The extreme rainfall that hit Afghanistan, Pakistan and Iran in April and May this year was made twice as likely by El Niño, a new rapid attribution study shows.
The World Weather Attribution service finds that spring rainfall over the region has become 25% heavier over the past 40 years.
As climate models were unable to reproduce this trend, the authors were unable to assess the impact of rising global temperatures on the event. However, a study author tells Carbon Brief that she “would be extremely surprised if climate change is not at least part of this trend”..
In contrast, the authors were able to identify the influence of the strong El Niño event that has been underway in the Pacific Ocean since the autumn of 2023.
They find that such heavy rainfall would be expected once every 20 years in the absence of El Niño, but this frequency rises to once every 10 years when an event occurs.
Flash flooding
In the spring of 2024, a series of unseasonably early spring storms swept across large parts of central Asia, causing severe flooding which destroyed homes and crops, and killed thousands of people.
In Pakistan, the first spell of intense rainfall began on 12 April. The resulting flooding damaged more than 450 schools and 5,000 houses, and killed more than 100 people. Subsequent periods of heavy rainfall across the country caused further damage to buildings and crops, destroying huge fields of wheat that were ready for harvest.
The flooding “has resulted in significant economic losses for local farmers and communities, compounding the losses from the rain-related incidents”, the UN Office for the Coordination of Humanitarian Affairs warned.
Afghanistan also suffered a series of deadly floods. After a dry winter, which made the soil less able to absorb rainfall, the country was hit by waves of intense rainfall throughout much of April and May,
About 70 people were killed in April after flash floods destroyed about 2,000 homes, three mosques and four schools. On 10 May, another period of intense rainfall hit the country – especially in the north-east, resulting in hundreds of fatalities and many more missing people. Around 9,100 livestock and 20,800 acres of agricultural land were destroyed.
Five days later, the International Federation of Red Cross and Red Crescent Societies warned that 25 out of 34 provinces in Afghanistan had been affected by flooding, adding that “thousands of displaced people have no homes to return to after their houses were swept away”. The organisation also warned:
“This latest disaster is happening within the context of what is already one of the world’s worst humanitarian crises, where communities are already barely able to cope.”
Meanwhile, the Guardian reported that “in a country with a health system already on its knees, some health facilities were rendered non-operational last week by the flooding”.
Similarly, intense rainfall and flooding killed multiple people in Iran. The
Iran International Newsroom blamed “government mismanagement and flawed urban planning” for “exacerbating” the intense rainfall.
The study authors decided to focus on April-May rainfall in a region centred on Afghanistan, bounded by Iran on the west and Pakistan on the east.
The map below shows the difference in April-May total rainfall between 2024 and the 1991-2020 average, where blue indicates that 2024 saw heavier than average rainfall, and red indicates lighter than average rainfall. The region analysed in this study – covering parts of Afghanistan, Pakistan and Iran – is outlined in red.

The region’s main winter rainfall season runs from November to early April, meaning that this year’s intense rainfall was unusually early, the study says.
Attribution
The spring flooding over Afghanistan, Pakistan and Iran was “incredibly deadly”, according to the. To determine how likely this period of intense rainfall was, the authors analysed a timeseries of observed rainfall data to put the event into its historical context.
The graph below shows April-May rainfall from 1950 to the present day over the study region. The blue and orange lines indicate different datasets.

The observational data shows that April-May rainfall in the region has become, on average, 25% heavier over the past 40 years.
The authors conducted an attribution study to identify the “fingerprint” of climate change on the extreme rainfall trend. They used models to compare the world as it is today – which has already warmed by around 1.2C because of human activity – to a “counterfactual” world without climate change.
However, the climate models used in this analysis did not consistently reproduce the trends shown by observed data.
“We can’t formally attribute it because the models don’t reproduce these trends,” Dr Friederike Otto – senior lecturer in climate science at the Grantham Institute for Climate Change and the Environment at Imperial College London and co-author of the study – told Carbon Brief at a press briefing.
However, Otto – who is also a Carbon Brief contributing editor – explained that climate change is known to make individual storms more intense. “So I would be extremely surprised if climate change is not at least part of this trend,” she added.
The authors also investigate the impact of El Niño – a global weather phenomenon that originates in the Pacific Ocean – on rainfall in the region. The world has been experiencing El Niño conditions since around October 2023 and is now showing signs of ending.
Dr Mariam Zachariah, who is also study author from the Grantham Institute, told Carbon Brief that El Niño leads to warmer sea surface temperatures over the western Indian ocean, which are a “known driver” of extreme rainfall over the study region.
Using a series of statistical models, the authors determined that an El Niño during the winter (December-February) often leads to an increase in rainfall over the study period during April and May.
The 2024 spring rainfall over Afghanistan, Pakistan and Iran was not “particularly rare” in today’s climate, and could be expected to occur roughly once every 10 years if only El Niño years are considered, the authors find.
Under “neutral” conditions in the Pacific Ocean, similar periods of heavy rainfall are expected roughly once every 20 years, they add.
They conclude that El Niño doubled the likelihood of the extreme rainfall that hit Afghanistan, Pakistan and Iran in spring 2024.
(These findings are yet to be published in a peer-reviewed journal. However, the methods used in the analysis have been published in previous attribution studies.)
Vulnerability
Afghanistan ranks fourth on the list of countries most at risk of a crisis, and eighth on the Notre Dame Global Adaptation Initiative index of countries most vulnerable and least prepared to adapt to climate change.
However, the country has been absent from COP climate summits since the Taliban took over in 2021. No foreign government has formally recognised Taliban leadership and it does not have a seat at the UN General Assembly.
The Taliban’s takeover has impacted Afghanistan’s access to climate finance. The country’s climate plan estimates it needs $20.6bn over 2021-30. But around 32 large environmental programmes worth more than $800m were suspended when the Taliban took over, including a major rural solar installation project backed by the Green Climate Fund.
Nevertheless, the country is still receiving some climate finance. A recent freedom-of-information request by Carbon Brief shows that the UK government has opted to meet their £11.6bn climate finance target by “redirecting” or “relabelling” existing funds as “climate finance”, while failing to commit new money in sufficient volumes.
This includes reclassifying nearly £500m of aid for war-torn and impoverished countries, including Afghanistan, as “climate finance”.
And, in late April this year, the Taliban initiated its first discussions with the UN, donors and non-governmental organisations about the implications of climate change in Afghanistan, as confirmed by organisers.
However, in the meantime, Afghanistan remains highly vulnerable to the impacts of climate change.
The authors say that many residents of Afghanistan – as well as Pakistan and Iran – are “highly vulnerable” to flash flooding, as many of them live on river basins that are highly vulnerable to flash floods.
Maja Vahlberg – a climate risk consultant from the Red Cross Red Crescent Climate Centre and author on the study – told Carbon Brief that “marginalised communities” were among the most severely impacted by the flooding.
The study adds that “displaced populations were particularly impacted, especially as limited essential infrastructure was destroyed and already vulnerable populations were exposed to more waterborne diseases”.
Vahlberg told Carbon Brief that, across the region, there is “limited” data sharing and flood risk management, meaning that flood early warning systems are “significantly less efficient” than they could be.
The study concludes that there are “ample opportunities to improve climate adaptation and resilience”, including “increasing the coverage of early warning systems, and improving flood risk management policy and planning”.
The post Afghanistan’s ‘deadly’ early spring rainfall made twice as likely by El Niño appeared first on Carbon Brief.
Afghanistan’s ‘deadly’ early spring rainfall made twice as likely by El Niño
Climate Change
What Is the Economic Impact of Data Centers? It’s a Secret.
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.
Climate Change
GEF raises $3.9bn ahead of funding deadline, $1bn below previous budget
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”.
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.
Santa Marta conference: fossil fuel transition in an unstable world
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
Climate Change
Marine heatwaves ‘nearly double’ the economic damage caused by tropical cyclones
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
-
Climate Change8 months ago
Guest post: Why China is still building new coal – and when it might stop
-
Greenhouse Gases8 months ago
Guest post: Why China is still building new coal – and when it might stop
-
Greenhouse Gases2 years ago嘉宾来稿:满足中国增长的用电需求 光伏加储能“比新建煤电更实惠”
-
Climate Change2 years ago
Bill Discounting Climate Change in Florida’s Energy Policy Awaits DeSantis’ Approval
-
Climate Change2 years ago嘉宾来稿:满足中国增长的用电需求 光伏加储能“比新建煤电更实惠”
-
Climate Change Videos2 years ago
The toxic gas flares fuelling Nigeria’s climate change – BBC News
-
Renewable Energy6 months agoSending Progressive Philanthropist George Soros to Prison?
-
Carbon Footprint2 years agoUS SEC’s Climate Disclosure Rules Spur Renewed Interest in Carbon Credits










