The climate is changing so fast that we haven’t seen how bad extreme weather could get

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Andreas Thaller/Alamy Stock Photo

Simon H. Lee, University of St Andrews; Hayley J. Fowler, Newcastle University, and Paul Davies, Newcastle University

Extreme weather is by definition rare on our planet. Ferocious storms, searing heatwaves and biting cold snaps illustrate what the climate is capable of at its worst. However, since Earth’s climate is rapidly warming, predominantly due to fossil fuel burning, the range of possible weather conditions, including extremes, is changing.

Scientists define “climate” as the distribution of possible weather events observed over a length of time, such as the range of temperatures, rainfall totals or hours of sunshine. From this they construct statistical measures, such as the average (or normal) temperature. Weather varies on several timescales – from seconds to decades – so the longer the period over which the climate is analysed, the more accurately these analyses capture the infinite range of possible configurations of the atmosphere.

Typically, meteorologists and climate scientists use a 30-year period to represent the climate, which is updated every ten years. The most recent climate period is 1991-2020. The difference between each successive 30-year climate period serves as a very literal record of climate change.

This way of thinking about the climate falls short when the climate itself is rapidly changing. Global average temperatures have increased at around 0.2°C per decade over the past 30 years, meaning that the global climate of 1991 was around 0.6°C cooler than that in 2020 (when accounting for other year-to-year fluctuations), and even more so than the present day.

A moving target for climate modellers

If the climate is a range of possible weather events, then this rapid change has two implications. First, it means that part of the distribution of weather events comprising a 30-year climate period occurred in a very different background global climate: for example, northerly winds in the 1990s were much colder than those in the 2020s in north-west Europe, thanks to the Arctic warming nearly four times faster than the global average. Statistics from three decades ago no longer represent what is possible in the present day.

Second, the rapidly changing climate means we have not necessarily experienced the extremes that modern-day atmospheric and oceanic warmth can produce. In a stable climate, scientists would have multiple decades for the atmosphere to get into its various configurations and drive extreme events, such as heatwaves, floods or droughts. We could then use these observations to build up an understanding of what the climate is capable of. But in our rapidly changing climate, we effectively have only a few years – not enough to experience everything the climate has to offer.

Extreme weather events require what meteorologists might call a “perfect storm”. For example, extreme heat in the UK typically requires the northward movement of an air mass from Africa combined with clear skies, dry soils and a stable atmosphere to prevent thunderstorms forming which tend to dissipate heat.

Such “perfect” conditions are intrinsically unlikely, and many years can pass without them occurring – all while the climate continues to change in the background. Based on an understanding of observations alone, this can leave us woefully underprepared for what the climate can now do, should the right weather conditions all come together at once.

Startling recent examples include the extreme heatwave in the Pacific north-west of North America in 2021, in which temperatures exceeded the previous Canadian record maximum by 4.6°C. Another is the occurrence of 40°C in the UK in summer 2022, which exceeded the previous UK record maximum set only three years earlier by 1.6°C. This is part of the reason why the true impact of a fixed amount of global warming is only evident after several decades, but of course – since the climate is changing rapidly – we cannot use this method anymore.

Playing with fire

To better understand these extremes, scientists can use ensembles: many runs of the same weather or climate model that each slightly differ to show a range of plausible outcomes. Ensembles are routinely used in weather prediction, but can also be used to assess extreme events which could happen even if they do not actually happen at the time.

When 40°C first appeared in ensemble forecasts for the UK before the July 2022 heatwave, it revealed the kind of extreme weather that is possible in the current climate. Even if it had not come to fruition, its mere appearance in the models showed that the previously unthinkable was now possible. In the event, several naturally occurring atmospheric factors combined with background climate warming to generate the record-shattering heat on July 19 that year.

The highest observed temperature each year in the UK, from 1900 to 2023

A graph showing the highest observed temperature in the UK between 1900 and 2023.
The hottest days are getting hotter in the UK. Met Office/Kendon et al. 2024

Later in summer 2022, after the first occurrence of 40°C, some ensemble weather forecasts for the UK showed a situation in which 40°C could be reached on multiple consecutive days. This would have posed an unprecedented threat to public health and infrastructure in the UK. Unlike the previous month, this event did not come to pass, and was quickly forgotten – but it shouldn’t have been.

It is not certain whether these model simulations correctly represent the processes involved in producing extreme heat. Even so, we must heed the warning signs.

Despite a record-warm planet, summer 2024 in the UK has been relatively cool so far. The past two years have seen global temperatures far above anything previously observed, and so potential extremes have probably shifted even further from what we have so far experienced.

Just as was the case in August 2022, we’ve got away with it for now – but we might not be so lucky next time.


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Simon H. Lee, Lecturer in Atmospheric Science, University of St Andrews; Hayley J. Fowler, Professor of Climate Change Impacts, Newcastle University, and Paul Davies, Chief Meteorologist, Met Office and Visiting Professor, Newcastle University

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

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Global wheat yields would be ‘10%’ higher without climate change

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Original article by Orla Dwyer republished from Carbon Brief under a CC license.

Wheat affected by drought conditions in Bremen, Germany in May 2025. Credit: dpa picture alliance / Alamy Stock Photo.

Global yields of wheat are around 10% lower now than they would have been without the influence of climate change, according to a new study. 

The research, published in the Proceedings of the National Academy of Sciences, looks at data on climate change and growing conditions for wheat and other major crops around the world over the past 50 years. 

It comes as heat and drought have this year been putting wheat supplies at risk in key grain-producing regions, including parts of Europe, China and Russia. 

The study finds that increasingly hot and dry conditions negatively impacted yields of three of the five key crops examined. 

Overall, global grain yields soared during the study period due to technological advancements, improved seeds and access to synthetic fertilisers. 

But these yield setbacks have “important ramifications for prices and food security”, the study authors write. 

Grain impacts 

Most parts of the world have experienced “significant” yield increases in staple crops since the mid-20th century. 

The new study notes that, in the past 50 years, yields increased by 69-123% for the five staple crops included in the research – wheat, maize, barley, soya beans and rice. 

But crop production is increasingly threatened by climate change and extreme weather. A 2021 study projected “major shifts” in global crop productivity due to climate change within the next two decades.

Earlier this year, Carbon Brief mapped out news stories of crops being destroyed around the world by heat, drought, floods and other weather extremes in 2023-24. Maize and wheat were the crops that appeared most frequently in these reports. 

The crops that appeared most frequently in media reports of extreme weather impacts analysed by Carbon Brief, ranked in order of most to least frequent: maize, wheat, rice, potatoes, soya beans, olives, bananas, grapes, sunflowers and coffee. Credit: Carbon Brief.
The crops that appeared most frequently in media reports of extreme weather impacts analysed by Carbon Brief, ranked in order of most to least frequent: maize, wheat, rice, potatoes, soya beans, olives, bananas, grapes, sunflowers and coffee. Credit: Carbon Brief.

Hot and dry weather is currently threatening wheat crops in parts of China, the world’s largest wheat producer, Reuters reported this month.

In the UK, wheat crops are struggling amid the “driest start to spring in England for almost 70 years”, the Times recently reported. Farm groups say some crops are already failing, the Guardian said. 

As a result, global wheat supplies are “tight”, according to Bloomberg, with price rises possible depending on weather conditions in parts of Europe, China and Russia. 

Food security and prices

The study uses climate datasets, modelling and national crop statistics from the UN Food and Agriculture Organization to assess crop production and climate trends in key grain-producing countries over 1974-2023, including Argentina, Brazil, Canada, China, the EU, Russia and the US. 

The researchers assess climate observations and then use crop models to calculate what yields would have been with and without these climate changes. 

For example, “if it has warmed 1C over 50 years and the model says that 1C leads to 5% yield loss, we’d calculate that the warming trend caused a loss of 5%”, Prof David Lobell, the lead study author and a professor at Stanford University, tells Carbon Brief. 

The study looks at two reanalysis climate datasets that include information on temperature and rainfall over the past 50 years: TerraClimate (TC) and ERA5-Land. (Reanalysis data combines observations with a modern forecasting model.)

The researchers find that yields of three of the five crops are lower than they would have been without warmer temperatures and other climate impacts in the past 50 years. 

Yields were lower than they otherwise would have been by 12-14% for barley, 8-12% for wheat and 4% for maize. 

The impacts on soya beans were less clear as there were “significant differences” between data sources. But both datasets show a negative impact on yields, ranging from 2% to 8%.

The effects on rice yields were inconclusive, with one dataset showing a positive effect of around 1% while the other showed a negative effect of about 3%.   

The chart below shows the estimated yield impacts for each crop based on the calculations from the two climate datasets.

The estimated percentage impact of climate factors on yields of wheat (brown), maize (yellow), rice (blue), soya bean (green) and barley (purple) from 1974-2023, using two different historical climate datasets. Source: Lobell et al. (2025).
The estimated percentage impact of climate factors on yields of wheat (brown), maize (yellow), rice (blue), soya bean (green) and barley (purple) from 1974-2023, using two different historical climate datasets. Source: Lobell et al. (2025).

Given soaring overall crop yields during this time, impacts of 4-13% “may seem trivial”, the researchers write. But, they say, it can have “important ramifications for prices and food security” given growing food demand, noting: 

“The overall picture of the past half-century is that climate trends have led to a deterioration of growing conditions for many of the main grain-producing regions of the world.” 

Water stress and heat

The study also assesses the impacts that warming and vapour pressure deficit – a key driver of plant water stress – have on crop yields. 

Vapour pressure deficit is the difference between the amount of water vapour in the air and the point at which water vapour in the air becomes saturated. As air becomes warmer, it can hold more water vapour. 

A high deficit can reduce plant growth and increase water stress. The models show that these effects may be the main driver of losses in grain yield, with heat having a more “indirect effect”, as higher temperatures drive water stress. 

Agricultural irrigation system watering dry soil on a crop field in the US. Credit: Andrii Biletskyi / Alamy Stock Photo. Image ID: 3AKGHEX.
Agricultural irrigation system watering dry soil on a crop field in the US. Credit: Andrii Biletskyi / Alamy Stock Photo.

The study finds that vapour pressure deficit increased in most temperate regions in the past 50 years. 

The researchers compare their data to climate modelling simulations covering the past 50 years. They find largely similar results, but notice a “significant underestimation” of vapour pressure deficit increases in temperate regions in most climate models. 

Many maize-growing areas in the EU, China, Argentina and much of Africa have vapour deficit trends that “exceed even the highest trend in models”, they write. 

The researchers also find that most regions experienced “rapid warming” during the study period, with the average crop-growing season now warmer than more than 80% of growing seasons 50 years ago. 

The findings indicate that, in some areas, “even the coolest growing season in the present day is warmer than the warmest season that would have occurred 50 years ago”. 

Wheat growing in a field. Credit: Jon Freeman / Alamy Stock Photo. Image ID: EXYNXR.
Wheat growing in a field. Credit: Jon Freeman / Alamy Stock Photo.

An exception to this is in the US and Canada, they find, with most maize and soya bean crop areas in the US experiencing lower levels of warming than other parts of the world and a “slight cooling” in wheat-growing areas of the northern Great Plains and central Canada.

(The central US has experienced a cooling trend in summer daytime temperatures since the middle of the 20th century, according to the National Oceanic and Atmospheric Administration. There are many theories behind this “warming hole”, which has continued despite climate change.) 

CO2 greening 

Dr Corey Lesk, a postdoctoral researcher at Dartmouth College who studies the impacts of climate on crops, says these findings are in line with other recent estimates. He tells Carbon Brief: 

“There are some uncertainties and sensitivity to model specification here – but it’s somewhat likely climate change has already reduced crop yields in the global mean.” 

The study’s “main limitation” is that it is “behind” on including certain advances in understanding how soil moisture impacts crops, Lesk adds: 

“Moisture changes and CO2 [carbon dioxide] effects are the largest present uncertainties in past and future crop impacts of climate change. This paper is somewhat limited in advancing understanding on those aspects, but it’s illuminating to pause and take stock.”

The research looks at whether the benefits of CO2 increases during the past 50 years exceed the negative effects of higher levels of the greenhouse gas. 

Rising CO2 levels can boost plant growth in some areas in a process called “CO2 fertilisation”. However, a 2019 study found that this “global greening” could be stalled by growing water stress. 

Yield losses for wheat, maize and barley “likely exceeded” any benefits of CO2 increases in the past 50 years, the study finds. 

The opposite is true for soya beans and rice, they find, with a net-positive impact of more than 4% on yields. 

Soya beans growing in a field. Credit: Volodymyr Shtun / Alamy Stock Photo. Image ID: 3B84F7G.
Soya beans growing in a field. Credit: Volodymyr Shtun / Alamy Stock Photo.

Climate science has “done a remarkable job of anticipating global impacts on the main grains and we should continue to rely on this science to guide policy decisions”, Lobell, the lead study author, says in a press release

He adds that there may be “blind spots” on specialised crops, such as coffee, cocoa, oranges and olives, which “don’t have as much modelling” as key commodity crops, noting: 

“All these have been seeing supply challenges and price increases. These matter less for food security, but may be more eye-catching for consumers who might not otherwise care about climate change.”

 Lobell et al. (2025), A half-century of climate change in major agricultural regions: Trends, impacts, and surprises, Proceedings of the National Academy of Sciences, doi:10.1073/pnas.2502789122

Original article by Orla Dwyer republished from Carbon Brief under a CC license.

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Overshooting 1.5°C: even temporary warming above globally agreed temperature limit could have permanent consequences

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A wildfire raging near a residential area of Daegu, South Korea in April 2025. EPA-EFE/Yonhap

Paul Dodds, UCL

Earth’s surface temperature has been 1.5°C hotter than the pre-industrial average for 21 of the last 22 months.

The 2015 Paris agreement committed countries to keeping the global temperature increase “well below 2°C”, which is widely interpreted as an average of 1.5°C over a 30-year period. The Paris agreement has not yet failed, but recent high temperatures show how close the Earth is to crossing this critical threshold.

Climate scientists have, using computer simulations, modelled pathways for halting climate change at internationally agreed limits. However, in recent years, many of the pathways that have been published involve exceeding 1.5°C for a few decades and removing enough greenhouse gas from the atmosphere to return Earth’s average temperature below the threshold again. Scientists call this “a temporary overshoot”.

If human activities were to raise the global average temperature 1.6°C above the pre-industrial average, for example, then CO₂ removal, using methods ranging from habitat restoration to mechanically capturing CO₂ from the air, would be required to return warming to below 1.5°C by 2100.


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Do we really understand the consequences of “temporarily” overshooting 1.5°C? And would it even be possible to lower temperatures again?

Faith that a temporary overshoot will be safe and practicable has justified a deliberate strategy of delaying emission cuts in the short term, some scientists warn. The dangers posed by remaining above the 1.5°C limit for a period of time have received little attention by researchers like me, who study climate change.

To learn more, the UK government commissioned me and a team of 36 other scientists to examine the possible impacts.

How nature will be affected

We examined a “delayed action” scenario, in which greenhouse gas emissions remain similar for the next 15 years due to continued fossil fuel burning but then fall rapidly over a period of 20 years.

We projected that this would cause the rise in Earth’s temperature to peak at 1.9°C in 2060, before falling to 1.5°C in 2100 as greenhouse gases are removed from the atmosphere. We compared this scenario with a baseline scenario in which the global temperature does not exceed 1.5°C of warming this century.

Our Earth system model suggested that Arctic temperatures would be up to 4°C higher in 2060 compared to the baseline scenario. Arctic Sea ice loss would be much higher. Even after the global average temperature was returned to 1.5°C above pre-industrial levels, in 2100, the Arctic would remain around 1.5°C warmer compared to the baseline scenario. This suggests there are long-term and potentially irreversible consequences for the climate in overshooting 1.5°C.

Comparative maps of global temperature increases in the middle of the century caused by overshooting 1.5°C, when compared to a pathway in which the global temperature does not exceed 1.5°C.
Temperature increases caused by overshooting 1.5°C are primarily felt in the Arctic and on land. Selena Zhang, Maria Russo, Luke Abraham and Alex Archibald.

As global warming approaches 2°C, warm-water corals, Arctic permafrost, Barents Sea ice and mountain glaciers could reach tipping points at which substantial and irreversible changes occur. Some scientists have concluded that the west Antarctic ice sheet may have already started melting irreversibly.

Our modelling showed that the risk of catastrophic wildfires is substantially higher during a temporary overshoot that culminates in 1.9°C of warming, particularly in regions already vulnerable to wildfires. Fires in California in early 2025 are an example of what is possible when the global temperature is higher.

Our analysis showed that the risk of species going extinct at 2°C of warming is double that at 1.5°C. Insects are most at risk because they are less able to move between regions in response to the changing climate than larger mammals and birds.

The impacts on society

Only armed conflict is considered by experts to have a greater impact on society than extreme weather. Forecasting how extreme weather will be affected by climate change is challenging. Scientists expect more intense storms, floods and droughts, but not necessarily in places that already regularly suffer these extremes.

In some places, moderate floods may reduce in size while larger, more extreme events occur more often and cause more damage. We are confident that the sea level would rise faster in a temporary overshoot scenario, and further increase the risk of flooding. We also expect more extreme floods and droughts, and for them to cause more damage to water and sanitation systems.

Floods and droughts will affect food production too. We found that impact studies have probably underestimated the crop damage that increases in extreme weather and water scarcity in key production areas during a temporary overshoot would cause.

We know that heatwaves become more frequent and intense as temperatures increase. More scarce food and water would increase the health risks of heat exposure beyond 1.5°C. It is particularly difficult to estimate the overall impact of overshooting this temperature limit when several impacts reinforce each other in this way.

In fact, most alarming of all is how uncertain much of our knowledge is.

For example, we have little confidence in estimates of how climate change will affect the economy. Some academics use models to predict how crops and other economic assets will be affected by climate change; others infer what will happen by projecting real-word economic losses to date into future warming scenarios. For 3°C of warming, estimates of the annual impact on GDP using models range from -5% to +3% each year, but up to -55% using the latter approach.

We have not managed to reconcile the differences between these methods. The highest estimates account for changes in extreme weather due to climate change, which are particularly difficult to determine.

We carried out an economic analysis using estimates of climate damage from both models and observed climate-related losses. We found that temporarily overshooting 1.5°C would reduce global GDP compared with not overshooting it, even if economic damages were lower than we expect. The economic consequences for the global economy could be profound.

So, what can we say for certain? First, that temporarily overshooting 1.5°C would be more costly to society and to the natural world than not overshooting it. Second, our projections are relatively conservative. It is likely that impacts would be worse, and possibly much worse, than we estimate.

Fundamentally, every increment of global temperature rise will worsen impacts on us and the rest of the natural world. We should aim to minimise global warming as much as possible, rather than focus on a particular target.


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Paul Dodds, Professor of Energy Systems, UCL

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

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Continue ReadingOvershooting 1.5°C: even temporary warming above globally agreed temperature limit could have permanent consequences

Climate crisis on track to destroy capitalism, warns top insurer

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https://www.theguardian.com/environment/2025/apr/03/climate-crisis-on-track-to-destroy-capitalism-warns-allianz-insurer

Some companies were ending home insurance in California due to wildfires, says Allianz SE board member. He says that without insurance, many other financial services become unviable, from mortgages to investments. Photograph: Mario Tama/Getty Images

Action urgently needed to save the conditions under which markets – and civilisation itself – can operate, says senior Allianz figure

The climate crisis is on track to destroy capitalism, a top insurer has warned, with the vast cost of extreme weather impacts leaving the financial sector unable to operate.

The world is fast approaching temperature levels where insurers will no longer be able to offer cover for many climate risks, said Günther Thallinger, on the board of Allianz SE, one of the world’s biggest insurance companies. He said that without insurance, which is already being pulled in some places, many other financial services become unviable, from mortgages to investments.

Global carbon emissions are still rising and current policies will result in a rise in global temperature between 2.2C and 3.4C above pre-industrial levels. The damage at 3C will be so great that governments will be unable to provide financial bailouts and it will be impossible to adapt to many climate impacts, said Thallinger, who is also the chair of the German company’s investment board and was previously CEO of Allianz Investment Management.

The core business of the insurance industry is risk management and it has long taken the dangers of global heating very seriously. In recent reports, Aviva said extreme weather damages for the decade to 2023 hit $2tn, while GallagherRE said the figure was $400bn in 2024. Zurich said it was “essential” to hit net zero by 2050.

Thallinger said: “The good news is we already have the technologies to switch from fossil combustion to zero-emission energy. The only thing missing is speed and scale. This is about saving the conditions under which markets, finance, and civilisation itself can continue to operate.”

Nick Robins, the chair of the Just Transition Finance Lab at the London School of Economics, said: “This devastating analysis from a global insurance leader sets out not just the financial but also the civilisational threat posed by climate change. It needs to be the basis for renewed action, particularly in the countries of the global south.”

Original article at https://www.theguardian.com/environment/2025/apr/03/climate-crisis-on-track-to-destroy-capitalism-warns-allianz-insurer

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Continue ReadingClimate crisis on track to destroy capitalism, warns top insurer

How global inequality hinders climate action

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Leaders from around the globe are meeting in Davos. Michael Derrer Fuchs/Shutterstock

Susan Ann Samuel, University of Leeds

World leaders have gathered for the World Economic Forum annual meeting in Davos, Switzerland. One of their main goals is to align their responses to geopolitical shocks such as floods and wildfires that hamper trade, investment and more.

The meeting also supposedly aims to find ways to stimulate economic growth to improve living standards, foster a just and inclusive energy transition, achieve security and cooperation amidst conflicts, and accelerate the economic response to an “intelligent age” of AI.

But, a new report from Oxfam International, published on the first day of the meeting in Davos, highlights how global inequality is more rampant than ever. The report, written by a team of policy campaigners and inequality research advisers outlines how billionaire wealth rose sharply in 2024 worldwide, with the pace of the increase three times faster than in 2023.

The World Economic Forum lists extreme weather as one of the top global risks. But, as world leaders convene in Davos, the high-profile anti-climate stances of some of them stand in stark opposition to any meaningful progress for climate action.

The Oxfam report highlights the exploitation involved in creating and sustaining wealth and outlines how, as inequalities deepen, vulnerable communities are disproportionately affected. The most vulnerable – overwhelmingly women, people of colour, Indigenous groups and low-wage workers – are caught in a cycle of insufficient wages, limited services and minimal political influence.

The report also highlights how wealth inequality is often intertwined with historical processes of extraction — both within countries (for example, through weak labour protections that lowers wages) and between countries (through trade, finance, and resource exploitation).

The climate connection

Other research has also shown how inequality is deeply interwoven with climate breakdown. Each crisis exacerbates the other. Historically, the richest nations – and within them, the wealthiest people – have contributed the most to greenhouse gas emissions.

Meanwhile, lower-income countries that bear little responsibility for global heating suffer the most. These countries, already burdened by debt and systemic inequality, have fewer resources to protect communities from extreme weather, crop failures and infrastructure damage. This makes day-to-day survival a struggle for billions.

When climate change exacerbates existing inequalities, marginalised communities are denied basic human rights. For instance, droughts reduce crop yields and deplete water sources, so more people — often women and children — have to ration supplies or go without. This directly infringes on their rights to food, safe drinking water and sanitation.

In these ways, without climate action, the warming planet threatens to widen inequalities by affecting the poorest people most severely. A 2020 World Bank report estimated that an additional 68 to 135 million people could be pushed into poverty by 2030 because of climate change. French researchers identified that climate change also slows down the economic catch-up of poorer countries.

The reality on the ground is bleak. Floods in Pakistan displaced thousands and affected more than 33 million people in 2023. That’s ten times more than the total population of Los Angeles where, when the recent wildfires struck, 170,000 people had to be evacuated.

Around the world, climate movements continue. Law suits that demand climate action are transforming governance. High-level negotiations like the UN’s annual climate summit carry on seeking progress, although the processes could be improved to accelerate change.

What can Davos do? World leaders need to look at how wealth and power can be redistributed (reparations for climate damages is one way to do this) and low-income, climate-vulnerable nations can be better represented in global decision-making.

Without this kind of change, there’s a risk climate action will perpetuate the same structural imbalances that first enabled environmental exploitation. Only by tackling both climate injustice and economic inequality together can the world prevent further climate disasters and ensure a more equitable future.


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Susan Ann Samuel, PhD Candidate, School of Politics and International Studies, University of Leeds

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

Continue ReadingHow global inequality hinders climate action