(The Conversation) – Tackling climate change by planting trees has an intuitive appeal. They absorb the greenhouse gas carbon dioxide from the atmosphere without using expensive technology.

The suggestion that you can plant trees to offset your carbon emissions is widespread. Many businesses, from those selling shoes to booze, now offer to plant a tree with each purchase, and more than 60 countries have signed up to the Bonn Challenge, which aims to restore degraded and deforested landscapes.

However, expanding tree cover could affect the climate in complex ways. Using models of the Earth’s atmosphere, land and oceans, we have simulated widescale future forestation. Our new study shows that this increases atmospheric carbon dioxide removal, beneficial for tackling climate change. But side-effects, including changes to other greenhouse gases and the reflectivity of the land surface, may partially oppose this.

Our findings suggest that while forestation – the restoration and expansion of forests – can play a role in tackling climate change, its potential may be smaller than previously thought.

When forestation occurs alongside other climate change mitigation strategies, such as reducing emissions of greenhouse gases, the negative side-effects have a smaller impact. So, forestation will be more effective as part of wider efforts to pursue sustainable development. Trees can help fight climate change, but relying on them alone won’t be enough.

What does the future hold?

Future climate projections suggest that to keep warming below the Paris Agreement 2°C target, greenhouse gas emissions must reach net-zero by the mid-to-late 21st century, and become net negative thereafter. As some industries, such as aviation and shipping, will be exceedingly difficult to decarbonise fully, carbon removal will be needed.

Forestation is a widely proposed strategy for carbon removal. If deployed sustainably – by planting mixtures of native trees rather than monocultures, for instance – forestation can provide other benefits including protecting biodiversity, reducing soil erosion, and improving flood protection.

We considered an “extensive forestation” strategy which expands existing forests over the course of the 21st century in line with current proposals, adding trees where they are expected to thrive while avoiding croplands.

In our models, we paired this strategy with two future climate scenarios – a “minimal effort” scenario with average global warming exceeding 4°C, and a “Paris-compatible” scenario with extensive climate mitigation efforts. We could then compare the extensive forestation outcome to simulations with the same climate but where levels of forestation followed more expected trends: the minimal effort scenario sees forest cover drop as agriculture expands, and the Paris-compatible scenario features modest increases in global forest cover.

Image by Anja from Pixabay

Up in the air

The Earth’s energy balance depends on the energy coming in from the Sun and the energy escaping back out to space. Increasing forest cover changes the Earth’s overall energy balance. Generally, changes that decrease outgoing radiation cause warming. The greenhouse effect works this way, as outgoing radiation is trapped by gases in the atmosphere.

Forestation’s ability to lower atmospheric CO₂, and therefore increase the radiation escaping to space, has been well studied. However, the amount of carbon that could feasibly be removed remains a subject of debate.

Forestation generally reduces land surface reflectivity (albedo) as darker trees replace lighter grassland. Decreases in albedo levels oppose the beneficial reduction of atmospheric CO₂, as less radiation escapes back to space. This is particularly important at higher latitudes, where trees cover land that would otherwise be covered with snow. Our scenario features forest expansion primarily in temperate and tropical regions.

Forests emit large quantities of volatile organic compounds (VOCs), with these emissions increasing with rising temperatures. VOCs react chemically in the atmosphere, affecting the concentrations of methane and ozone, which are also greenhouse gases. We find the enhanced VOC emissions from greater forest cover and temperatures increase levels of methane and, typically, ozone. This reduces the amount of radiation escaping to space, further opposing the removal of carbon.

However, the reaction products of VOCs can contribute to aerosols, which reflect incoming solar radiation and help form clouds. Increases in these aerosols with rising VOC emissions from greater forest cover result in more radiation escaping to space.

We find the net effect of changes to albedo, ozone, methane and aerosol is to reduce the amount of radiation escaping to space, cancelling out part of the benefit of reducing atmospheric CO₂. In a future where climate mitigation is not a priority, up to 30% of the benefit is cancelled out, while in a Paris-compatible future, this drops to 15%.

Cooler solutions

Tackling climate change requires efforts from all sectors. While forestation will play a role, our work shows that its benefits may not be as great as previously thought. However, these negative side-effects aren’t as impactful if we pursue other strategies, especially reducing our greenhouse gas emissions, alongside forestation.

This study hasn’t considered local temperature changes from forestation as a result of evaporative cooling, or the impact of changes to atmospheric composition caused by changes in the frequencies and severities of wildfires. Further work in these areas will complement our research.

Nevertheless, our study suggests that forestation alone is unlikely to fix our warming planet. We need to rapidly reduce our emissions while enhancing the ability of the natural world to store carbon. It is important to stress-test climate mitigation strategies in detail, because so many complex systems are at play.

James Weber, Lecturer in Atmospheric Radiation, Composition and Climate, University of Reading and James A. King, Research Associate in Climate Change Mitigation, University of Sheffield

This article is republished from The Conversation under a Creative Commons license. Read the original article.

The Nile is one of the world’s most famous rivers. It’s also Africa’s most important freshwater system. About 300 million people live in the 11 countries it flows through. Many rely on its waters for agriculture and fishing to make a living.

The Nile’s two main tributaries, the Blue Nile and the White Nile, come together in Sudan’s capital city, Khartoum. This industrial hub has grown rapidly over the past few decades.

The Nile is not immune to the same pollutants that affect rivers all over the world. Plastic debris is of particular concern. Over time plastics break down into smaller pieces known as microplastics. These are tiny plastic particles with a maximum size of five millimetres, all the way down to the nanoscale. Recent research found that

rivers are modelled to export up to 25,000 tons of plastics from their sub-basins to seas annually. Over 80% of this amount is microplastic.

This has huge negative consequences for biodiversity and the climate. As microplastics degrade, scientists have found, they produce greenhouse gases. Airborne microplastics may influence the climate by scattering and absorbing solar and terrestrial radiation, leading to atmospheric warming or cooling depending on particle size, shape and composition. It also negatively affects animal and human health. Microplastics have been shown in laboratory studies to be toxic to animals and cells.

Much of the research about microplastics in African waters has focused on marine and coastal areas. To address this gap, I conducted a study to assess the presence of microplastics in the River Nile in Khartoum. My students and I tested for the presence of microplastics in Nile tilapia. This popular African freshwater fish species forms the basis of commercial fisheries in many African countries, including Sudan.

Photo by Islam Hassan on Unsplash

The results do not make for happy reading. In the 30 freshly caught fish we surveyed, we found a total of 567 microplastic particles. This shows that the River Nile is contaminated with microplastics that can be consumed or absorbed in various ways by the tilapia and other aquatic organisms.

Our sample

The fish used in our study were caught just after the meeting point of the two Niles, known in Arabic as Al-Mogran.

We visited the Al-Mawrada fish market in the Omdurman area, which is also alongside the Nile. All 30 specimens we bought were freshly caught.

We dissected the fish to remove their digestive tracts. The individual tracts were treated so they would digest any organic matter they contained without interfering with the analysis of microplastics. The resulting solution was subject to another extraction procedure and we then conducted physical and chemical analyses.

Every specimen had microplastics in its digestive tract.

The number ranged from as few as five to as many as 47 particles per single fish. In total we identified 567 particles. This is high compared to studies that have reported microplastics in tilapia species in other rivers and lakes. There is, as yet, no global guideline or standard for what might be an “acceptable” number.

Shape, size and colour

We detected different sizes of microplastics (0.04mm to 4.94mm), shapes (fibres, fragments, films, foams and pellets) and colours. The most common were very small (less than 1mm), fibrous – they appear slender and elongated – and coloured (dyed).

These characteristics make sense because of how fish and other aquatic organisms feed. Nile tilapia are versatile feeders: they consume a variety of organisms including phytoplankton, aquatic plants, invertebrates, detritus, bacterial films, as well as other fish and fish eggs. That puts them at a high risk of ingesting microplastics.

Nile tilapia are also more likely to consume particles that are within a similar size range as their natural prey, as well as the same shape and colour.

Smaller microplastics are especially good carriers for other pollutants such as heavy metals, resulting in additional health risks. Their small size also makes it easier for them to move into organs like the liver. Studies have found microplastics in the tissues, muscles, livers, blubber and lungs of other aquatic as well as marine mammal species.

Fibres, the most dominant shape found in our specimens, stay in the intestine for longer than other microplastic shapes. This, too, can lead to health problems for the fish. Coloured microplastics contain dyes, many of which contain toxic chemicals.

This all has serious implications for human health, as people catch and eat the fish, which introduces those microplastics and associated chemicals into their bloodstreams.

Pollution sources

Where does all this plastic originate? For starters, 65% of plastic waste in Khartoum is disposed of in open dumps. From there, it contaminates water bodies and other parts of the environment.

Image by Refaat Naiem from Pixabay

The city’s wastewater treatment system is ineffective. The three wastewater treatment plants in Khartoum state, Karary, Wd-Daffiaa and Soba, are outdated and do not meet local and international standards. That means untreated effluent from domestic, industrial and agricultural activities is another probable source of microplastic pollution.

There are also countless recreational sites along the River Nile in Khartoum. The Nile Street is the most popular in the capital city, hosting water sports, restaurants, cafes, clubs, event venues and hotels, as well as the tea ladies (women who serve hot beverages from makeshift mobile cafes along the banks of the river). However, waste disposal and collection practices are sorely lacking, so plastic litter from these leisure activities leaks into the river.

No easy fix

Tackling microplastic pollution is not easy. It will require technological advances, as well as the collective efforts of consumers, producers, governments and the scientific community.

As consumers, we need to change our behaviour around plastic products, especially single-use plastics. For example, opt for fabric shopping bags instead of plastic bags; use glass and metal containers. Recycling is also important.

Governments must enforce waste management regulations and improve waste management practices, as well as helping to improve public awareness. Strategies and policies must explicitly feature microplastics.

Scientists can not only fill the knowledge gaps around microplastics. Communicating scientific findings is crucial; so too is developing innovations to protect against microplastics and their harmful effects.

I would like to thank and acknowledge my student Hadeel Alamin, who conducted this study with me.

Dalia Saad, Researcher, School of Chemistry, University of the Witwatersrand, University of the Witwatersrand

This article is republished from The Conversation under a Creative Commons license. Read the original article.

A heat wave in Greenland and a storm in Antarctica. These kinds of individual weather “events” are increasingly being supercharged by a warming climate. But despite being short-term events they can also have a much longer-term effect on the world’s largest ice sheets, and may even lead to tipping points being crossed in the polar regions.

We have just published research looking at these sudden changes in the ice sheets and how they may impact what we know about sea level rise. One reason this is so important is that the global sea level is predicted to rise by anywhere between 28 cm and 100cm by the year 2100, according to the IPCC. This is a huge range – 70 cm extra sea-level rise would affect many millions more people.

Partly this uncertainty is because we simply don’t know whether we’ll curb our emissions or continue with business as usual. But while possible social and economic changes are at least factored in to the above numbers, the IPCC acknowledges its estimate does not take into account deeply uncertain ice-sheet processes.

Sudden accelerations

The sea is rising for two main reasons. First, the water itself is very slightly expanding as it warms, with this process responsible for about a third of the total expected sea-level rise.

Second, the world’s largest ice sheets in Antarctica and Greenland are melting or sliding into the sea. As the ice sheets and glaciers respond relatively slowly, the sea will also continue to rise for centuries.

Photo by Cassie Matias on Unsplash

Scientists have long known that there is a potential for sudden accelerations in the rate at which ice is lost from Greenland and Antarctica which could cause considerably more sea-level rise: perhaps a metre or more in a century. Once started, this would be impossible to stop.

Although there is a lot of uncertainty over how likely this is, there is some evidence that it happened about 130,000 years ago, the last time global temperatures were anything close to the present day. We cannot discount the risk.

To improve predictions of rises in sea level we therefore need a clearer understanding of the Antarctic and Greenland ice sheets. In particular, we need to review if there are weather or climate changes that we can already identify that might lead to abrupt increases in the speed of mass loss.

Weather can have long-term effects

Our new study, involving an international team of 29 ice-sheet experts and published in the journal Nature Reviews Earth & Environment, reviews evidence gained from observational data, geological records, and computer model simulations.

We found several examples from the past few decades where weather “events” – a single storm, a heatwave – have led to important long-term changes.

The ice sheets are built from millennia of snowfall that gradually compresses and starts to flow towards the ocean. The ice sheets, like any glacier, respond to changes in the atmosphere and the ocean when the ice is in contact with sea water.

These changes could take place over a matter of hours or days or they may be long-term changes from months to years or thousands of years. And processes may interact with each other on different timescales, so that a glacier may gradually thin and weaken but remain stable until an abrupt short-term event pushes it over the edge and it rapidly collapses.

Because of these different timescales, we need to coordinate collecting and using more diverse types of data and knowledge.

Historically, we thought of ice sheets as slow-moving and delayed in their response to climate change. In contrast, our research found that these huge glacial ice masses respond in far quicker and more unexpected ways as the climate warms, similarly to the frequency and intensity of hurricanes and heatwaves responding to changes with the climate.

Ground and satellite observations show that sudden heatwaves and large storms can have long-lasting effects on ice sheets. For example a heatwave in July 2023 meant at one point 67% of the Greenland ice sheet surface was melting, compared with around 20% for average July conditions. In 2022 unusually warm rain fell on the Conger ice shelf in Antarctica, causing it to disappear almost overnight.

These weather-driven events have long “tails”. Ice sheets don’t follow a simple uniform response to climate warming when they melt or slide into the sea. Instead their changes are punctuated by short-term extremes.

For example, brief periods of melting in Greenland can melt far more ice and snow than is replaced the following winter. Or the catastrophic break-up of ice shelves along the Antarctic coast can rapidly unplug much larger amounts of ice from further inland.

Failing to adequately account for this short-term variability might mean we underestimate how much ice will be lost in future.

What happens next

Scientists must prioritise research on ice-sheet variability. This means better ice-sheet and ocean monitoring systems that can capture the effects of short but extreme weather events.

This will come from new satellites as well as field data. We’ll also need better computer models of how ice sheets will respond to climate change. Fortunately there are already some promising global collaborative initiatives.

We don’t know exactly how much the global sea level is going to rise some decades in advance, but understanding more about the ice sheets will help to refine our predictions.

Edward Hanna, Professor of Climate Science and Meteorology, University of Lincoln and Ruth Mottram, Climate Scientist, National Centre for Climate Research, Danish Meteorological Institute

This article is republished from The Conversation under a Creative Commons license. Read the original article.

Amid the escalating threats of a warming world, and with the latest annual United Nations global climate conference (COP28) behind us, there is one critical message that’s often left out of the climate change discourse. Halting overfishing is itself effective climate action.

This argument is the logical conclusion of a plethora of studies that unequivocally assert that stopping overfishing isn’t just a necessity, it’s a win-win for ocean vitality, climate robustness and the livelihoods reliant on sustainable fisheries.

The intricate relationship between climate change and ocean ecosystems was the subject of recent collaborative research — led by researchers at the University of British Columbia — that highlighted the crucial links between overfishing and climate change.

Finding the connections

Our collaborative team of international researchers applied a host of methodologies ranging from literature reviews to quantitative and quality analysis. The findings of this research illuminate eight key multifaceted impacts.

1 — Ending overfishing isn’t merely an ecological imperative but a vital climate action. Doing so would bolster marine life resilience in the face of climate shifts and reduce associate carbon emissions.

2 — Large subsidized fishing boat fleets can actually be a burden on small-scale fisheries, leaving them disproportionately vulnerable to shocks. In turn, overfishing not only depletes resources but also escalates carbon emissions, intensifying climate impacts on these fisheries and their communities, particularly women.

Additionally, the vulnerability of shellfish fisheries to climate stressors further underscores the importance of adaptive strategies tailored to local conditions.

3 — Success stories, like the recovery of European hake stocks, reveal a direct tie between stock recuperation and reduced emissions intensity from fisheries. We must champion and also learn from these successes.

4 — Ecosystem-based fisheries management reverses the “order of priorities so that management starts with ecosystem considerations rather than the maximum exploitation of several target species.”

Ecosystem-based fisheries management has considerable potential to enhance sustainable catches while fostering carbon sequestration. This is perhaps best exemplified by the successful implimentation of ecosystem-based fisheries management in the western Baltic Sea.

5 — Heavy metal pollution in the ocean — such as mercury or lead waste — intensifies the negative impacts of warming and overfishing. This pollution reinforces the need for developing multifaceted regulations based around ecosystem and ocean sustainability solutions.

6 — Overfishing exacerbates climate and biodiversity threats. Climate change contributes to less defined and predictable seasons and is causing reproductive challenges and the propagation of diseases in fish populations — among other issues.

Via Pixabay. .

Adding to these problems, overfishing itself is altering ecological dynamics, modifying habitats and opening new pathways for invasive species. These compounding crises further exacerbate the impacts of overfishing on marine ecosystems while at the same time making fish populations more vulnerable to climate change.

The above factors all combine to reduce the catch potential in any given ecosystem. In turn, fishers are forced to venture farther and deeper in the ocean to fish — increasing carbon emissions, personal risk factors to fishers and bycatch concerns.

7 — International fisheries management must play a central role in promoting biodiversity and retaining the ocean’s carbon sequestration potential. While 87 nations have signed the UN’s Biodiversity of Areas Beyond National Jurisdiction Treaty (also known as the High Seas Treaty), only one has ratified it. This treaty must be fully ratified and its effective implementation should be contingent upon the creation of marine protected areas that cover at least 30 per cent of the high seas.

8 — The ocean has huge carbon sequestration potential. Shifting from the generally accepted maximum of sustainable yield management to maximizing carbon sequestration in fisheries management could further advance climate goals.

Future regulations should allocate a percentage of the annual fish quota to maintain the carbon sequestration function of marine animals. Simply put, beyond just being food, fish stocks serve vital carbon sequestration and biodiversity services that directly benefit humanity. Future regulations should reflect this reality.

A simple goal

This joint collaborative research underscores the urgency of this issue. Ending overfishing isn’t just an ecological imperative but a linchpin for climate action. Furthermore, fisheries aren’t mere victims in these dynamics, but have real agency to play a pivotal role in either exacerbating or mitigating climate change.

An ideal governance framework would focus on managing ecosystems with considerations for their diverse benefits, based on the best evidence available. Regulation of fisheries, while controversial, is essential to not overly exploit such a valuable public resource.

As we gear up to the next COP, we would do well to remember these conclusions. Without nurturing ocean life, addressing climate change becomes an uphill battle. Sustainable fisheries management is not just an ecological necessity. It is also the cornerstone of a resilient, sustainable future.

Rashid Sumaila, Director & Professor, Fisheries Economics Research Unit, University of British Columbia

This article is republished from The Conversation under a Creative Commons license. Read the original article.

<( Tomdispatch.com ) – We live in a world of dangerous, deadly extremes. Record-breaking heat waves, intense drought, stronger hurricanes, unprecedented flash flooding. No corner of the planet will be spared the wrath of human-caused climate change and the earth’s fresh water is already feeling the heat of this new reality. More than half of the world’s lakes and two-thirds of its rivers are drying up, threatening ecosystems, farmland, and drinking water supplies. Such diminishing resources are also likely to lead to conflict and even, potentially, all-out war.

“Competition over limited water resources is one of the main concerns for the coming decades,” warned a study published in Global Environmental Change in 2018. “Although water issues alone have not been the sole trigger for warfare in the past, tensions over freshwater management and use represent one of the main concerns in political relations between… states and may exacerbate existing tensions, increase regional instability and social unrest.”

The situation is beyond dire. In 2023, it was estimated that upwards of three billion people, or more than 37% of humanity, faced real water shortages, a crisis predicted to dramatically worsen in the decades to come. Consider it ironic then that, as water is disappearing, huge dams — more than 3,000 of them — that require significant river flow to operate are now being built at an unprecedented pace globally. Moreover, 500 dams are being constructed in legally protected areas like national parks and wildlife reserves. There was a justification for this, claimed the U.N.’s Intergovernmental Panel on Climate Change (IPCC) some years ago. Such projects, it believed, would help battle climate change by curbing carbon dioxide emissions while bringing electricity to those in the greatest of need.

“[Hydropower] remains the largest source of renewable energy in the electricity sector,” the IPCC wrote in 2018. “Evidence suggests that relatively high levels of deployment over the next 20 years are feasible, and hydropower should remain an attractive renewable energy source within the context of global [greenhouse gas] mitigation scenarios.”

The IPCC acknowledged that unceasing droughts impact stream flow and that climate change is unpredictably worsening matters. Yet its climate experts still contended that hydropower could be a crucial part of the world’s energy transition, arguing that an electric dam will produce seemingly endless energy. At the same time, other renewable sources like wind and solar power have their weather- and sunlight-bound limitations.

A Crack in the Dam Logic

Well-intentioned as it may have been, it’s now far clearer that there is a crack in the IPCC’s appraisal. For one thing, recent research suggests that hydro-powered dams can create an alarming amount of climate-altering greenhouse gas emissions. Rotting vegetation at the bottom of such reservoirs, especially in warmer climates (as in much of Africa), releases significant amounts of methane, a devastating greenhouse gas, into the atmosphere.

“Most of this vegetation would have rotted anyway, of course. But, without reservoirs, the decomposition would occur mostly in the atmosphere or in well-oxygenated rivers or lakes,” explains Fred Pearce in the Independent. “The presence of oxygen would ensure the carbon in the plants formed carbon dioxide. But many reservoirs, particularly in the tropics, contain little oxygen. Under those anaerobic conditions, rotting vegetation generates methane instead.”

While CO2 also seriously harms the climate, methane emissions are far worse in the short term.

“We estimate that dams emit around 25% more methane by unit of surface than previously estimated,” says Bridget Deemer of the School of Environment at Washington State University in Vancouver, lead author of a highly-cited study on greenhouse gas emissions from reservoirs. “Methane stays in the atmosphere for only around a decade, while CO2 stays several centuries, but over the course of 20 years, methane contributes almost three times more to global warming than CO2.”

Buy the Book

And that’s hardly the only problem dams face in the twenty-first century. At the moment, Chinese financing is the most significant global driver of new hydropower construction. China has invested in the creation of at least 330 dams in 74 countries. Each project poses its own set of environmental quandaries. But above all, the heating of the planet — last year was the warmest in human history and January 2024 the hottest January on record — is making many of those investments look increasingly dubious. On this ever-hotter globe of ours, for instance, a drought in Ecuador has all too typically impacted the functionality of the Amaluza Dam on the Paute River, which provides 60% of that country’s electricity. Paute was running at 40% capacity recently as its river flow dwindled. Similarly, in southern Africa, water levels at the Kariba Dam’s reservoir, located between Zambia and Zimbabwe, have fluctuated drastically, impairing its ability to produce consistent energy.

“In recent years, drought intensified by climate change has caused reservoirs on all five continents⁠ to drop below levels needed to maintain hydroelectric production,” writes Jacques Leslie in Yale E360, “and the problem is bound to worsen as climate change deepens.”

Even in the United States, the viability of hydropower is an increasing concern. The Hoover Dam on the Colorado River, for example, has been impacted by years of drought. Water levels at its reservoir, Lake Mead, continue to plummet, raising fears that its days are numbered. The same is true for the Glen Canyon Dam, which also holds back the Colorado, forming Lake Powell. As the Colorado dries up, Glen Canyon may also lose its ability to produce electricity.

Driven by dwindling water resources, the global hydropower crisis has become a flashpoint in the far reaches of Northern Africa, where the creation of a giant dam could very well lead to a regional war and worse.

A Crisis on the Nile

The lifeblood of northeastern Africa, the Nile River, flows through 11 countries before emptying into the Mediterranean Sea. Measured at 6,650 kilometers, the Nile may be the longest river on Earth. For millennia, its meandering waters, which run through lush jungles and dry deserts, have been irrigating farmlands and providing drinking water for millions of people. Nearly 95% of Egypt’s 109 million people live within a few kilometers of the Nile. Arguably the most important natural resource in Africa, it’s now at the epicenter of a geopolitical dispute between Egypt, Ethiopia, and Sudan that’s brought those countries to the brink of military conflict.

A major dam being built along the Blue Nile, the river’s main tributary, is upending the status quo in the region, where Egypt has long been the preeminent nation. The Grand Ethiopian Renaissance Dam (GERD for short) is to become one of the largest hydroelectric dams ever constructed, stretching more than 1,700 meters and standing 145 meters tall, a monument many will love and others despise.

There’s no question that Ethiopia needs the electricity GERD will produce. Nearly 45% of all Ethiopians lack regular power and GERD promises to produce upwards of 5.15 gigawatts of electricity. To put that in perspective, a single gigawatt would power 876,000 households annually in the United States. Construction on the dam, which began in 2011, was 90% complete by last August when it began producing power. In total, GERD’s cost is expected to eclipse $5 billion, making it the largest infrastructure project Ethiopia has ever undertaken and the largest dam on the African continent.

It will not only bring reliable power to that country but promises a culture shift welcomed by many. “Mothers who’ve given birth in the dark, girls who fetch wood for fire instead of going to school — we’ve waited so many years for this — centuries,” says Filsan Abdi of the Ethiopian Ministry of Women, Children, and Youth. “When we say that Ethiopia will be a beacon of prosperity, it starts here.”

While most Ethiopians may see the dam in a positive light, the downstream countries of Egypt and Sudan (itself embroiled in a devastating civil war) were never consulted, and their officials are indignant. The massive reservoir behind GERD’s gigantic cement wall will hold back 74 billion cubic meters of water. That means Ethiopia will have remarkable control over the flow of the Nile, giving its leaders power over how much access to water both Egyptians and Sudanese will have. The Blue Nile, after all, provides 59% of Egypt’s freshwater supply.

As it happens, fresh water in Egypt has long been growing scarcer and so the country’s leadership has taken the threat of GERD seriously for years. In 2012, for instance, Wikileaks obtained internal emails from the “global intelligence” firm Stratfor revealing that Egypt and Sudan were even then considering directing the Egyptian Special Forces to destroy the dam, still in the early stages of construction. “[We] are discussing military cooperation with Sudan,” a high-level Egyptian source was quoted as saying. While such a direct attack never transpired, Stratfor claimed that Egypt might once again lend support to “proxy militant groups against Ethiopia” (as it had in the 1970s and 1980s) if diplomacy were to hit a dead end.

Unfortunately, the most recent negotiations to calm the hostility around GERD have gone distinctly awry. Last April, the embittered Egyptians responded to the lack of any significant progress by conducting a three-day military drill with Sudan at a naval base in the Red Sea aimed at frightening Ethiopian officials. “All options are on the table,” warned Egyptian Foreign Minister Sameh Shoukry. “[All] alternatives remain available and Egypt has its capabilities.”

Seemingly unfazed by such military threats, Ethiopia plans to finish building the dam, claiming it will provide much-needed energy to impoverished Ethiopians and limit the country’s overall carbon footprint. “[GERD] represents a sustainable socio-economic project for Ethiopia: replacing fossil fuels and reducing CO2 emissions,” the Ethiopian embassy in Washington has asserted.

GERD, however, falls squarely into the category of being a major problem dam — and not just because it could lead to a bloody war in a region already in horrific turmoil. Once filled, its massive reservoir will cover a staggering 1,874 square kilometers, making it more than three-quarters the size of Utah’s Great Salt Lake (after it started to shrink).

Unfortunately, GERD never underwent a proper environmental impact assessment (EIA) despite being legally required to do so. No EIA was ever carried out because the notoriously corrupt Ethiopian government knew that the results wouldn’t be pleasing and was unwilling to let any roadblocks get in the way of the dam’s construction, something that became more obvious when upwards of 20,000 indigenous Gumuz and Berta natives began to be forced from their homes to make way for the monstrous dam.

Publicly coming out against the dam has proven a risky business. Employees of International Rivers, a nonprofit that advocates for people endangered by dams, have been harassed and received death threats in response to their opposition. Prominent Ethiopian journalist Reeyot Alemu, a critic of the dam and the government’s actions concerning it, was imprisoned for more than four years under draconian anti-terrorism laws.

Electric Water Wars

While GERD has created a dicey conflict, it also has international ramifications. China, which has played such a pivotal role in bankrolling hydropower projects globally in these years, has provided $1.2 billion to help the Ethiopians build transmission lines from the dam to nearby towns. Since it has also heavily invested in Egypt, it’s well-positioned, if any country is, to help navigate the GERD dispute.

Military analysts in the United States argue that China’s involvement with the dam is part of a policy meant to put the U.S. at a distinct disadvantage in the race to exploit Africa’s abundant rare earth minerals from the cobalt caverns of the Congo to the vast lithium deposits in Ethiopia’s hinterlands. China, the world’s “largest debt collector,” has indeed poured money into Africa. As of 2021, it was that continent’s largest creditor, holding 20% of its total debt. The growth of Chinese influence internationally and in Africa — it has large infrastructure projects in 35 African countries — is crucial to understanding the latest version of the globe’s imperial geopolitics.

Most of China’s African ventures are connected to Beijing’s “Belt and Road Initiative,” a program of this century to fund infrastructure deals across Eurasia and Africa. Its economic ties to Africa began, however, with Chinese leader Mao Zedong’s push in the 1950s and 1960s for an “Afro-Asian” alliance that would challenge Western imperialism.

So many decades later, the idea of such an alliance plays second fiddle to China’s global economic desires, which, like so many past imperial projects in Africa, have significant downsides for those on the receiving end. Developing countries desperately need capital, so they’re willing to accept rigid terms and conditions from China, even if they represent the latest version of the century’s old colonialism and neo-colonialism that focused on controlling the continent’s rich resources. This is certainly true in the case of China’s hydropower investments in places like Ghana’s Bui Dam and the Congo River Dam in the Republic of Congo, where multi-billion-dollar loans are backed by Congo’s crude oil and Ghana’s cocoa crops.

In 2020, the U.S. belatedly inserted itself into the GERD feud, threatening to cut $130 million in aid for Ethiopia’s anti-terrorism efforts. The Ethiopians believed it was related to the dam controversy, as they also did when, in June 2023, the Biden administration directed USAID to halt all food assistance to the country (upwards of $2 billion), claiming it wasn’t reaching Ethiopians, only to reverse course months later.

The dispute over Ethiopia’s enormous dam should be a warning of what the future holds on a hotter, drier planet, where the rivers that feed dams like GERD are drying up while the superpowers continue to jockey for position, hoping to control what remains of the world’s resources. Hydropower won’t help solve the climate crisis, but new dam projects may lead to war over one thing key to our survival — access to fresh, clean water.

Copyright 2024 Joshua Frank

Via Tomdispatch.com

Superstorms, abrupt climate shifts and New York City frozen in ice. That’s how the blockbuster Hollywood movie “The Day After Tomorrow” depicted an abrupt shutdown of the Atlantic Ocean’s circulation and the catastrophic consequences.

While Hollywood’s vision was over the top, the 2004 movie raised a serious question: If global warming shuts down the Atlantic Meridional Overturning Circulation, which is crucial for carrying heat from the tropics to the northern latitudes, how abrupt and severe would the climate changes be?

Twenty years after the movie’s release, we know a lot more about the Atlantic Ocean’s circulation. Instruments deployed in the ocean starting in 2004 show that the Atlantic Ocean circulation has observably slowed over the past two decades, possibly to its weakest state in almost a millennium. Studies also suggest that the circulation has reached a dangerous tipping point in the past that sent it into a precipitous, unstoppable decline, and that it could hit that tipping point again as the planet warms and glaciers and ice sheets melt.

In a new study using the latest generation of Earth’s climate models, we simulated the flow of fresh water until the ocean circulation reached that tipping point.

The results showed that the circulation could fully shut down within a century of hitting the tipping point, and that it’s headed in that direction. If that happened, average temperatures would drop by several degrees in North America, parts of Asia and Europe, and people would see severe and cascading consequences around the world.

We also discovered a physics-based early warning signal that can alert the world when the Atlantic Ocean circulation is nearing its tipping point.

The ocean’s conveyor belt

Ocean currents are driven by winds, tides and water density differences.

In the Atlantic Ocean circulation, the relatively warm and salty surface water near the equator flows toward Greenland. During its journey it crosses the Caribbean Sea, loops up into the Gulf of Mexico, and then flows along the U.S. East Coast before crossing the Atlantic.

This current, also known as the Gulf Stream, brings heat to Europe. As it flows northward and cools, the water mass becomes heavier. By the time it reaches Greenland, it starts to sink and flow southward. The sinking of water near Greenland pulls water from elsewhere in the Atlantic Ocean and the cycle repeats, like a conveyor belt.

Too much fresh water from melting glaciers and the Greenland ice sheet can dilute the saltiness of the water, preventing it from sinking, and weaken this ocean conveyor belt. A weaker conveyor belt transports less heat northward and also enables less heavy water to reach Greenland, which further weakens the conveyor belt’s strength. Once it reaches the tipping point, it shuts down quickly.

What happens to the climate at the tipping point?

The existence of a tipping point was first noticed in an overly simplified model of the Atlantic Ocean circulation in the early 1960s. Today’s more detailed climate models indicate a continued slowing of the conveyor belt’s strength under climate change. However, an abrupt shutdown of the Atlantic Ocean circulation appeared to be absent in these climate models.

Ted-Ed Video: “How do ocean currents work? – Jennifer Verduin”

This is where our study comes in. We performed an experiment with a detailed climate model to find the tipping point for an abrupt shutdown by slowly increasing the input of fresh water.

We found that once it reaches the tipping point, the conveyor belt shuts down within 100 years. The heat transport toward the north is strongly reduced, leading to abrupt climate shifts.

The result: Dangerous cold in the North

Regions that are influenced by the Gulf Stream receive substantially less heat when the circulation stops. This cools the North American and European continents by a few degrees.

The European climate is much more influenced by the Gulf Stream than other regions. In our experiment, that meant parts of the continent changed at more than 5 degrees Fahrenheit (3 degrees Celsius) per decade – far faster than today’s global warming of about 0.36 F (0.2 C) per decade. We found that parts of Norway would experience temperature drops of more than 36 F (20 C). On the other hand, regions in the Southern Hemisphere would warm by a few degrees.

These temperature changes develop over about 100 years. That might seem like a long time, but on typical climate time scales, it is abrupt.

The conveyor belt shutting down would also affect sea level and precipitation patterns, which can push other ecosystems closer to their tipping points. For example, the Amazon rainforest is vulnerable to declining precipitation. If its forest ecosystem turned to grassland, the transition would release carbon to the atmosphere and result in the loss of a valuable carbon sink, further accelerating climate change.

The Atlantic circulation has slowed significantly in the distant past. During glacial periods when ice sheets that covered large parts of the planet were melting, the influx of fresh water slowed the Atlantic circulation, triggering huge climate fluctuations.

So, when will we see this tipping point?

The big question – when will the Atlantic circulation reach a tipping point – remains unanswered. Observations don’t go back far enough to provide a clear result. While a recent study suggested that the conveyor belt is rapidly approaching its tipping point, possibly within a few years, these statistical analyses made several assumptions that give rise to uncertainty.

Instead, we were able to develop a physics-based and observable early warning signal involving the salinity transport at the southern boundary of the Atlantic Ocean. Once a threshold is reached, the tipping point is likely to follow in one to four decades.

The climate impacts from our study underline the severity of such an abrupt conveyor belt collapse. The temperature, sea level and precipitation changes will severely affect society, and the climate shifts are unstoppable on human time scales.

It might seem counterintuitive to worry about extreme cold as the planet warms, but if the main Atlantic Ocean circulation shuts down from too much meltwater pouring in, that’s the risk ahead.

This article was updated on Feb. 11, 2024, to fix a typo: The experiment found temperatures in parts of Europe changed by more than 5 F per decade.

René van Westen, Postdoctoral Researcher in Climate Physics, Utrecht University; Henk A. Dijkstra, Professor of Physics, Utrecht University, and Michael Kliphuis, Climate Model Specialist, Utrecht University

This article is republished from The Conversation under a Creative Commons license. Read the original article.

( Clean Energy Wire ) – Germany’s boom in stationary batteries linked to solar PV systems accelerated last year, doubling the total number of units to more than one million, reports solar industry association BSW. The batteries have a combined capacity of 12 gigawatt-hours – enough to power 1.5 million 2-person households for a day.

“The expansion of solar electricity storage systems has picked up speed rapidly. Both the total number of solar batteries installed and their storage capacity have doubled in just one year,” said the lobby group.

“When installing new solar power systems on private buildings, electricity storage systems are now standard. More and more companies are also storing solar power from their roofs to use it around the clock,” said the association’s director, Carsten Körnig. He added that the market for home and commercial storage systems grew by over 150 per cent in 2023.

The industry group lamented that current policies still underestimate the potential of battery storage systems, and that market barriers continue to slow their spread. Against this backdrop, BSW welcomed the economy and climate ministry’s proposals for a storage strategy published in December, but said the draft didn’t address central strategic questions regarding the role of batteries in tomorrow’s electricity system.

Germany Trade & Invest (GTAI) Video : “Going Green – Germany’s Energy Transition”

Storage systems should be considered a central pillar of the electricity system, on par with generation, grid, and consumption, the industry association said.

Storage will become key in the next phase of the energy transition, as Germany aims to cover 80 percent of power demand with renewable sources by 2030. A traditional electricity system doesn’t require much storage because power generation can be adjusted to match demand.

This changes dramatically as the system uses more renewable energy, as power generation from wind turbines and solar PV systems depends on the weather. This means that production often dramatically exceeds demand but also that current power production can fall well short of what is needed at a given moment.

Via Clean Energy Wire

Published under a “ Creative Commons Attribution 4.0 International Licence (CC BY 4.0)” .

This essay was originally published in Foreign Policy in Focus

Just before the recent climate summit in Dubai, COP28 president Sultan Al-Jaber, with some exasperation, came out with the following rather amazing statement:

“Please help me, show me the roadmap for a phase out of fossil fuel that will allow for sustainable socioeconomic development, unless you want to take the world back into caves.”

Al-Jabar was posturing when he made this quip about caves, but he can almost be forgiven. We badly need a roadmap for a “phase out of fossil fuel that will allow for sustainable socioeconomic development.” By noting the lack of one, he underscored its absence. This is true even if he spoke as a flack of the fossil fuel cartel.

Speaking of COP28, it helped settle the question of the COPs, which still troubles the climate left. The COPs are easily dismissed as “blah blah blah.” But they are, in a word, necessary. We would be in far greater trouble without them, and this is true even though the COPs are condemned to make decisions by consensus, even though they engender endless greenwashing, even though, with next year’s COP29 slated for Azerbaijan, two in a row will be hosted by straight-up petrostates.

The climate negotiations are finally circling core issues. COP26 saw a decision to “phase down” coal, and COP28 opened with the Loss and Damage fund finally lurching into existence. Then came COP28’s key decision text, which called for “Transitioning away from fossil fuels in energy systems, in a just, orderly and equitable manner, accelerating action in this critical decade, so as to achieve net zero by 2050 in keeping with the science.” Only a month later—with President Biden’s move to “pause” the approval of new liquified natural gas terminals, a decision the White House explicitly linked to COP28— the COP decision demonstrated real world benefits. It could have many more in the future, including outside the United States.

Meanwhile, COP29 is set to see the next big battle begin in earnest, as climate finance takes center stage. This battle could (if all goes well) culminate in 2025, where COP30 will be hosted by Lula da Sila’s Brazil, and deliver a meaningful decision on that crucial front. This is not the time to performatively insist that COP stands for “conference of polluters.”

Having said all this, I must immediately add that the climate negotiations have thus far failed, as decisively witnessed by the steadily rising atmospheric carbon-dioxide concentration. COP skeptics are quite right about this. But in their failure the international negotiations are hardly alone. Domestic climate action has had many victories, but it has hardly put us on a path to deep and rapid decarbonization. Nor has the green technology revolution brought planetary emissions into a peak-and-decline pathway. Nor—and this is not easy to say—have the world’s direct action and climate justice movements filled the gaps. Politically, they may be everything, but they too have failed to stop the warming.

One key point: the COP28 text does not simply call for transitioning away from fossil fuels but rather stipulates that this transition must be “just, orderly, and equitable,” a much more challenging prospect. This led Sivan Kartha, a climate equity specialist at the Stockholm Environment Institute, to add that the “deepest fissure” in Dubai was between those who simply want a rapid fossil phase out and those who insist that, to have any hope of success, such a phase out must be fair.

Many of us agree—but what does such fairness imply? 

Embracing “Climate Emergency”

It has become fashionable, yet again, to argue that terms like “climate emergency” are dangerously demoralizing. Perhaps they are. Unfortunately, they are also accurate. We really do have to aim for net-zero emission by 2050, and that means facing political-economic challenges that are difficult to exaggerate. As are those posed by the closely related 1.5°C temperature goal. 

A graphic is appropriate here. I chose this one:

So far, the temperature spike we saw in 2023 is just temporary. For details, see here.

There are lots of voices telling us that 1.5°C is no longer achievable, but this is not quite true. Rather, 1.5°C remains achievable, but only via “overshoot and decline” pathways in which, sometime after the warming grinds past 1.5°C, we manage to claw it back down. What must we do to improve our chances? This is the real question.

We’re going to go into 1.5°C overshoot soon. As we do, even if we assume we’ll be able to draw the temperature back down, we can’t know how extreme the overshoot will be, or how long it will last. We can’t know because it depends on what happens in the future! Some people, Marxist climate hawk Andreas Malm among them, do not think we’ll be able to pull off the necessary drawdown (“I’m not an optimist about the human project”), though he agrees that it is technically possible. 

If we seriously intend to keep 1.5°C alive (as a long-term goal—think 2100), we must in the short term do everything to keep the temperature peak “well below 2°C” (the weak end of the Paris target), which is widely judged, by top scientists, to still be achievable. But there’s a hitch. Even this weaker goal demands, per the IPCC, “rapid, far-reaching and unprecedented changes in all aspects of society.” It’s not going to happen in the world as we have it today. 

If, in 2050, we are approaching true net-zero planetary emissions, we’ll have a good chance of avoiding a world in which the cascading consequences of the warming become unmanageable. Very rapidly building low- and ultra-low emissions energy systems around the world is a necessary step towards that goal—and because such systems are emerging, and rapidly dropping in cost, it’s possible to be honestly optimistic. But such systems are not going to be enough. 

Net-zero 2050 means going beyond the deployment of new, ultra-low emissions infrastructure to also eliminate existing fossil fuel infrastructure. This means that virtually all countries, be they rich or poor, developed or developing, should immediately stop investing in fossil fuel infrastructure, not least because that infrastructure will have to be decommissioned—shut down, mothballed, stranded—long before it’s worn out. All countries must also very rapidly decommission the fossil fuel infrastructure (e.g. existing oil wells, old coal plants) they already have in place—even if it’s profitable and even if people depend on it for their livelihoods. Such a decommissioning process is going to be both expensive and disruptive, in both political and economic terms, and in ways that are particularly hard on poor and insecure populations. 

In a world geared for rapid transition, these would be tractable challenges, but that would be a world in which we were speaking honestly about the depth and profundity of the necessary transformation, a world in which we were, as per Australian author and analyst David Spratt, in “emergency mode.” This, obviously, is not our world, which still tends towards greenwashing, soft-pedaling, and small-bore gradualism, if not actual denialism and climate “brightsiding.”

League of Conservation Voters Video: “A New England Case Study: Accelerating the Clean Energy Transition Through Offshore Wind”

The encouraging possibilities are real, don’t get me wrong.

The green technology revolution really does make it possible for us to save ourselves, and to build new futures. But we’re still facing almost impossible strategic challenges, and justice is at the heart of many of them. Brave choices are going to be necessary, and a political movement that tries to avoid them will not do well when push comes to shove. As it will, within the lifetimes of our children. 

A global extraction phase out

It will be very difficult to engineer a sufficiently rapid phase out of fossil fuel consumption. But the difficulties are even greater when it comes to fossil fuel extraction and production. Think mining, and drilling, and fracking.

There are rich countries like the United States and Norway, which are heavily invested in oil and gas extraction. High-poverty developing countries, like South Africa and India, are heavily invested in coal, while the Democratic Republic of Congo is highly dependent on oil revenue to provide public services. Gulf oil exporters like the United Arab Emirates, the COP28 host, was a developing country before it struck oil. Today, though the UAE may not be “developed” in the same way as, say, the United States or Germany, it is nonetheless a wealthy, high-capacity country with the money and resources to buffer the turbulence that will come with any rapid abandonment of oil.

Which countries deserve more time before they have to stop extracting and selling fossil fuels? The question haunts the climate negotiations, but it is not, in an important sense, the right question at all. The greater truth is that we must do everything to stop the fossil energy pipeline, globally and as soon as possible, and the right question is which countries need support—financial, political, and technological support—before they can hope to rapidly break their dependency on fossil fuel extraction. 

All extracting countries plead their cases. The most legitimate pleas come from poor developing countries that are highly dependent on fossil-related revenues and livelihoods. But before this can become obvious, a point of potential confusion must be clearly acknowledged – lots of countries call themselves developing, but some of them are a lot richer than others. The good news is that this confusion is dissipating, for reasons that were easy to appreciate in Dubai, the global city of the United Arab Emirate. The UAE, like Saudi Arabia, is an extremely wealthy Gulf oil exporter that, while still officially a member of the “Group of 77” developing countries, is not a developing country at all.

Why must we say this? Because we must transition away from fossil fuels in a “just, orderly, and equitable” manner, and because – as the challenge of a fossil fuel extraction phase out makes particularly clear – such a transition is going to be extremely difficult. It is also going to be expensive, which immediately raises the “who pays?” question. Those who wish to evade this question—there are many, and they tend to be rich—seek delay by any available means, and it is important to stress that in the next 10 years aggressively rosy predictions about carbon-dioxide removal—which would, if real, make a perfect case for delay—seem certain to play a leading role in their strategies. 

In this situation, with uncertainty layered upon complexity upon emergency, optimism is as much a danger as pessimism. For one thing, it is not at all obvious that we will manage to rapidly draw temperatures back down after they overshoot 1.5°C—Malm’s pessimism may, in the end, be well placed. For another, all efforts to honestly face the severity of our situation will be endlessly harried by soft-pedaling, false solutions, dangerous distractions, and lies. Politicians everywhere will want all the wiggle room they can get, and meanwhile the fossil cartel will move at every opportunity to deflect all efforts to mandate, or even discuss, the strategic demands of an actual planetary fossil-fuel phase out. 

Al-Jaber was right: we need that roadmap. 

On the ground, with war in the air

The climate negotiations are marked by endless skirmishing between global North and global South, which will not abate anytime soon. How could it, when our world – and its crises – are still strongly structured by the “uneven and combined development” of the colonial past, and the countries of the global North still host the majority of the world’s wealth?

Despite this skirmishing, which has for decades kept fossil fuels off the negotiating agenda, COP28 saw the fossil phaseout challenge finally take center stage. Activists and diplomats alike saw this challenge as a litmus test that would show if the climate negotiations were fit for purpose. Will the negotiations take up the challenge, or can they be forever derailed and distracted, while the fossil cartel just continues its relentless expansion? Perhaps we’ll know in a few years, but just now, after Dubai, a bit of guarded optimism may actually be in order. 

Not everyone in Dubai connected the brutal logic of the climate reckoning to the larger geopolitical crisis, but this crisis hung palpably in the air. COP28 took place in the Arab world, and Gaza did not seem so very far away. The atrocity of the Israeli bombing continued day by excruciating day, and it did not seem that it could be entirely separated from the discussions in the conference halls. The pain was acute within civil society circles. Demonstrations took place, and though they were marginalized by the COP’s security regime, they were noticed. Importantly, the ethos of the protests was an expansive one. The bombing, in particular, was not an isolated consequence of local hatreds. There were larger forces at work. The Palestinians had been given to champion the global South. The United States—the same United States that refused all talk of climate liability—was more than implicated. The term “settler colonialism” was heard again and again. The war, and war in general, was not a distant abstraction.

COPs are not mere climate meetings. The talk is not confined to carbon budgets and energy-system transformation. International debt relief, for example, is now front and center, as is the need for a radically new planetary finance architecture. The global military budget—now over $2 trillion a year—is a common point of comparison, and a reminder that we routinely subsidize violence on a vast scale. The problem of climate is the problem of history, and history is suddenly a very big problem. As the Financial Times noted,

The anecdotal evidence that war is surging round the world is confirmed by the numbers. A recent report by the International Institute for Strategic Studies documented 183 ongoing conflicts around the world, the highest number in more than three decades. And that figure was arrived at before the outbreak of the war in Gaza.

The fraying of the world order is, obviously, a threat to climate cooperation. Beyond this, and beyond the fading illusion that the climate challenge will yield to simple interventions, we’re still only beginning to come to terms with its implacable sprawl. There is little chance of climate stabilization without a political-economic shift that makes robust cooperation possible, but such a shift isn’t going to come cheaply and easily, and simple stories will not help trigger it. How could they when the riddle of climate stabilization is as well the riddle of development, and the riddle of peace?

The Gaza bombing is now on the agenda of the International Court of Justice, where it has joined a crowded docket that includes climate change lawsuits and all manner of other infamies. Nor can these all be laid entirely at the feet of the global North. The two million people of Gaza are currently, and justly, in the spotlight, but spare a thought for another two million people, the Rohingya of Myanmar, who have been murdered and expelled by a huge and terrifying wave of anti-Muslim violence. Southern elites are not innocent. 

And don’t forget Russia’s war in Ukraine, which, in addition to its immediate murderous consequences, is a milestone in the global right’s campaign against collective action, including climate action. It has certainly been an enormous setback to the Russian activist campaign for carbon neutrality.

Spinning the outcome

During COP28’s second week, the negotiations were roiled by the leak of a letter that Haitham al-Ghais, the OPEC secretary general, had sent to the 13 members of OPEC. The letter warned that “pressure against fossil fuels may reach a tipping point with irreversible consequences”, and argued that OPEC members must “proactively reject any text or formula that targets energy i.e. fossil fuels rather than emissions.” 

This was not an isolated move. There was also, by accounts, a great deal of arm twisting, and even a Saudi walkout. Jennifer Morgan, a long-time civil society climate strategist who is now Special Envoy at the German Foreign Ministry, went so far as to speculate that OPEC might be in “a bit of panic.” If so, the panic quickly passed. Once COP28 was over, the Saudis argued that the Dubai agreement to transition away from fossil fuels was entirely optional, just one of several “choices” on an “a la carte menu.”

There are two essential points here. The first is that the OPEC cartel, and the fossil cartel more generally, wants to prevent the “transitioning away” or “phasing out” or “phasing down” frames from taking hold, and argues that “emissions” (which can, it is said, be “captured”) are the real problem. This is the core of the greenwashing strategy, and its partisans will use all available arguments in its service, including repeated references to energy justice. Al-Ghais, for example, explains that “Our goal must be to reduce emissions, which is the core objective of the Paris Agreement, while ensuring energy security and universal access to affordable energy.” 

OPEC has no intention of scaling back fossil fuel extraction. This could change (one must hope) but there is absolutely no chance that it will do so unless the great powers of the global North have already taken the lead and begun their own fossil fuel extraction phase out. Which is why the Biden administration’s decision to scrutinize and hopefully reject a wave of new LNG export terminals, if it survives the counterattacks, could mark a decisive turning point. Talk, after all, is cheap, and just because a country’s delegation supported phase down/out at COP28 (as did the U.S. delegation) this doesn’t mean its actual decision makers are ready and able to follow through. At the COP, many of them clearly weren’t, as is crisply shown in this December 2023 graphic from Carbon Brief:

Some countries, or rather the fossil powers within those countries, are planning even greater production increases than the United States is. Some of these (India and Nigeria) are clearly developing countries, while some (Canada, Russia, and Saudi Arabia) are not. Most all fossil-rich countries, whether their history lay with the global North or the global South, are still planning on exploiting their coal, oil, and gas resources for as long as they possibly can, though do note that China is at the encouraging bottom of the chart. All told, despite its complexities, the picture is grim.

At the same time, the climate reckoning is arriving, and it finds us everywhere divided between rich and poor. In consequence, the countries of the global South can continue to make compelling appeals to basic levels of developmental justice, and these appeals cannot be easily dismissed, even when they bleed into PR cover for continued fossil investment. The energy poverty of the global South is deadly real, as is its pressing need—and its right—to a viable development path, as are the obstacles that today’s world system strews in its path.

(Note that this chart is somewhat out of date – Azerbaijan, which holds the COP29 presidency, has since COP28 announced that it is planning on raising its gas production by a third.)

Moving forward

To succeed, the fossil fuel phaseout roadmap must be reasonably detailed and properly funded. At the same time, it must sharply increase the development and build-out of low-carbon energy systems. In practice, this roadmap has to include nationally differentiated coal, oil, and gas extraction phaseout timeframes detailed enough to be useful to both government planners and political organizers, and financing strategies that can support them. 

Given the emergency, these phaseout timeframes will be extremely challenging, as befits the goal of net-zero emissions by or around 2050. We have to be realistic about this, but it’s not a traditional realism that we’re after. Traditional realism tells us that the necessary timeframes are unachievable, in large part because countries always hew to their “national interests,” which can be only slowly changed. Climate realism, on the other hand, tells us that it’s the pace of the necessary decarbonization, not the politics of the day, that is immutable, and that climate stabilization must come as a solution to a global collective action problem, in which national interests rapidly change. 

Collective action problems—commons problems—have a special relationship to justice. So, while I have no idea what the “orderly” part of “just, orderly, and equitable” is going to wind up meaning, I’m confident that justice and equity are going to be key to any successful climate transition. 

But what kind of justice? And what shape must it take? These questions bring us back to Al-Jaber’s roadmap, the one for a “phase out of fossil fuel that will allow for sustainable socioeconomic development.” It’s a bear of a problem, but lots of people are working on it. For starters, look at the work of the Fossil Fuel Non-Proliferation Treaty initiative. Or Phaseout Pathways for Fossil Fuel Production within Paris-Compliant Carbon Budgets, the Tyndell Centre report that Dan Calverley and Kevin Anderson published in 2022. Or Economic Diversification from Oil Dependency, a report Vincent Yu, a key G77 negotiator, wrote for the Third World Network. Or the many reports of the Civil Society Equity Review, an international collaborative that, full disclosure, I work closely with. The conversation is still in its early days, but there are lots of good ideas floating around. 

Meanwhile, if we’re going to use terms like “economic diversification” and “developing countries,” let’s use them carefully. The challenges here involve “differentiation” between different kinds of countries and different kinds of circumstances, and they are anything but easy. The obvious example is the Gulf oil exporters like Saudi Arabia and the UAE. They may in some sense be developing countries, but they have the money to diversify their economies as they phase out fossil fuel extraction, in ways that other developing countries like Kenya or even India absolutely do not. Harder cases come when you consider China, a hybrid that is both developed and developing, or when you take inequality within countries into proper account. For example, Saudi Arabia is traditionally considered to be a developing country, while the United States is the richest country in the world, but both are brutally divided between rich and poor. Somehow, this has to matter. 

At the end of the day, the biggest differentiation problem remains the one between the global North and the global South. The challenges here are now widely if not routinely recognized. In Dubai, soon after the COP28 decision was gaveled through, Avinash Persaud, now Barbados’ special climate envoy, noted that “Some activists were disappointed we didn’t commit to an immediate fossil fuel phase out. Still, without the trade, investment, and finance to achieve it, it would either have hit developing countries hardest or been meaningless.”

These points will have to be addressed as the finance challenge—the need for a global financial architecture that can support rapid climate transition—takes center stage. Which brings me to a new report – An Equitable Phase Out of Fossil Fuel Extraction: Towards a reference framework for a fast and fair rapid global phase out of coal, oil and gas—the preliminary version of which was released at COP28 by the Extraction Equity Working Group of the Civil Society Equity Review. 

I can’t summarize this report here—though it does sport a fine executive summary—but I do want to explain why its subtitle includes the words “towards a reference framework.” The explanation, basically, is that a detailed climate transition roadmap is not yet possible. An Equitable Phase Out of Fossil Fuel Extraction thus proposes a framework by which to judge the steps that can be taken in the next few years, to at least indicate if they are fair and ambitious enough to have a real chance. To this end, it concentrates on calculating coal, oil, and gas phaseout dates for all major fossil fuel producing countries—here’s a scatterplot with the oil dates; scroll right or left for coal and gas—and on estimating the minimum level of annual international public finance that will be needed to support these phase outs.

This minimum is denominated in “hundreds of billions of dollars” a year. 

An Equitable Phase Out of Fossil Fuel Extraction argues that, if we would limit warming to 1.5°C, all countries must immediately cease to build new fossil fuel extraction infrastructure. Further, wealthy fossil fuel producers whose overall economies are less dependent on fossil extraction—such as the United States, UK, Australia, Norway, Germany, and Canada—must phase out all fossil fuel extraction by 2031, while also providing significant financial support to poorer countries that are economically dependent on fossil fuel revenues and employment. Such poorer countries are given until 2050, though they too must be wrapping things up much earlier. 

One key point, in all this, should never be forgotten. The “unrealistic” nature of these dates is not the result of any equity-side logic—in which we try to model a fair phase out—but rather derives from the implacable constraints imposed by the Earth’s nearly-depleted 1.5°C emissions budget. To push these deadlines out, say to 2060 or 2070, we must either weaken our temperature goal or we must assume—as the geoengineers will incessantly encourage us to do—that gigatons upon gigatons of carbon-dioxide can very soon, and affordably, and safely, be collected and concentrated and “sequestered” away. 

Back to the ground

After Dubai, much of the left’s commentary focused on criticizing the late-game negotiations in which “phase out” was replaced by “transitioning away,” as if such diplomatic wordsmithing was only a watering down, as if it revealed the compromised truth at the core of a meaningless negotiation. For the activists embedded in the negotiations, the sense was different. They generally agreed that Dubai had “sent the necessary signal”—despite everything, the world’s governments have decided the fossil economy has to go.

Bill McKibben, to my mind, had the right take on this disagreement when he argued that the “transitioning away” phrase “will hang over every discussion from now on—especially the discussions about any further expansion of fossil fuel energy.” In a nutshell, he argued that the diplomats forged a tool and it’s up to us all to wield it.

The Dubai decision is of course limited. But its real weakness has more to do with loopholes and omissions than with any fine point of diplomatic wording. And the greatest of its omissions is financial: there is no agreement on how the phaseout will be funded. Harjeet Singh, now the Global Engagement Director for the Fossil Fuel Non-Proliferation Treaty Initiative, put the overall picture succinctly and well,

A long-overdue direction to move away from coal, oil, and gas has been set. Yet, the resolution is marred by loopholes that offer the fossil fuel industry numerous escape routes, relying on unproven, unsafe technologies. The hypocrisy of wealthy nations, particularly the USA, as they continue to expand fossil fuel operations massively while merely paying lip service to the green transition, stands exposed. Developing countries, still dependent on fossil fuels for energy, income, and jobs, are left without robust guarantees for adequate financial support in their urgent and equitable transition to renewables. COP28 recognised the immense financial shortfall in tackling climate impacts, but the final outcomes fall disappointingly short of compelling wealthy nations to fulfil their financial responsibilities—obligations amounting to hundreds of billions, which remain unfulfilled.

Harjeet is being diplomatic when he refers to “hundreds of billions,” a figure that echoes the one used in the Equitable Phase Out of Fossil Fuel Extraction report. It seems to be the formulation of choice these days, at least when civil society researchers and activists want to assert financial markers large enough to move the window, but small enough to be taken as realistic.

It’s important to understand that figures of this scale refer to public monies—grants and grant equivalents—and that they’ve lately been sharing the stage with references to trillions, which are typically private monies framed as “investments.” As in Dubai’s high-level Leader’s Declaration, which spoke of the opportunities that lay in “investing $5-7tn annually in greening the global economy by 2030.” 

The elites, left to their own devices, are far more likely to deliver on ambitious private finance pledges than on ambitious public ones. Investment is something they know how to do. But a future defined by “investment” and “insurance” and “loans” and “aid” is unlikely be a future that takes proper account of even deep decarbonization, let alone the challenges of development in a climate-constrained world, let alone people-centered adaptation and an ethically defensible loss and damage response and recovery system. Which is to say that, unless we win a comprehensive climate finance breakthrough, all hope for a “fair, orderly, and equitable” transition will be abandoned in favor of a short-term neoliberal expediency that is unlikely to deliver the global just transition we actually need. 

The challenge here encompasses everything from the historical responsibility of the global North to the debt crisis now wracking the global South to the inequality crisis raging in both North and South. Not to mention the crisis of democracy and the endless techno-economic complexities of the great rebuilding that’s now on the horizon. Bracket all this for now, but know that the next international battle will be fought over finance. 

It’s about time. 

Tom Athanasiou

This essay was originally published in Foreign Policy in Focus

An effective criticism of social and political woes by public intellectuals might get the attention of some segments of the public, especially those who might be labeled “politically aware”—individuals who regularly follow the news and crises of the day. But there is more to being a public intellectual than becoming a gadfly gnawing on the pestiferous hide of the establishment. Eloquently depicting misdirection, mismanagement, and overweening ambitions among the political class can be motivating but often prove insufficient. Worse yet, it could become a self-defeating enterprise when these criticisms lead to public despair and political alienation. It is akin to the proverbial heralding that “the emperor has no clothes,” with the added twist that no tailor can sew one either. When others pile on, we get closer to a political black hole.

Churning out critical essays and commentaries should not be the end but an inducement to search for remedies. What utility do such analyses offer if their message only intimates a rotten and entrenched status quo immune to change and improvements?

Channel 4 New Video: “Hannah Ritchie on replacing eco-anxiety with ‘cautious optimism’ & how to build a sustainable world”

The public intellectual must go beyond criticism of the unsatisfactory status quo and policies by inspiring a sense of optimism in the public’s mind about change and reform and suggesting how they might be achieved. How can this be done responsibly?

Paul Romer, a Nobel laureate in Economics (2018), distinguishes complacent optimism from contingent optimism (he calls it  “conditional optimism”; I prefer contingent optimism to  accentuate the difference with complacent optimism) by giving an example of each: “Complacent optimism is the feeling of a child waiting for presents. “Contingent optimism “ is the feeling of a child who is thinking about building a treehouse. ‘If I get some wood and nails and persuade some other kids to help do the work, we can end up with something really cool.” In the first case (complacent optimism), the child is passive, awaiting a present with earnest expectation. In the second case (contingent optimism), the child lays out a plan to make her wish a reality. The optimism of the first child is wholly dependent on the largesse of others; she makes herself the object of her expectations. The optimism of the second child is born of her agency to identify and secure the resources she needs to build her treehouse.

Contingent optimism begins by taking stock of the challenge. Once the problem is defined, you search for credible solutions to change the situation in the desired direction. In other words, contingent optimism makes the reason for developing an optimistic outlook contingent on working out a strategy of change that makes it likely to achieve the outcomes one seeks. It is the careful mapping out of a plan that justifies feeling optimistic about change. That optimism is contingent on having correctly defined the problem and potential solutions.

We should expect contingent optimism from public intellectuals, not despair. They are uniquely equipped and positioned to critically analyze our societal ills and propose remedies that can change the system to better serve the common good. The same goes for the rest of us. Deluding ourselves with passive hope is the essence of complacent optimism. Planning how to achieve our wishes justifies optimism—contingently, of course!