful technologies like solar energy, but insufficient for the scale-up required to meet the Paris temperature goal”, says the report.

The graphic below illustrates how the contribution of conventional CDR currently dwarfs novel CDR, but how the latter techniques are quickly growing.

Infographic showing current CDR are almost entirely from conventional, but novel methods are growing
A graphic illustrating the contribution of “conventional” and “novel” to current CDR methods. Credit: Edwards et al. (2026)

The report says that investment in CDR companies recovered in 2025 following a dip – and its “share of all climate-tech funding” grew to 2.6%.

The report also notes that, at present, most CDR efforts are unevenly distributed across the world.

For example, two-thirds of conventional CDR in voluntary carbon markets is in Latin America, according to the report. (Voluntary carbon markets are where companies can buy credits for carbon-reducing or removing projects, such as tree-planting, to claim that they have “offset” some of their own emissions.)

In addition, most pilot projects that aim to demonstrate novel CDR methods are located in only a few countries, such as Sweden, Denmark and the US, says the report.

The chart below shows the location and timeline of demonstration projects that have been announced, are under construction or in operation globally.

Chart showing demonstration projects announced, under construction or in operation 2020-2030
Location and timeline of demonstration projects that have been announced, are under construction or in operation globally. Credit: Edwards et al. (2026)

The report continues:

“While first-movers play important roles, if their actions do not diffuse more widely, vulnerability emerges, as evidenced by the impact of US climate policy dismantling.”

(For more, see: How is policy impacting CDR demand?)

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How much CDR is needed to reach net-zero goals?

The report examines three scenarios where global temperature rise is limited to “well below” 2C by 2100:

  • A current ambition scenario, based on national climate pledges (but omitting the US);
  • A highest-possible ambition scenario;
  • A delayed ambition scenario, which is consistent with current targets until 2035 and then switches to the highest ambition scenario.

The pledges considered in the report are “nationally determined contributions”, or NDCs, which countries submit periodically to the UN Framework Convention on Climate Change (UNFCCC). NDCs lay out a country’s climate ambition.

Under the current ambition scenario, the report projects a total of 5.9GtCO2 of CDR by 2050 and 12GtCO2 by 2100.

This scenario would result in end-of-century warming of 1.7-2.7C. Importantly, the report says, this scenario does not result in the world reaching net-zero CO2 levels, “meaning that global temperatures would continue to rise, albeit at a much more gradual pace, beyond 2100”.

Under the highest-possible ambition scenario, CDR scales up to 8.8GtCO2 by mid-century and 15.3GtCO2 by the end of the century.

This scenario assumes “full buy-in by all nations”, with economics, scale-up and sustainability providing the main constraints on CDR deployment, the report says.

The highest ambition scenario results in global temperatures peaking at 1.7-1.8C around 2050 and the world achieving net-zero emissions around that time.

Under the delayed ambition scenario, CDR would scale up to 7GtCO2 by 2050 and 23.6GtCO2 by 2100. This scenario shows global temperatures peaking between 1.7C and 2.0C.

This scenario requires larger CDR deployment in the long term than the highest-ambition scenario does, due to the larger cumulative emissions caused by delaying deep emissions reductions.

In both the high ambition and delayed ambition scenarios, the world reaches “deeply net-negative CO2 emissions” by 2100, the report says. This continued deployment of CDR will further draw CO2 from the atmosphere, lowering global temperatures back down to 1.5C.

The chart below shows annual global greenhouse gas emissions through the end of the century under current ambition (red), highest ambition (green) and delayed ambition (blue) scenarios.

Annual emissions, in GtCO2e per year, for the three scenarios: current ambition (red), highest ambition (green) and delayed ambition (blue). Source: Edwards et al. (2026)
Annual emissions, in GtCO2e per year, for the three scenarios: current ambition (red), highest ambition (green) and delayed ambition (blue). Source: Edwards et al. (2026)

While global CDR capacity scales up more slowly in the first and third scenarios, the report notes that, in all three cases, “novel CDR reaches gigatonne-scale deployment by 2050”.

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What does the science say about the potential and costs of CDR?

There is a wide range of both carbon-removal potential and associated costs between different methods of CDR, according to the report.

However, it also notes that these numbers “range widely” in the scientific literature.

The discrepancies in estimates of carbon-removal potential are due to a number of factors, the report says, including a lack of available scientific data, inconsistencies in the assumptions made in assessing technical feasibility and a lack of agreement on what, exactly, “potential” means.

These elements also influence the cost of different CDR methods, but additional factors – such as deployment costs in different areas, technological approaches and scope – also play a role in establishing price differences. Because of this, the report says, “cost estimates are often difficult to compare across methods, complicating design and policy decisions”.

The chart below shows the reported range of mitigation potential (left) and reported range of costs (right) for different CDR methods. The top four rows indicate conventional CDR methods, while bottom 11 rows show novel CDR methods. The chart refers to “mitigation potential”, rather than removal potential, because some estimates do not distinguish between removals and avoided emissions.

(Avoided emissions refers to the difference in emissions from carrying out a project, compared to a hypothetical alternative – such as the reduced emissions from halting deforestation.)

The darker colours indicate estimates that are more constrained, meaning that they are either based on stricter assumptions or there is more agreement between different estimates.

Annual mitigation potential (left) and cost range per tonne of CO2 (right) for conventional and novel CDR methods. Orange bars indicate the range of values reported, with darker colours indicating less uncertainty about the estimates. Source: Edwards et al. (2026)
Annual mitigation potential (left) and cost range per tonne of CO2 (right) for conventional and novel CDR methods. Orange bars indicate the range of values reported, with darker colours indicating less uncertainty about the estimates. Source: Edwards et al. (2026)

The report notes that for most removal methods, the low end of the potential is around 1GtCO2 per year, while the upper limit of costs is more than $200/tCO2.

The least expensive CDR approaches are forestry-based methods, soil-carbon sequestration and biomass burial. For forestry-based methods, the report puts the cost of CDR at $5-$53 per tonne of CO2 removed. Soil-carbon sequestration costs reach as high as $150 per tonne of CO2 removed, but could have negative overall costs “when accounting for crop yield increases potentially resulting” from changed farm-management practices, the report says.

However, it adds that “these CDR methods are typically associated with lower levels of permanence” than other methods.

Other relatively low-cost methods include coastal wetland restoration, biochar, bioenergy with carbon capture and storage (BECCS) and enhanced rock weathering, while ocean alkalinity enhancement is a medium-cost option.

The most expensive methods include direct air carbon capture and storage (DACCS) and direct ocean carbon capture and storage (DOCCS).

The report also notes that a total estimate of CDR removals cannot be obtained by adding up the removal potential of all of the separate methods, since different methods can compete for scarce resources. For example, BECCS, biochar, biomass burial and biomass sinking all rely on the same base input – biomass – and therefore cannot all be maximised at the same time.

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What have governments pledged on CDR?

While many countries include some amount of CDR in their national climate plans, there is currently a large gap between the amount of CDR pledged in these plans and the amount that will be needed to limit global temperature rise to 1.5C by the end of the century, says the report.

This quantity is referred to as the “CDR gap” – the difference between what is pledged and what is needed.

The size of the CDR gap is dependent not just on the pledges made by countries, but also the choice of the “benchmark” scenario against which the pledges are measured. Lower – or delayed – emissions reductions lead to larger shortfalls in the long term, meaning “CDR must subsequently be scaled to very high levels”, says the report.

Current NDCs and other country submissions to the UNFCCC total 2.5GtCO2 per year of removals in 2030, 2.7GtCO2 per year in 2035 and 3.6GtCO2 per year in 2050.

This gives a CDR gap of 0.3GtCO2 in 2030, 1.2GtCO2 in 2035 and 5.2GtCO2 in 2050, according to the report. These figures are obtained using assumed “immediate, ambitious action at all levels to reduce emissions” and the most-ambitious estimates of CDR set out in national pledges. Together, this provides a “lower bound” for the CDR gap, says the report.

By comparison, a 10-year delay in implementing ambitious emissions reductions will result in the need to remove at least an additional 150GtCO2 from the atmosphere, compared to the most ambitious scenario. (See: How much CDR is needed to reach net-zero goals?)

The report says that the CDR gap has widened since the second state of CDR report was released in 2024, due to the US leaving the Paris Agreement. It adds that other countries have “not delivered a step change in ambition” in their latest round of climate pledges.

It also cautions that “credibility issues with national pledges may mean that the CDR gap is actually larger than what we assess here”.

The report notes that current CDR pledges by companies are “substantially higher than country pledges”, at 5GtCO2 per year in 2050. However, it adds, “credibility in these announcements is low”.

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What is the current funding and research landscape for CDR?

Funding of CDR research and development – as well as investment in CDR companies – has continued to increase in recent years.

In total, there has been around $5.6bn in grant funding distributed to CDR research since 2005, according to the report’s analysis. Roughly one-third of this has come in the past three years.

Funding for CDR research grants grew 13% each year between 2022 and 2025, the report says, and the corresponding number of research publications grew at a similar rate.

Funding was largely targeted at a handful of key areas, notably soil carbon sequestration, biochar and forest-based CDR.

DACCS and BECCS only make up a small number of active grants, but together account for around two-fifths of all funding due to “substantially larger” project sizes.

Despite the growth of research grants and scientific publications, the report concludes that early-stage innovation in CDR is “uneven” and says there is “no strong evidence of a step-change”.

It notes that much of the support for CDR has come from projects with a broader focus, rather than those that focus specifically on CDR.

The authors also point to a decline in “inventive activity”, as measured by patenting of CDR-related innovations. While patenting for emissions-cutting technologies in general has been on an upward trajectory, CDR patenting peaked in 2011.

Meanwhile, the report highlights the “remarkable” sustained investment in CDR companies, against a backdrop of falling investment in climate-related technologies. It notes that CDR now accounts for around 3% of overall “climate-tech funding”.

Yet, again, it says future developments remain “uncertain”. Since the previous 2024 “state of CDR” report, companies have scaled back their ambitions and policy reversals – notably in the US – “underscore that funding uncertainty remains a key barrier”. (See: How is policy impacting CDR demand?)

An upward tick in funding in 2025 was driven primarily by a “surge” in grants from predominantly public institutions, as well as $0.5bn in debt financing for a single BECCS project in Sweden.

Reliance on such funding sources “highlight[s] the volatility of the CDR innovation ecosystem”, according to the report.

The report also has a chapter focusing on the voluntary carbon market, which it describes as “propelling most of the current demand for novel CDR”.

The scale of this market remains fairly small, with contracts for 0.04GtCO2 of removals signed last year.

Moreover, the concentration of sales within a small number of buyers – particularly Microsoft – remains a “critical vulnerability”, the authors note.

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How is policy impacting CDR demand?

The report analyses CDR policies in G20 nations – which together account for three-quarters of global emissions – to assess how they are acting to support CDR across their economies.

In total, 140 countries have announced net-zero targets, including virtually all of the world’s major emitters. In doing so, the report points out that the governments of these nations have “implicitly included a role for CDR in their climate plans”.

However, this does not always translate into measures specifically designed to scale up CDR.

Only the EU has adopted a binding, quantified removals target into law – namely, the goal to reach 310m tonnes of CO2 equivalent (MtCO2e) of annual net removals in the land sector by 2030.

Overall, conventional CDR is the main focus of policy, with various governments focusing on tree planting to absorb CO2 from the atmosphere.

Among G20 nations, only the UK and Australia have set specific goals to scale up novel CDR, such as BECCS and DACCS, over the coming decade.

The report highlights some nations, including Canada, Germany, Switzerland and the UK, as taking proactive steps to incentivise CDR.

The authors point to national strategies, financial support for CDR and efforts to integrate it into emissions trading systems (ETS) as examples of effective policy making.

(The report also stresses that the US, which was previously a “leader” on CDR, has now “frozen or dismantled funding and support” for CDR under the Trump administration.)

Most of the successful policies highlighted in the report focus on supporting the supply of CDR, with “less attention so far on creating demand”.

This is significant because CDR “generally lacks a natural market”, meaning there are not automatically buyers willing to spend money on emissions removals. Therefore, the authors say, policy interventions are important to create markets and boost demand.

“Compliance” carbon creditsreferring to credits that can be used to meet legally mandated emissions targets – provide a way to support demand, according to the report authors.

Only some ETSs, such as those used in New Zealand and Australia, allow the use of credits based on forest-related removals for compliance. (It is worth noting that such credits are controversial, as removals by forests are not always permanent.)

The report also highlights the need for “foundational policies to create a governance framework for CDR, including rules for quantification of removal, guidelines for community engagement and the minimisation of negative environmental impacts”.

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The post Q&A: The current state of ‘carbon dioxide removal’ around the world appeared first on Carbon Brief.

Q&A: The current state of ‘carbon dioxide removal’ around the world

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Alligator Alcatraz Emissions Threaten Human Health, Violate Clean Air Act, Lawsuit Claims

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The air pollution is associated with the more than 200 diesel-burning generators powering the Everglades migrant detention facility, along with 100 diesel-burning lighting towers.

A new federal lawsuit contends emissions at the Everglades migrant detention site known as Alligator Alcatraz, associated with more than 200 diesel-burning generators and 100 diesel-burning lighting towers, are harmful to human health and the environment and violate the Clean Air Act.

Alligator Alcatraz Emissions Threaten Human Health, Violate Clean Air Act, Lawsuit Claims

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