The Tropical Forest Forever Facility (TFFF) – a major new rainforest protection fund launched by Brazil at COP30 – is unlikely to make payments to rainforest countries until at least 2028, experts said, while it raises funds in financial markets.
The proposed new mechanism aims to pay rainforest countries for achieving low deforestation rates. Rather than depending on grants, the TFFF would seek to raise public and private capital to make investments in financial markets, and then use part of the returns to reward countries which protect their rainforests.
But raising the US$125 billion of public and private investment needed to make meaningful payments could take years, according to Andrew Deutz, managing director of Global Policy and Partnerships at WWF, one of the organisations involved in the fund’s design.
He said it will likely take two or three years for the fund to raise private capital by issuing bonds, invest the money and generate enough returns to make significant payments. “So I don’t think we’re going to see payments to rainforest countries until 2028 or 2029,” Deutz said.
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Norway’s climate minister Andreas Bjelland Eriksen, another of the fund’s early backers, told Climate Home News that “the TFFF requires scale, which will take some time”, but added that it “is a historic opportunity” to finance the protection of tropical forests “for generations”.
The delay is not necessarily bad, according to Deutz, as it will allow communities to build capabilities and legal structures to handle the new flow of funds. “There needs to be a capacity-building process over the next couple of years with Indigenous organisations and local communities to be able to manage the flow of funds at that level,” he added.
At the COP26 climate summit in 2021, over 140 countries – covering 85% of the world’s forests – pledged to end deforestation by 2030. At last year’s COP30, the Brazilian government promised to create a roadmap towards ending deforestation by that same date.
But governments are far off track, with a yearly review showing that deforestation rates are currently 63% higher than what they should be to reach this goal. An estimated $570 billion funding gap for nature protection has contributed to the deficient results.
First step: raising $10 billion
While the TFFF has a long-term goal of raising $125bn in public and private capital, its proponents say the key goal for the fund in 2026 will be to raise the total amount of public investment to $10bn so that it can start to scale up.
The fund has already raised $6.7bn, but Norway’s $3bn pledge requires that the TFFF raises about $10bn mostly from other funders by the end of 2026 or they will not invest.
Before scaling up to the long-term $125bn goal – of which $25bn is public and $100bn private – the TFFF will have to prove that it can be successful in paying back investors and channeling funds for rainforest protection. The whole process can take years, Deutz said.
If this $10bn target is reached, the fund could begin raising private finance – up to an estimated $40bn, Deutz said. This initial $50bn tranche would serve to start making investments and show that the model works and can generate returns.
Bjelland Eriksen also said that reaching the $10bn target will be “an important priority” this year. “Only a handful of countries had the opportunities to assess it in detail before the [COP30] Belém summit – now is the time for more countries to do so,” the Norwegian minister said.
Public finance from governments is key for the TFFF model because it would act as a guarantee to lower risk for private investors, something very common in the financial sector, said Charlotte Hamill, partner at hedge fund Bracebridge Capital and one of the fund’s financial advisors, at an event earlier in January in Davos.
“Being able to do this at scale is actually really important, not only to be able to make the payments that are necessary for rainforest preservation but also, in a funny way, it allows you to buy slightly less risky assets because you’re gonna have a much larger pool to buy them off of,” she added.
New contributions?
João Paulo de Resende, TFFF Leader at Brazil’s Ministry of Finance, told Climate Home News that the country will continue fundraising efforts throughout this year, and said he has recently concluded a tour in East Asia speaking with government officials from Japan, South Korea and China.
Conversations with the Chinese government have become “a lot more serious”, said Felix Finkbeiner, founder of the non-profit Plant-for-the-Planet, which operates the online tracking platform TFFF Watch. He added that a Chinese investment would likely be similar in size to the French or German contributions, which would grant the country a seat on the TFFF board. France has pledged a €500m ($578m) investment while Germany has promised €1bn ($1.17bn).
While China is categorised as a developing country at UN climate talks, and thus has no legal responsibility to grant climate finance, the TFFF has been seen as an opportunity for the Asian country to contribute because it’s not an official mechanism within the UN. Deutz said that, for the Chinese government to contribute, they will need reassurance that the funds will not be counted as formal climate finance.
The UK is another of the countries expected to announce a contribution in the coming months, both Finkbeiner and Deutz said. The country announced cuts to climate finance this week as it ramps up defense spending, but Deutz noted that it could still contribute with funds to the TFFF.
“I’m still somewhat optimistic that [the $10bn goal] can happen despite the geopolitical turmoil because the TFFF does not require grant money. We’re not competing with humanitarian assistance,” Deutz explained. “Because governments are being asked to make a loan that would be paid back with interest, this comes out of a different pile of money”.
Multilateral banks such as the European Bank for Reconstruction and Development (EBRD) and the Asian Infrastructure Investment Bank (AIIB) also reportedly considered contributions.
Brazil sharing leadership
Despite having led the official launch of the fund and spearheading its fundraising efforts, Brazil is now aiming to “share leadership” as other countries join the TFFF’s steering committee and establish a new board.
De Resende told Climate Home News that “the project no longer belongs solely to Brazil”, and added that the group of countries that have pledged contributions to the TFFF are also now playing a larger role in “finding ways to jointly promote sponsor outreach”.
Deutz said that Brazil wants to move towards a “shared leadership model”. “They are now asking the European countries to have one of them set up to be the co-chairs so that this is not seen as a Brazilian initiative but is rather seen as owned by all of them,” he added.
The fund will now have to form a steering committee, likely chaired by Brazil and one European country, which will instruct the World Bank on setting up the formal structures of the fund.
Bjelland Eriksen said there is “important work” ongoing to formally establish the fund’s investment arm (known as the TFIF), while de Resende said he expects to “have the fund incorporated in some European jurisdiction by the beginning of the second semester.”
The post COP30 rainforest fund unlikely to make first payments until 2028 appeared first on Climate Home News.
COP30 rainforest fund unlikely to make first payments until 2028
N.C. Gov. Josh Stein wants state lawmakers to rethink tax breaks for data centers. The industry’s opacity makes it difficult to evaluate costs and benefits.
Tax breaks for data centers in North Carolina keep as much as $57 million each year into from state and local government coffers, state figures show, an amount that could balloon to billions of dollars if all the proposed projects are built.
The Global Environment Facility (GEF), a multilateral fund that provides climate and nature finance to developing countries, has raised $3.9 billion from donor governments in its last pledging session ahead of a key fundraising deadline at the end of May.
The amount, which is meant to cover the fund’s activities for the next four years (July 2026-June 2030), falls significantly short of the previous four-year cycle for which the GEF managed to raise $5.3bn from governments. Since then, military and other political priorities have squeezed rich nations’ budgets for climate and development aid.
The facility said in a statement that it expects more pledges ahead of the final replenishment package, which is set for approval at the next GEF Council meeting from May 31 to June 3.
Claude Gascon, interim CEO of the GEF, said that “donor countries have risen to the challenge and made bold commitments towards a more positive future for the planet”. He added that the pledges send a message that “the world is not giving up on nature even in a time of competing priorities”.
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Donors under pressure
But Brian O’Donnell, director of the environmental non-profit Campaign for Nature, said the announcement shows “an alarming trend” of donor governments cutting public finance for climate and nature.
“Wealthy nations pledged to increase international nature finance, and yet we are seeing cuts and lower contributions. Investing in nature prevents extinctions and supports livelihoods, security, health, food, clean water and climate,” he said. “Failing to safeguard nature now will result in much larger costs later.”
At COP29 in Baku, developed countries pledged to mobilise $300bn a year in public climate finance by 2035, while at UN biodiversity talks they have also pledged to raise $30bn per year by 2030. Yet several wealthy governments have announced cuts to green finance to increase defense spending, among them most recently the UK.
As for the US, despite Trump’s cuts to international climate finance, Congress approved a $150 million increase in its contribution to the GEF after what was described as the organisation’s “refocus on non-climate priorities like biodiversity, plastics and ocean ecosystems, per US Treasury guidance”.
The facility will only reveal how much each country has pledged when its assembly of 186 member countries meets in early June. The last period’s largest donors were Germany ($575 million), Japan ($451 million), and the US ($425 million).
The GEF has also gone through a change in leadership halfway through its fundraising cycle. Last December, the GEF Council asked former CEO Carlos Manuel Rodriguez to step down effective immediately and appointed Gascon as interim CEO.
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New guidelines
As part of the upcoming funding cycle, the GEF has approved a set of guidelines for spending the $3.9bn raised so far, which include allocating 35% of resources for least developed countries and small island states, as well as 20% of the money going to Indigenous people and communities.
Its programs will help countries shift five key systems – nature, food, urban, energy and health – from models that drive degradation to alternatives that protect the planet and support human well-being by integrating the value of nature into production and consumption systems.
The new priorities also include a target to allocate 25% of the GEF’s budget for mobilising private funds through blended finance. This aligns with efforts by wealthy countries to increase contributions from the private sector to international climate finance.
Niels Annen, Germany’s State Secretary for Economic Cooperation and Development, said in a statement that the country’s priorities are “very well reflected” in the GEF’s new spending guidelines, including on “innovative finance for nature and people, better cooperation with the private sector, and stable resources for the most vulnerable countries”.
Aliou Mustafa, of the GEF Indigenous Peoples Advisory Group (IPAG), also welcomed the announcement, adding that “the GEF is strengthening trust and meaningful partnerships with Indigenous Peoples and local communities” by placing them at the “centre of decision-making”.
The post GEF raises $3.9bn ahead of funding deadline, $1bn below previous budget appeared first on Climate Home News.
GEF raises $3.9bn ahead of funding deadline, $1bn below previous budget
Tropical cyclones that rapidly intensify when passing over marine heatwaves can become “supercharged”, increasing the likelihood of high economic losses, a new study finds.
Such storms also have higher rates of rainfall and higher maximum windspeeds, according to the research.
The study, published in Science Advances, looks at the economic damages caused by nearly 800 tropical cyclones that occurred around the world between 1981 and 2023.
It finds that rapidly intensifying tropical cyclones that pass near abnormally warm parts of the ocean produce nearly double – 93% – the economic damages as storms that do not, even when levels of coastal development are taken into account.
One researcher, who was not involved in the study, tells Carbon Brief that the new analysis is a “step forward in understanding how we can better refine our predictions of what might happen in the future” in an increasingly warm world.
As marine heatwaves are projected to become more frequent under future climate change, the authors say that the interactions between storms and these heatwaves “should be given greater consideration in future strategies for climate adaptation and climate preparedness”.
‘Rapid intensification’
Tropical cyclones are rapidly rotating storm systems that form over warm ocean waters, characterised by low pressure at their cores and sustained winds that can reach more than 120 kilometres per hour.
The term “tropical cyclones” encompasses hurricanes, cyclones and typhoons, which are named as such depending on which ocean basin they occur in.
When they make landfall, these storms can cause major damage. They accounted for six of the top 10 disasters between 1900 and 2024 in terms of economic loss, according to the insurance company Aon’s 2025 climate catastrophe insight report.
These economic losses are largely caused by high wind speeds, large amounts of rainfall and damaging storm surges.
Storms can become particularly dangerous through a process called “rapid intensification”.
Rapid intensification is when a storm strengthens considerably in a short period of time. It is defined as an increase in sustained wind speed of at least 30 knots (around 55 kilometres per hour) in a 24-hour period.
There are several factors that can lead to rapid intensification, including warm ocean temperatures, high humidity and low vertical “wind shear” – meaning that the wind speeds higher up in the atmosphere are very similar to the wind speeds near the surface.
Rapid intensification has become more common since the 1980s and is projected to become even more frequent in the future with continued warming. (Although there is uncertainty as to how climate change will impact the frequency of tropical cyclones, the increase in strength and intensification is more clear.)
Marine heatwaves are another type of extreme event that are becoming more frequent due to recent warming. Like their atmospheric counterparts, marine heatwaves are periods of abnormally high ocean temperatures.
Previous research has shown that these marine heatwaves can contribute to a cyclone undergoing rapid intensification. This is because the warm ocean water acts as a “fuel” for a storm, says Dr Hamed Moftakhari, an associate professor of civil engineering at the University of Alabama who was one of the authors of the new study. He explains:
“The entire strength of the tropical cyclone [depends on] how hot the [ocean] surface is. Marine heatwave means we have an abundance of hot water that is like a gas [petrol] station. As you move over that, it’s going to supercharge you.”
However, the authors say, there is no global assessment of how rapid intensification and marine heatwaves interact – or how they contribute to economic damages.
Using the International Best Track Archive for Climate Stewardship (IBTrACS) – a database of tropical cyclone paths and intensities – the researchers identify 1,600 storms that made landfall during the 1981-2023 period, out of a total of 3,464 events.
Of these 1,600 storms, they were able to match 789 individual, land-falling cyclones with economic loss data from the Emergency Events Database (EM-DAT) and other official sources.
Then, using the IBTrACS storm data and ocean-temperature data from the European Centre for Medium-Range Weather Forecasts, the researchers classify each cyclone by whether or not it underwent rapid intensification and if it passed near a recent marine heatwave event before making landfall.
The researchers find that there is a “modest” rise in the number of marine heatwave-influenced tropical cyclones globally since 1981, but with significant regional variations. In particular, they say, there are “clear” upward trends in the north Atlantic Ocean, the north Indian Ocean and the northern hemisphere basin of the eastern Pacific Ocean.
‘Storm characteristics’
The researchers find substantial differences in the characteristics of tropical cyclones that experience rapid intensification and those that do not, as well as between rapidly intensifying storms that occur with marine heatwaves and those that occur without them.
For example, tropical cyclones that do not experience rapid intensification have, on average, maximum wind speeds of around 40 knots (74km/hr), whereas storms that rapidly intensify have an average maximum wind speed of nearly 80 knots (148km/hr).
Of the rapidly intensifying storms, those that are influenced by marine heatwaves maintain higher wind speeds during the days leading up to landfall.
Although the wind speeds are very similar between the two groups once the storms make landfall, the pre-landfall difference still has an impact on a storm’s destructiveness, says Dr Soheil Radfar, a hurricane-hazard modeller at Princeton University. Radfar, who is the lead author of the new study, tells Carbon Brief:
“Hurricane damage starts days before the landfall…Four or five days before a hurricane making landfall, we expect to have high wind speeds and, because of that high wind speed, we expect to have storm surges that impact coastal communities.”
They also find that rapidly intensifying storms have higher peak rainfall than non-rapidly intensifying storms, with marine heatwave-influenced, rapidly intensifying storms exhibiting the highest average rainfall at landfall.
The charts below show the mean sustained wind speed in knots (top) and the mean rainfall in millimetres per hour (bottom) for the tropical cyclones analysed in the study in the five days leading up to and two days following a storm making landfall.
The four lines show storms that: rapidly intensified with the influence of marine heatwaves (red); those that rapidly intensified without marine heatwaves (purple); those that experienced marine heatwaves, but did not rapidly intensify (orange); and those that neither rapidly intensified nor experienced a marine heatwave (blue).
Dr Daneeja Mawren, an ocean and climate consultant at the Mauritius-based Mascarene Environmental Consulting who was not involved in the study, tells Carbon Brief that the new study “helps clarify how marine heatwaves amplify storm characteristics”, such as stronger winds and heavier rainfall. She notes that this “has not been done on a global scale before”.
However, Mawren adds that other factors not considered in the analysis can “make a huge difference” in the rapid intensification of tropical cyclones, including subsurface marine heatwaves and eddies – circular, spinning ocean currents that can trap warm water.
Dr Jonathan Lin, an atmospheric scientist at Cornell University who was also not involved in the study, tells Carbon Brief that, while the intensification found by the study “makes physical sense”, it is inherently limited by the relatively small number of storms that occur. He adds:
“There’s not that many storms, to tease out the physical mechanisms and observational data. So being able to reproduce this kind of work in a physical model would be really important.”
Economic costs
Storm intensity is not the only factor that determines how destructive a given cyclone can be – the economic damages also depend strongly on the population density and the amount of infrastructure development where a storm hits. The study explains:
“A high storm surge in a sparsely populated area may cause less economic damage than a smaller surge in a densely populated, economically important region.”
To account for the differences in development, the researchers use a type of data called “built-up volume”, from the Global Human Settlement Layer. Built-up volume is a quantity derived from satellite data and other high-resolution imagery that combines measurements of building area and average building height in a given area. This can be used as a proxy for the level of development, the authors explain.
By comparing different cyclones that impacted areas with similar built-up volumes, the researchers can analyse how rapid intensification and marine heatwaves contribute to the overall economic damages of a storm.
They find that, even when controlling for levels of coastal development, storms that pass through a marine heatwave during their rapid intensification cause 93% higher economic damages than storms that do not.
They identify 71 marine heatwave-influenced storms that cause more than $1bn (inflation-adjusted across the dataset) in damages, compared to 45 storms that cause those levels of damage without the influence of marine heatwaves.
This quantification of the cyclones’ economic impact is one of the study’s most “important contributions”, says Mawren.
The authors also note that the continued development in coastal regions may increase the likelihood of tropical cyclone damages over time.
Towards forecasting
The study notes that the increased damages caused by marine heatwave-influenced tropical cyclones, along with the projected increases in marine heatwaves, means such storms “should be given greater consideration” in planning for future climate change.
For Radfar and Moftakhari, the new study emphasises the importance of understanding the interactions between extreme events, such as tropical cyclones and marine heatwaves.
Moftakhari notes that extreme events in the future are expected to become both more intense and more complex. This becomes a problem for climate resilience because “we basically design in the future based on what we’ve observed in the past”, he says. This may lead to underestimating potential hazards, he adds.
Mawren agrees, telling Carbon Brief that, in order to “fully capture the intensification potential”, future forecasts and risk assessments must account for marine heatwaves and other ocean phenomena, such as subsurface heat.
Lin adds that the actions needed to reduce storm damages “take on the order of decades to do right”. He tells Carbon Brief:
“All these [planning] decisions have to come by understanding the future uncertainty and so this research is a step forward in understanding how we can better refine our predictions of what might happen in the future.”
The post Marine heatwaves ‘nearly double’ the economic damage caused by tropical cyclones appeared first on Carbon Brief.
Marine heatwaves ‘nearly double’ the economic damage caused by tropical cyclones
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