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Fred Pearce is a freelance author and journalist writing on behalf of Wetlands International Europe.

Everybody knows that saving the Amazon rainforest is critical to our planet’s future. But the Pantanal? Most people have never heard of Brazil’s other ecological treasure, the world’s largest tropical wetland – let alone understood its importance, as home to the highest concentration of wildlife in the Americas, while keeping a billion tonnes of carbon out of the atmosphere, and protecting millions of people downstream from flooding.

Hundreds of millions of euros are spent every year on protecting and restoring the world’s forests. Wetlands are just as important, yet don’t get anything like the same recognition or investment. That, scientists insist, has to change. And Europe can lead the way.

For forests, the EU already provides financial and technical assistance for a series of Forest Partnerships with non-EU countries, as part of its Global Gateway strategy for investing globally in environmentally and socially sustainable infrastructure. Such partnerships operate in Guyana, the Democratic Republic of the Congo, Mongolia and elsewhere.

I believe the time is now right to establish a parallel EU Wetland Partnerships, framing wetlands as a strategic, cost-effective investment offering high financial, environmental and social returns.

Wetlands store a third of global soil carbon

Wetlands come in many shapes and sizes: freshwater peatlands, lakes and river floodplains, as well as coastal salt marshes, mangroves and seagrass beds. They are vital natural infrastructure, maintaining river flows that buffer against extreme weather events such as floods and drought, as well as protecting biodiversity, and providing jobs and economic opportunities, often for the most vulnerable nature-dependent communities.

Wetlands cover just six percent of the land surface, but store a third of global soil carbon – twice the amount in all the world’s forests. Yet they have been disappearing three times faster than forests, with 35 percent lost in the past half century.

A just agricultural transition takes root in Brazil

Their loss adds to climate change, causes species extinction, triggers mass exoduses of fishers and other people whose livelihoods disappear, and depletes both surface and underground water reserves. Continued wetlands destruction is estimated to contribute five percent of global CO2 emissions – more than aviation and shipping combined.

EU Wetland Partnerships can be critical to unlocking finance to stem the losses and realise the benefits by promoting nature-based economic development, such as sustainable aquaculture, eco-tourism, and forms of wetlands agriculture known as paludiculture, while contributing to climate adaptation by improving the resilience of water resources.

Pantanal faces multiple threats

The Pantanal would be a prime candidate for a flagship project. The vast seasonal floodplain stretching from Brazil into Paraguay and Bolivia, is home to abundant populations of cayman, capybaras, jaguars and more than 600 species of birds. It is vital also for preventing flooding on the River Paraguay for some 2000 kilometres downstream to the Atlantic Ocean.

The Pantanal faces multiple threats, from droughts due to upstream water diversions and climate change, invasions by farmers setting fires and a megaproject to dredge the river and create a shipping corridor through the wetland.

But EU investment to achieve partnership targets agreed with Brazil on restoration, conservation and sustainable management could reinvigorate traditional sustainable land use – including cattle ranching that helps sustain the Pantanal’s open flooded grasslands.

A delegation from the Pantanal Association for Organic and Sustainable Livestock Farming, pictured in the Pantanal wetland, Mato Grosso do Sul, Brazil. (Photo: Wetlands International Brazil office)

A delegation from the Pantanal Association for Organic and Sustainable Livestock Farming, pictured in the Pantanal wetland, Mato Grosso do Sul, Brazil. (Photo: Wetlands International Brazil office)

Accounting for wetlands carbon in national emissions targets

Africa, a main focus of the Global Gateway, has abundant potential for early partnership initiatives. They include the Inner Niger Delta in Mali, which sustains some three million inhabitants, but is threatened by upstream dams and conflicts over resources between farmers and herders.

Another is the Sango Bay-Minziro wetland, a region of swamp forests, flooded grasslands and papyrus swamp straddling the border between Uganda and Tanzania on the shores of Lake Victoria, Africa’s largest lake.

The two countries have agreed to cooperate in pushing back against illegal logging, papyrus extraction and farming, and Wetlands International has been working with local governments to encourage community-based initiatives. But an EU partnership could dramatically expand this work, helping sustain the wider ecology of Lake Victoria and the Nile Basin.

Deep in the Amazon, forest protection cash must vie with glitter of illegal gold

National pledges to bring wetlands to the fore of environmental action are proliferating rapidly, especially since the 2023 global climate stocktake at COP28 in the UAE emphasised the importance of accounting for wetlands carbon in national emissions targets.

Since then, more than 50 countries have signed up to the 2023 Freshwater Challenge to protect freshwater ecosystems; more than 40 governments with 40 percent of the world’s mangroves have endorsed the 2022 Mangrove Breakthrough that aims to protect and restore 15 million hectares by 2030; and the newly established Peatland Breakthrough aims at rewetting at least 30 million hectares and halting the loss of undrained peatland by 2030.

Such ambition will almost certainly be endorsed at the 2026 UN Water Conference to be hosted by the UAE and Senegal in December this year. But the key to turning targets into reality on the ground lies in finding the billions of Euros needed to deliver on the ambition. EU Wetlands Partnerships could help seal the deal.

The post The EU should partner with Global South to protect carbon-storing wetlands appeared first on Climate Home News.

The EU should partner with Global South to protect carbon-storing wetlands

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On the Historic Route From Selma to Montgomery, an AI Cloud Looms

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In this rural Alabama community, some residents can’t flush their toilets. Developers want to build a state-of-the-art data center next door.

HAYNEVILLE, Ala.—When Alabamians marched from Selma to Montgomery in 1965 to demand voting rights for African Americans, Highway 80 became their path toward freedom.

On the Historic Route From Selma to Montgomery, an AI Cloud Looms

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Guest post: How a record-high ‘energy imbalance’ is driving global warming

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The planet is heating up more quickly than ever before.

For decades, greenhouse gas emissions caused by human activity have been building up in the atmosphere and trapping ever-higher levels of heat.

The resulting asymmetry between incoming solar energy and energy radiated back out into space – known as “Earth’s energy imbalance” – provides a direct measure of the extent to which humans are disrupting the Earth’s climate system.

This imbalance is growing and in 2025 its 10-year average reached a record high, indicating that global temperatures could increase at even higher rates in the future.

This is among the headline findings of the latest “indicators of global climate change” (IGCC) report, published in the journal Earth System Science Data, which tracks changes in the climate system on an annual basis.

The report, now in its fourth iteration, has been produced by dozens of scientists from around the world.

Its findings are designed to fill the gap between Intergovernmental Panel on Climate Change (IPCC) science reports, which are published every 5-7 years.

In this article, we unpack the IGCC report, which explores how human activity is driving a growing energy imbalance and why monitoring systems to track global climate are so crucial.

(For more on previous IGCC reports, see Carbon Brief’s coverage in 2023, 2024 and 2025.)

Greenhouse gas emissions remain at an all-time high

Global greenhouse gas emissions are continuing to increase, mostly as a result of the use of fossil fuels. However, deforestation, agriculture and industrial processes also play an important role.

Glossary
CO2 equivalent: Greenhouse gases can be expressed in terms of carbon dioxide equivalent, or CO2e. For a given amount, different greenhouse gases trap different amounts of heat in the atmosphere, a quantity known as… Read More

Over the most recent decade (2015-24), emissions stood at the equivalent of 54.6bn tonnes of carbon dioxide equivalent (GtCO2e) per year. In 2024, the most recent year for which we have complete data, emissions reached 56.8GtCO2e.

As the chart below shows, these emissions have pushed up atmospheric levels of CO2, methane and nitrous oxide. In 2025, concentrations of these gases reached 425.6 parts per million (ppm), 1936.3 parts per billion (ppb) and 339.4ppb, respectively.

This represents a rise of 3.8%, 3.8% and 2.2%, respectively, since the 2019 levels reported in the IPCC’s sixth assessment report (AR6).

Atmospheric concentrations of CO2
Atmospheric concentrations of CO2 (yellow), methane (blue) and nitrous oxide (green) over 2000-25. The grey-shaded region represents continuing changes since AR6. Note the different vertical scales for each gas. Credit: Forster et al. (2026)

At the same time, declines in emissions of aerosols such as sulphur dioxide, partly as a result of efforts to tackle air pollution, are increasing the Earth’s energy imbalance. This is because aerosols have a cooling effect on the Earth’s climate, counteracting warming from CO2 and other greenhouse gas emissions.

(Tackling sulphur dioxide, alongside other particulate emissions, remains critical because the immediate health and environmental damage they cause far outweighs their short-term cooling effect on the climate.)

The Earth’s energy imbalance is rising rapidly

The Earth’s energy imbalance has long been recognised as a key indicator of how the climate is being affected by human activities.

However, it is only in the last few decades that scientists have been able to record temperature changes deep enough in the ocean to accurately quantify it.

Earth’s energy imbalance measures how quickly excess heat is accumulating in every part of the Earth system, primarily in the ocean, but also in land, ice and atmosphere.

Through this accumulation of heat, the energy imbalance influences the rate of sea level rise and ice melt across the world, as well as increasing the frequency and intensity of extreme weather events, such as storms, floods and droughts.

Without human influence, the Earth’s energy imbalance would be close to zero.

But, as greenhouse gas emissions have built up in the atmosphere, the imbalance has been growing since the 1970s. Recent increases to Earth’s energy imbalance have outpaced those projections made by climate models — indicating the planet could see more warming than expected in the future.

As the right-hand chart below shows, the imbalance is now at a record high, having more than doubled over the past two decades.

It has increased by around 40% since 2019, from an average 0.79 watts per square metre (Wm2) over 2006-18, according to IPCC AR6, to 1.12Wm2 over 2013-25.

The left-hand chart shows how heat is accumulating in the ocean (blues), ice (grey), land (orange) and atmosphere (purple).

 Observed changes in the Earth heat inventory
Left: Observed changes in the Earth heat inventory for the period 1971-2020. Right: Estimates of the Earth energy imbalance for successive overlapping 20-year periods and the most recent decade (right). Shaded regions indicate the very likely range (90-100 % probability), while the stars show the CERES (NASA Clouds and the Earth’s Radiant Energy System) estimates for comparison. Credit: Forster et al. (2026)

Global temperature rise

The excess heat building up in the climate system from the energy imbalance is pushing up global temperatures at a record rate of 0.27C per decade.

We estimate that human-induced warming – the amount of observed global surface

temperature increase attributable to both the direct and indirect effects of human activities – reached 1.37C in 2025. This has risen from 1.0C in 2017, as reported in IPCC AR6.

While natural variability in the climate system – such as El Niño or La Niña events – can also influence temperatures year-to-year, the upward temperature trend we are seeing is being driven by the persistent imbalance in energy.

We now expect global temperatures to exceed the Paris Agreement limit of 1.5C above pre-industrial levels around the year 2030.

This is significant because 1.5C has been identified as the critical dividing line between manageable climate risks and catastrophic, potentially irreversible damage to global ecosystems and human societies.

Heat accumulating throughout the Earth system

While heat is accumulating throughout the Earth system, it is not being distributed evenly around the globe.

Since the 1970s, around 90% of this heat has been taken up by the ocean, affecting marine ecosystems, ocean circulation patterns, sea level rise and climate extremes.

For example, the number of marine heatwave days – periods of unusually high sea surface temperatures – has more than tripled globally since the early 1990s. The year 2025 alone saw 65 days of marine heatwaves – meaning they occurred, on average, more than one day a week.

Meanwhile, the cryosphere – the portion of the Earth made up of frozen water, including glaciers, ice sheets and permafrost – is experiencing widespread ice loss and thawing in response to the growing energy imbalance. This affects ecosystems, sea level rise and infrastructure in polar and high-latitude regions.

Rapid warming has also resulted in record extreme temperatures over land, with average maximum temperatures for any single day over 2016-25 around 1.92C above pre-industrial levels). This is an increase of almost half a degree compared to the previous decade (2006-15).

Sea level rise and the energy imbalance

Sea level rise provides one of the clearest long-term signals of a changing planet.

It is closely linked to Earth’s energy imbalance. As heat accumulates in the ocean, water expands, raising sea levels. Meanwhile, a warming land and atmosphere means addition of water to the oceans through melting of glaciers and ice sheets, also adding to sea level rise.

Over the long-term, sea levels have been rising, on average, at a rate of around 1.8mm per year since 1901, totalling a record 23cm in 2025. This is increasing the risk of coastal flooding, erosion and habitat loss in many low-lying areas around the world.

This rise can be seen in the left-hand chart below, which shows observed global sea level changes from tide gauges (grey and blue dashed lines) and satellites (red dashed lines) since 1901. The solid lines indicate the average across multiple datasets.

Sea level rise is accelerating consistent with the observed increase in Earth’s energy imbalance. Over 2006-25, sea levels have risen at a rate of 3.67mm per year – more than double the rate of 1.69mm per year seen over 1976-95.

This increasing rate is shown in the right-hand figure below, which shows four successive overlapping 20-year periods and the most-recent decade.

(Last year’s transition from El Niño to weak La Niña conditions affected global rainfall patterns and led to a small and temporary fall in global average sea level in 2025. This explains the slight decrease in rate of sea level rise for the most recent decade, which is affected more than the 20-year period 2006-25.)

Global average sea level rise over 1901-2025
Left: Global average sea level rise over 1901-2025, relative to a 1995-2014 baseline. Individual timeseries are shown with dashed lines, while the black solid line shows the average (from tide gauges and satellites) used in AR6 and the solid red line shows the 1993-2025 average from satellites. Right: Global mean sea-level rates (in mm per year) for four successive overlapping 20-year periods and the most-recent decade. The shading indicates the very likely range. Credit: Forster et al. (2026)

The bigger picture

Despite greenhouse gas emissions not increasing as rapidly as in the 2000s, this year’s IGCC findings continue to show how far and how fast the climate is changing due to human activity.

A significant increase in decarbonisation efforts in the second half of this decade is required to slow down the rate of human-caused warming and limit the escalation of climate risks and impacts.

These findings, like many others produced by scientists across the globe, rely on international expertise, partnership and the maintenance and availability of global climate datasets and the global observing programmes that underpin them.

This year’s edition of IGCC used more than 40 global datasets produced by research teams around the world, including the NASA satellite record of the Earth’s energy imbalance and the ARGO deep ocean float network.

However, a number of long-term monitoring programmes could be threatened by funding decisions made by governments around the world, most notably the Trump administration in the US.

Local meteorological data and weather balloon measurement programmes in many countries have declined in recent years, especially in Africa, the west Pacific and South America. This reduces scientists’ ability to monitor and understand key indicators of climate change.

This is not just an issue for climate science. Many of these observations are key to weather forecasts and systems that provide early warning for extreme weather. For example, media reports have suggested that recent reductions in weather balloon measurements in Alaska led to a lack of warnings for a recent winter storm.

The continuity and integrity of the climate observations that scientists use to understand how the climate is changing depends on effective and sustained coordination by international organisations, such as the Global Climate Observing System, the World Meteorological Organization and World Climate Research Programme.

Without this data and its coordination, future assessments will be much more difficult at a time when urgent climate action is needed.

The post Guest post: How a record-high ‘energy imbalance’ is driving global warming appeared first on Carbon Brief.

Guest post: How a record-high ‘energy imbalance’ is driving global warming

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Across Ecosystems, Dead Organisms Help Shape the Living World

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A new paper found that the remnants of “foundation species” strongly influenced the fate of survivors.

Death casts a shadow over life, not only for people but also other animals, plants and entire ecosystems.

Across Ecosystems, Dead Organisms Help Shape the Living World

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