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The Ocean Has Been Breaking Heat Records. Marine Life Is Paying the Price

Record ocean heat is already changing marine life, from declining sardines and coral reefs to shifts in fish populations. Here is what the warming means for ecosystems and people.

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Ocean waves under a dramatic sunset as global ocean temperatures reach record highs
A warming ocean is placing growing pressure on marine ecosystems, fisheries and coastal communities as global sea temperatures continue to reach record levels. Representational Image. Image credit: Ray Bilcliff/Pexels

In the waters around Jeju Island in South Korea, divers are watching coral colonies collapse. The soft corals around the island are showing a condition researchers call “slumping”. Instead of holding their usual shape, parts of the colonies are losing their structure as the water becomes warmer due to ocean warming and environmental stress increases. Researchers have found signs of deterioration across coral clusters, with some areas showing severe decline. The corals are important nurseries for other marine species, so their deterioration affects more than the organisms themselves.

The situation in Jeju is one small example of a much larger change taking place across the world’s oceans. For about 100 days this summer, global sea-surface temperatures outside the polar regions remained at record levels for the time of year. Climate Central‘s analysis of NOAA data found the record streak running from June 2 through September 10, 2026. The NOAA dataset reached 21.24°C on August 23.

Ocean warming and daily global sea surface temperature
Global daily sea-surface temperatures from 2023 to 2026 show how recent years have remained well above the range recorded from 1982–2022, with 2026 reaching the highest levels shown. Source: Climate Central, using NOAA OISSTv2.1 data.

Copernicus recorded a slightly different peak of 21.11°C because it uses another dataset and methodology. Its August average of 21.07°C was the highest August value in its record. The number itself is difficult to picture. Its consequences are easier to see.

Ocean Warming and Marine Animals

Consider the oil sardine, one of the most familiar fish along India’s coast. The species is particularly sensitive to changes in sea temperature. India’s Central Marine Fisheries Research Institute has warned that the El Niño-driven warming expected later this year could affect oil sardine availability in 2027. CMFRI says small pelagic fish such as oil sardines are among the species most vulnerable to marine heatwaves and ocean warming.

That makes the current global warming signal relevant to an Indian fishing household as well as to climate scientists. The same pattern is already visible elsewhere. Morocco’s sardine landings fell 46% in 2026. Warmer waters were identified as a major factor, along with overfishing, pollution and higher fuel costs. The decline contributed to an export ban on frozen sardines and shortages in European markets.

In Peru, the fishing sector fell 73% year on year in May. The country’s first anchovy fishing season produced only about 0.5 million tonnes, compared with 1.9 million tonnes a year earlier. Manufacturing connected to fishing fell 42%. The fish do not need to die for this to become an economic problem. If the water becomes uncomfortable for a species, it can move. A fishing fleet that has depended on finding that species in the same waters for generations may then have to travel farther, catch less or change what it fishes for.

A 2026 study examining more than 33,000 fish populations found that long-term ocean warming was associated with annual biomass declines of up to 19.8%. Marine heatwaves produced much sharper losses in some populations at the warmer edge of their range, reaching 43.4%.

Then There is the Coral That Cannot Move

This is where the damage becomes harder to reverse. Fish can follow cooler water. A coral reef cannot. When seawater remains too warm, corals expel the microscopic algae living inside their tissues. Those algae provide much of the coral’s energy and give it its colour. The result is coral bleaching. If the heat persists, the coral can die.

Ocean warming causing coral bleaching across a shallow coral reef
Ocean warming and prolonged marine heat stress can cause corals to bleach, putting reef ecosystems at greater risk of damage and mortality. Representational image. Image credit: Zir YU/Pexels

The Mesoamerican Reef has experienced this on a huge scale. Almost the entire reef was exposed to serious heat stress during 2023 and 2024. Around half of its corals were severely affected by bleaching. Between 2023 and 2025, the reef lost about half of its living coral, leaving live coral cover at only 17%.

That loss changes the habitat available to fish and other marine organisms. It also affects people who depend on reefs for fishing, tourism and protection from waves. The Mediterranean has seen another kind of biological upheaval. Repeated marine heatwaves have contributed to mass deaths of marine organisms, while coral populations in some areas have fallen sharply. The noble fan mussel, one of the Mediterranean’s largest shellfish, has been pushed close to extinction in recent years.

Some Animals Thrive: Hidden Trouble

Ocean warming does not kill everything equally. Some species benefit from warmer conditions or move into areas that were previously too cold for them. That can produce an unfamiliar mix of species and upset existing food chains.

British waters are already showing this shift. Warmer conditions have been associated with increasing numbers of warm-water species such as sunfish, sardines and anchovies, while cold-water species including cod have declined along parts of the southern coast. Octopus populations have increased in some areas, putting additional pressure on crab and lobster fisheries.

That is not necessarily a sign that the ecosystem is becoming healthier. An ecosystem works through relationships between species. Change one part and others can be affected. A new predator, a disappearing prey species or a fish moving into unfamiliar waters can alter what other animals eat and where they survive. A 2026 study of Western Mediterranean ecosystems found that marine heatwaves were associated with declines in commercially important fish and invertebrates, with catch reductions exceeding 10% in some areas.

The Smallest Organisms Matter

There is another change taking place much lower in the food chain. Phytoplankton are tiny organisms that use sunlight to produce energy in the ocean. They form the base of many marine food webs. When ocean temperatures and nutrient conditions change, their productivity can change as well.

ISRO’s Oceansat-3 observations found a marked decline in surface chlorophyll-a concentrations in the equatorial Pacific in June 2026, consistent with reduced marine productivity as El Niño developed. Chlorophyll-a is commonly used as an indicator of the amount of microscopic plant life in the water. ([The Indian Express][6])

That matters because the effects can move upward through the food chain. Less food for tiny organisms can mean less food for small fish. That can affect larger fish, seabirds and marine mammals. During past marine heatwaves, the consequences have been dramatic. The 2014–16 “Blob” in the northeast Pacific contributed to the starvation of thousands of sea lion pups and the deaths of about four million common murres, according to the factsheet.

The bird deaths were not simply a story about birds struggling with hot water. The heatwave altered the marine food web, making it harder for them to find enough suitable food.

The Ocean can Change What Happens on Land

This is where the story moves from marine biology into everyday life. Warm seawater can supply additional heat and moisture to weather systems. Marine heatwaves have been linked with stronger storms, extreme rainfall and heatwaves over land. One study cited in the factsheet found that 22% of continental heatwaves and 43% of coastal heatwaves began as marine heatwaves.

Storm Daniel, which killed nearly 6,000 people in 2023, was fuelled by unusually warm Mediterranean waters. Climate change made the storm 50 times more likely and increased its intensity by 50%, according to the attribution analysis cited in the factsheet. Cyclone Gabrielle, which struck New Zealand in 2023, formed over abnormally warm seas and caused NZ$14 billion in damage. Climate change increased the intensity of its rainfall.

The connection is not as simple as saying “warm ocean equals stronger storm”. Storms depend on several atmospheric and ocean conditions. But a warmer ocean changes the conditions available to those weather systems.

Warming is not a One-year Event

El Niño is contributing to the current heat. It explains part of the unusually high temperatures in 2026, particularly in the Pacific. The larger trend is much older. The ocean has absorbed about 93% of the excess heat trapped by the warming atmosphere. Around 104 zettajoules of energy have entered the ocean during the past decade. The rate of warming during the last 20 years has been more than twice that of the preceding 40 years.

That is why today’s “cool” La Niña years are still warmer than El Niño years from earlier decades. After the previous El Niño ended in May 2024, sea temperatures remained close to or above previous records through 2025 and early 2026. The ocean is essentially carrying the accumulated heat of a warming planet.

What 21.24°C Really Means

A global ocean temperature is an average. It does not mean every part of the sea is 21.24°C. Tropical waters are much warmer; polar waters are far colder. What matters is the departure from the conditions marine ecosystems have evolved around, and how long that departure lasts.

In July 2026, 37% of the world’s ocean was experiencing a marine heatwave, according to NOAA. That ranked second among all months since 1991. NOAA’s forecast also points to potentially even greater marine heatwave coverage during the northern-hemisphere winter of 2026–27. For a coral colony, that can mean bleaching. For a sardine, it can mean moving into different waters. For a fishing community, it can mean a smaller catch. For a seabird, it can mean less food. For a country dependent on fisheries, it can mean lost revenue.

And for people living on the coast, changes in the ocean can eventually arrive as a storm, a disrupted livelihood or a higher food bill. The most important number in the 2026 ocean record may therefore not be 21.24°C. It is the roughly 100 days that the ocean stayed at record warmth. Marine ecosystems can sometimes recover from a short shock. Repeated or prolonged heat gives them much less time to do so. That is what makes a hot ocean worth watching even for people who rarely see the sea.

EP Staff is the editorial team at EdPublica, an independent media organisation focused on science, education, environment and public policy. The team produces evidence-based news, features, explainers and analysis on issues that shape society and everyday life.

Climate

Climate Change, Overfishing and the Uncertain Future of Bangladesh’s Hilsa Fishermen

EDPUBLICA GROUND REPORT: Climate change, overfishing and pollution are putting Bangladesh’s Hilsa fishery under pressure, threatening catches and fishermen’s livelihoods.

Rafiqul Islam Montu

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Bangladesh Hilsa fishermen crisis
Fishermen head out to sea in search of Hilsa, but many return with little or no catch as Bangladesh’s fishery comes under growing pressure. Photo by Rafiqul Islam Montu.

An EdPublica ground report from Bangladesh examines why the Hilsa catch has fallen after nearly two decades of growth, and what climate change and human pressures mean for the fishermen who depend on the fish.

DHALCHAR, Bhola, Bangladesh–At the fish landing centre, boats still come in one after another, and the crowd of fishermen on the shore grows with each arrival. But Ruhul Amin has stopped counting on what they carry.

“I can no longer support my family by catching Hilsa. I have been carrying the burden of debt for years. I wait for the Hilsa season every year with high hopes, but time and again, those hopes are dashed. There is no sign of Hilsa this year either, so I have to return home facing a loss.”

Ruhul Amin, 45, spoke these words amid the clamour of the fish landing centre on Dhalchar Island, situated along the banks of the Meghna River, one of the three principal rivers that form the vast Ganges Delta. Several other fishermen echoed his sentiments.

Hilsa Fishery Bangladesh
Fishing trawlers head out to sea to catch Hilsa at great expense, but many return to the dock empty-handed or with only a meagre catch. Photo by Rafiqul Islam Montu.

Dhalchar Island, located in the Meghna estuary, lies 100 kilometres from the Bhola district headquarters and 347 kilometres from the capital, Dhaka. Waves from the Meghna River crash against the island’s fish landing centre. The morning sun has just risen. Seagulls fly in flocks alongside the river waves. Boats dock one after another at the landing centre, and the crowd of fishermen grows. Yet, most of the boats arriving at the dock carry no Hilsa.

The area is bustling with activity—tea stalls, eateries, boat repair shops, and other establishments are crowded. However, there is a scarcity of the very fish—Hilsa—around which this landing centre was built. The fragile Dhalchar landing centre is shrinking due to river erosion, yet it remains a lifeline for the fishermen. Dhalchar Island remains quiet for most of the year but comes alive during the Hilsa season. Every year, thousands of fishermen gather here, filled with hope. It is not just Dhalchar Island; numerous fish landing centres along the coast of Bangladesh inspire similar hope among fishermen. About one million fishermen earn their livelihoods by catching Hilsa at these centres. Yet, they can no longer rely on Hilsa for their sustenance.

Ruhul Amin is one of those million fishermen. Amidst this despair and financial loss, the four-month-long Hilsa season is set to conclude on 7 October. The government has banned the catching, storing, transporting, and marketing of Hilsa for 22 days—from 8 October to 29 October—during the fish’s breeding season. Fishermen will once again have to wait until the following year for the Hilsa season.

“Fishing no longer sustains a livelihood”

Amidst the bustle and noise of the Dhalchar fish landing centre, Ruhul Amin voiced his frustration: “Every year, I’m forced to take out loans to go fishing with my boat and nets. I cast my nets during the Hilsa season with high hopes, but the catch is so meagre that it doesn’t even cover the operating costs. How am I supposed to repay the loans? How will I support my family? I may have to abandon this ancestral fishing profession; I can no longer bear the burden of debt.”

Bangladesh’s Hilsa Catch Is Falling After Two Decades of Growth

Even as the Hilsa season draws to a close, Ruhul Amin and many other fishermen have failed to recover their fishing expenses; they are ending the season at a loss. After nearly two decades of steady growth in Hilsa production in Bangladesh, the catch has fallen in each of the past three years. Simultaneously, the average weight of the fish is decreasing—a trend that has raised concerns among researchers.

IMAGE 2
The Hilsa season is a time of intense activity for fishermen, involving various preparations with nets and trawlers—all driven by the hope of a good catch. Photo by Rafiqul Islam Montu.

“Same nets, same boats, same rivers. Yet, the spots where we used to catch Hilsa in the past no longer yield any fish,” said Abdur Rob and several other fishermen from Kuakata on the Bangladeshi coast. They explained that as times change, they are encountering new crises while fishing at sea. Fishermen across most coastal districts—including Barguna, Patuakhali, Bhola, Bagerhat, and Lakshmipur—are grappling with professional crises. Climate change has impacted their lives and livelihoods, while natural disasters create obstacles to their fishing activities. Another group of fishermen believes that, beyond natural disasters, government-imposed seasonal fishing bans and various human-induced factors are hindering their profession.

According to records from the Bangladesh Department of Fisheries, the volume of Hilsa catch in Bangladesh began to rise in the 2016–17 fiscal year. That year, 496,000 tonnes of Hilsa were harvested within Bangladesh’s waters. In the 2017–18 fiscal year, the catch rose to 517,000 tonnes. The upward trend continued steadily until the 2022–23 fiscal year, when the harvest reached 571,000 tonnes. However, in the following year—2023–24—the catch volume suddenly dropped to 529,000 tonnes. It declined further to 500,000 tonnes in the 2024–25 fiscal year. Sources indicate that the Hilsa catch during July and August of the current year has fallen by 30–40% compared to the previous year.

Hilsa Bangladesh
Illustration: EdPublica

According to data from WorldFish and the Department of Fisheries, Bangladesh accounts for roughly 70–86% of the world’s Hilsa catch. India lands about 10–15%, mainly in West Bengal, Odisha, and Gujarat, and Myanmar about 3–10%. The remainder is caught in the coastal rivers and seas of Pakistan, Iran, Iraq, Kuwait, Bahrain, Thailand, Malaysia, and Indonesia.

Since 2019, Bangladesh has exported Hilsa to India, particularly during Durga Puja and other occasions; this practice continued until last year. However, this year, the situation reversed, with India exporting Hilsa to Bangladesh.

Bangladesh Hilsa Catch Is Falling After Two Decades of Growth
Fishermen are delighted when they find even a few Hilsa in their trawlers upon returning from the sea. Photo by Rafiqul Islam Montu.

Climate change has created crises in various marine sectors, including the Hilsa fishery. As catch volumes decline, fishermen are facing new challenges. Scientists fear that marine risks will escalate in the future. A study titled “Climate Change as Observed in the Bay of Bengal” highlights the dangers posed to the marine environment by climate change. Another study by the World Bank also addresses the impact of climate change on fishermen at sea.

Visualisation: EdPublica

Hilsa Is Losing Its Favourable Habitat

Fishermen observe that coastal temperatures, rainfall patterns, and the nature of the monsoon season have all shifted. The timing of freshwater influx into rivers and coastal salinity levels are changing, as are marine environmental conditions. Collectively, these changes influence the migration and breeding cycles of the Hilsa fish. A specific combination of factors—including water temperature, salinity, currents, tides, water density, oxygen levels, and rainfall—is required to create the right conditions for Hilsa migration and spawning. However, the environment essential for the Hilsa has been significantly degraded.

Hilsa experts largely concur with these observations made by fishermen. Anisur Rahman, former Director of the Bangladesh Fisheries Research Institute (BFRI), states, “Hilsa require specific water currents and depths to migrate into inland waters. They need a water depth of at least 10 metres to navigate the rivers, but they are not finding it.”

In some areas, river depth has dropped to just 18–20 feet (about 5.5–6 metres)—far below the 75–80 feet (about 23–24 metres) required for Hilsa breeding. Furthermore, submerged shoals and sandbars have obstructed waterways between Chandpur and Monpura, leaving only narrow channels for navigation. Hilsa migrate from the sea to inland waters by swimming against the current; however, reduced river navigability and diminished water flow are hindering this migration. Hilsa from the Padma River are renowned for their superior taste, yet the fish are no longer entering the Padma in significant numbers.

a small number of Hilsa get caught in their nets
Fishermen venture out to sea at great cost, yet only a small number of Hilsa get caught in their nets. Photo by Rafiqul Islam Montu.

Hilsa production in Bangladesh—which had been steadily rising for two decades—is now declining. This has raised concerns regarding the survival of this popular fish and its affordability for ordinary people. Anisur Rahman has been conducting research on Hilsa for a long time. Expressing concern over the decline in Hilsa catches, he said, “I’m truly worried about the population or stock of Hilsa.”

“The fish’s food chain is being disrupted by falling water levels, rising temperatures, and changes in water quality. This balance is further destabilized by excessive heat and altered rainfall patterns caused by climate change,” added Anisur Rahman.

Dr Md Sajedul Haque, a professor in the Department of Fisheries Technology at Patuakhali Science and Technology University (PSTU), observed, “Hilsa catches used to be higher; now they are lower. This is a global problem. It is happening due to global warming.”

“If Hilsa does not find a suitable environment, it will neither stay there nor spawn. Factors such as water salinity, the availability of plankton for food, and water temperature are crucial for Hilsa. If salinity is too high, they will not spawn, or the eggs will fail to hatch and perish. Without food, they will not grow. If the temperature is not optimal, the eggs will not be fertilized, and the fry will not hatch. The Hilsa’s life cycle is directly linked to these factors,” added Sajedul Haque.

To a fisherman, climate change is not a PowerPoint presentation; it is a harsh reality and a matter of life and death.

Human-Induced Factors

Alongside climate change, human-induced factors are jeopardising the breeding of Hilsa fish. Local fishermen, trawler owners, and wholesalers engage in unregulated and illegal fishing practices. The number of illegal trawlers in the sea has multiplied significantly. Trawlers are essentially large wooden boats powered by high-capacity engines. They operate by dragging illegal ‘Behundi’ nets (bag nets) through the sea for hours using this engine power. These nets catch not only large fish but also small fish fry and juvenile Hilsa (Jatka), thereby destroying the primary breeding grounds of Hilsa and other marine species.

Three power plants are located within Hilsa sanctuaries along the Bangladeshi coast—the Payra Power Plant, the Patuakhali Power Plant on the banks of the Ramnabad Channel, and the Barishal Power Plant at Taltali on the banks of the Bishkhali River. Many have expressed concern regarding the pollution caused by these facilities. These coal-fired power plants discharge waste and heated water into the rivers. A decline in Hilsa populations has been observed since the establishment of these plants. Fishermen are no longer catching Hilsa in the Ramnabad River (Patuakhali district) and the Payra River (Barguna district) as they used to; consequently, many are turning to other professions.

The hilsa crisis
Most fishermen’s fish baskets are lying empty. Photo by Rafiqul Islam Montu.

Fishermen Face Growing Risks at Sea

Fishermen report that while Hilsa exists in the deep sea, the fish are not migrating to shallower waters, as the environment there is no longer suitable for their survival. Small-scale fishermen face a dire crisis because the Hilsa do not venture into shallow waters, and many have already abandoned the trade. Those who remain in the profession are forced to venture into the deep sea to catch Hilsa, where they face increasing risks.

Every year, many fishermen go missing due to various natural hazards. The sea is becoming more turbulent than in the past, and the level of danger is rising. Nuruddin, a fisherman from Char Fasson in Bhola district, says, “I have been going out to sea to fish since childhood. I used to have no fear, but now venturing out to sea is frightening for us. I cannot say for certain if it is due to climate change, but the waves are rougher than before. We often face accidents because we do not receive weather warnings in time. I have personally been involved in accidents a few times; fortunately, I survived and returned.”

A study titled “Resilient Bangladesh: Fishermen Cope with Rough Seas” notes that for centuries, the fishermen’s traditional boats were sturdy enough to withstand conditions in the Bay of Bengal. That is no longer the case. Fishermen are increasingly facing more powerful storms and turbulent seas. Every time they head out to fish, they are essentially gambling with their lives.

Even as the risks for fishermen rise, fish stocks in the sea are declining, impacting their livelihoods. Despite this crisis, fishermen continue to struggle for survival. Research titled “Dwindling Coastal Fisheries Biodiversity of Bangladesh: The Causes and Effects” indicates that coastal fish stocks are being overexploited, leading to a depletion of many species. The marine sector’s contribution to the country’s fisheries is shrinking annually. According to assessments by the IUCN (International Union for Conservation of Nature), approximately 28% of coastal fish species now fall under the IUCN Red List of threatened species.

Golam Mostafa Chowdhury, President of the Barguna District Trawler Owners’ Association, states, “In most cases, fishermen go missing when their trawlers capsize. The sea has become rougher than before, and weather conditions have deteriorated. Siltation has occurred in many areas, and many fishermen fail to receive proper weather warnings. These factors are contributing to a rise in the number of missing fishermen. Rescue vessels need to be stationed in areas with high concentrations of fishermen, and arrangements must be made for the rehabilitation of those who go missing.”

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Traders invest heavily to catch Hilsa, but their crates at the wholesale market remain empty. Photo by Rafiqul Islam Montu.

Initiatives to Protect Hilsa

The government is taking various measures to protect the Hilsa fish. Conservation and management activities for Hilsa in Bangladesh are conducted under the Protection and Conservation of Fish Act, 1985. A programme to protect Jatka (juvenile Hilsa) was launched in Bangladesh in 2003–04, leading to a gradual increase in Hilsa production. The Jatka conservation drive runs for two months—March and April—during which fishing of all kinds, including Hilsa, is prohibited in designated sanctuaries across the country. Additionally, fishing for all species, including Hilsa, is banned in marine waters for 58 days, from 15 April to 11 June. Initially, in 2008, the ban on catching mother Hilsa (Ma Hilsh) was set for 11 days, but from the following year onwards, this period was extended to 22 days. A ban on catching mother Hilsa is in effect from 8 October to 29 October this year. For two decades, the trend of Hilsa harvesting had been on the rise; however, research is currently underway to understand why the catch rate has recently begun to decline.

chart3 ban calendar
Visualisation: EdPublica

Ruhul Amin, a fisherman, is spending the final days of the Hilsa season at the Dhalchar fish landing centre. He might venture out to sea a few more times with other fishermen to catch Hilsa. Yet, amidst the crowds and grueling labor, a question weighs on his mind: will he be able to take home enough earnings to support his family for the coming months? Ruhul Amin does not know the answer—nor do many other fishermen.

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A teenage fisherman is overjoyed to hold two Hilsa fish, yet he worries about whether he will be able to bring home any earnings. Photo by Rafiqul Islam Montu

For the fishermen of Bangladesh, the Hilsa season is drawing to a close amidst a period of uncertainty. The voices of the crowd at the fish landing centre fade into the air, carrying with them the indistinct sounds of the fishermen’s suffering.

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COP30

Pacific Nations Push 1.5°C and Climate Finance Ahead of COP31

Pacific nations are using Pre-COP31 talks in Fiji to push for stronger action on climate change, including keeping the 1.5°C target within reach and improving access to climate finance.

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A black climate protest sign reading “ONE WORLD” with a hand-painted illustration of Earth, symbolising global cooperation on climate change ahead of COP31.
A “One World” sign symbolising the global cooperation.Representative image. Image Credit: Pexels

Pacific island nations are seeking to put their climate concerns at the centre of global negotiations as ministers, climate negotiators and senior officials gather in Fiji for preparatory talks ahead of the COP31 climate summit.

The Pre-COP meeting, scheduled in Nadi from October 5 to 8, is intended to build momentum for the United Nations climate conference in Antalya, Türkiye, in November. COP31 will be held from November 9 to 20.

For Pacific countries, however, the meeting is more than a diplomatic step towards the main summit. It is an opportunity to press the world’s major economies on issues that directly affect the region, particularly the 1.5°C warming limit, climate finance and the growing impact of climate change on oceans and coastal communities.

Fiji has outlined four priorities for the Pre-COP discussions: keeping the 1.5°C target within reach, improving access to climate finance, placing oceans more prominently in climate negotiations and strengthening Pacific leadership.

The 1.5°C target is particularly important for small island nations facing rising seas, coastal erosion, extreme weather and growing pressure on communities and infrastructure.

Fiji’s climate officials have said the country wants to maintain the role of climate science in international decision-making and “hold the line” on 1.5°C. The country is also calling for climate finance to reach vulnerable communities more quickly, arguing that lengthy funding procedures can leave communities waiting for resources while climate risks continue to increase.

Access to finance is expected to be one of the key issues carried from the Pacific discussions into COP31. Pacific governments are seeking greater support for adaptation and resilience, including through a proposed Pacific Resilience Facility that would finance climate projects across the region.

The region is also seeking to bring oceans more firmly into the climate agenda. For Pacific island states, climate change is closely connected to the health of marine ecosystems, coastal communities, fisheries and food security.

The preparatory talks will therefore bring together two aspects of the climate debate: the global effort to limit further warming and the immediate need to protect communities already experiencing its effects.

The setting is significant. Leaders and delegates will also spend time in Tuvalu, a low-lying Pacific island nation particularly exposed to sea-level rise. The programme includes visits to adaptation projects, including reclaimed land and solar installations, allowing visiting leaders to see some of the measures being used by island states to respond to climate risks.

But the meeting comes with a diplomatic challenge. Reuters reported that relatively few leaders from outside the Pacific have confirmed their participation. Leaders from Antigua and Barbuda, Cabo Verde, Thailand, the Maldives and Timor-Leste are among those confirmed, while around 30 representatives of countries and institutions are expected at the leaders’ segment.

pexels ron lach 9035234

A placard displaying ‘Save the Earth’.Representational image.Image Credit:Pexels

The limited participation has drawn criticism from some Pacific officials, who argue that the region’s climate concerns deserve greater international attention. At the same time, the meeting is expected to bring thousands of delegates to Fiji, giving Pacific governments a platform to shape discussions before the main negotiations in Türkiye.

For the Pacific, the focus in Nadi will therefore be on translating regional concerns into negotiating priorities for COP31 — from keeping the 1.5°C goal central to improving access to climate finance and strengthening attention to oceans and adaptation.

The outcome of the Fiji discussions will feed into negotiations at COP31, where governments will have to work through the wider questions of climate ambition, finance and implementation.

For island nations on the frontline of climate change, the immediate priority is to ensure that their experience and demands are reflected proportionately in those negotiations.

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Climate

Europe Crops Are Maturing Earlier. Does That mean Bigger Harvest?

Europe’s crops are maturing earlier as rising temperatures accelerate plant development, but earlier maturity does not necessarily mean bigger harvests. Heat and drought can shorten critical growth stages and reduce crop yields.

Jishnu P

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Wheat harvest being collected by a combine harvester in a European field
A combine harvester collects wheat during the harvest season in Europe. Image Credit:Pexels

Europe’s crops are reaching maturity earlier as extreme heat accelerates plant development. But the 2026 harvest shows why an earlier harvest should not be mistaken for a bigger one: heat can shorten the grain-filling period, reduce yields and leave crops with fewer and smaller grains.

A wheat field turning golden weeks earlier than it once did might appear to signal a productive growing season. But across Europe, the earlier agricultural calendar is increasingly coming with a less reassuring reality.

Winter wheat in some European Union regions is now reaching maturity up to 20 days earlier than in 2000, according to European Commission data reported by Reuters. Maize and rapeseed are also developing and reaching harvest stages earlier as rising temperatures accelerate the accumulation of heat needed for crops to progress through their life cycles.

But an earlier maturity date is not the same thing as a higher yield.

In fact, Europe’s 2026 growing season demonstrates the opposite can happen.

The European Commission’s Joint Research Centre (JRC) said in September that prolonged heat accelerated crop development and ageing, causing plants to move more quickly through critical stages including flowering and grain filling. At the same time, rainfall deficits depleted soil moisture. The combination left crops with less time and fewer resources to form well-developed grains, tubers and cobs. In the worst-affected areas, maize reached maturity as much as three weeks earlier than usual.

For wheat, one of the most important stages after flowering is grain filling. This is when the developing grain accumulates the carbohydrates and other resources that determine its eventual size and weight. If high temperatures accelerate the plant’s development, the time available for grain filling can be reduced.

The JRC’s July assessment explicitly found that repeated heatwaves had shortened the grain-filling phase of winter crops and brought harvests forward. Its winter-crop yield forecasts were consequently revised down by 1–4%, leaving the overall cereal outlook about 1% below the five-year average.

The September assessment showed how much more severe the situation became for crops whose critical development occurred during the summer.

EU forecasts put soybean yields 15% below the 2021–25 average, fresh maize 14% below, sugar beet 11% below, grain maize 8% below and potatoes 7% below. The JRC also warned that production losses could exceed yield losses because some severely damaged fields were no longer economically viable to harvest.

The 2026 grain forecast tells the same story

An analysis by the Energy and Climate Intelligence Unit (ECIU), based on COCERAL’s crop forecasts, provides another measure of the damage.

COCERAL’s September forecast put combined EU-27 and UK grain production at 278.9 million tonnes, down from 295.5 million tonnes in its June forecast. The 16.7-million-tonne downgrade between June and September came after an earlier nine-million-tonne reduction between the June and July forecasts.

The ECIU analysis estimates that the September forecast was 9.3% below 2025 levels, making it the smallest grain harvest in at least a decade. It estimates the current value of the lost production at about €3.2 billion.

Of the 16.7 million tonnes lost between the June and September forecasts, 11.1 million tonnes resulted from lower yield forecasts, while 5.6 million tonnes came from changes in crop-area estimates.

That makes yield the central part of the story.

Heat did not simply make European crops mature earlier. It reduced how much harvest many plants could produce before they reached maturity.

Wheat was hit during grain filling

The ECIU analysis, drawing on COCERAL’s assessment, identifies different vulnerable stages for different crops.

Wheat was hit during grain filling, when moisture is particularly important for grains to develop properly. Maize, meanwhile, was particularly vulnerable during pollination.

This helps explain why simply measuring the date of maturity can be misleading.

A plant may reach physiological maturity sooner because accumulated heat has pushed it through its developmental stages. But if extreme heat and water stress occurred during grain filling, the plant may reach that endpoint with less grain mass than it would have produced under more moderate conditions.

The JRC observed the same mechanism across crops in 2026: accelerated development combined with limited water meant less time and fewer resources for crops to form well-developed grains, tubers and cobs.

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Wheat field.Image credit:Pexels

The losses were uneven across Europe

The ECIU analysis shows just how differently countries were affected.

France recorded the largest downward revision, with grain production cut by 5.8 million tonnes, representing an estimated €1.47 billion in lost production value. Hungary’s forecast fell by 3.2 million tonnes, the UK’s by 3 million tonnes and Germany’s by 2.5 million tonnes.

France’s maize crop was particularly affected. COCERAL’s September estimate put production at 7.6 million tonnes, 45% below 2025.

In the UK, the wheat yield forecast was cut from 7.95 tonnes per hectare to 6.82 tonnes per hectare. Austria’s maize yield fell from 11.4 tonnes per hectare in 2025 to 7.2 tonnes per hectare.

The contrast is therefore stark: some crops were ready for harvest earlier, but the amount harvested per hectare was falling.

Why 2026 became so damaging

The JRC says the summer began from relatively favourable conditions before a combination of exceptional heat and rainfall deficits changed the outlook rapidly.

Large areas of Spain, France and Italy experienced more than 15 additional days above 35°C compared with a typical summer, with elevated heat exposure also affecting Greece and Croatia.

Earlier in the summer, the JRC’s drought monitoring showed that 50% of EU and UK territory was under some level of drought condition by late July, with 9% at alert level. The drought combined low rainfall, depleted soil moisture and vegetation stress.

Winter crops had largely completed their development before the most severe summer heat arrived, which helped keep their yields closer to the recent average. Summer crops were still developing when the heat and drought intensified and were consequently more exposed.

A changing agricultural calendar

The shift towards earlier maturity is therefore not meaningless. It is an important indicator of how warming temperatures are changing Europe’s agricultural calendar.

Earlier maturity may sometimes allow a crop to escape a later heatwave or drought. The problem arises when accelerated development happens because of intense heat during a period when the plant still needs time, water and moderate temperatures to build yield.

The 2026 data show this distinction clearly.

The European Commission’s July assessment already reported that heatwaves had shortened the grain-filling period of winter crops. By September, its models showed summer crops reaching maturity earlier while yields remained substantially below the five-year average.

The result is a paradox that will become increasingly important as temperatures rise: a crop can be harvested earlier and still produce less food.

The warning signal

The 2026 European heatwave attribution study reported that the 2026 temperatures would have been virtually impossible in the 1976 climate. The comparable daytime heat would have been around 10 times less likely in 2003, while comparable nighttime temperatures would have been more than 100 times less likely. A comparable June 2026 heatwave would also have been about 3.5°C cooler during the day in the 1976 climate.

That study should not be used to attribute the 2026 agricultural losses directly. But it provides important context for the wider trend: extreme heat is becoming a more important agricultural risk as the climate warms.

The 2026 European harvest shows what that risk can look like on the ground.

The question for agriculture is therefore no longer simply “When will the crop mature?”

It is also “How much yield can the plant build before it gets there?”

For wheat, maize and other crops, that difference could determine whether a warmer growing season produces an earlier harvest or simply an earlier end to a season that has failed to produce enough food.

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