“Atmospheric rivers” are bringing rain to the frozen slopes of the West Antarctic ice sheet, hitting the ice shelves that play a major role in holding back rapidly retreating glaciers.
In a new study, my colleagues and I show how rain is occurring in sub-zero temperatures due to these “rivers in the sky” – long, narrow plumes of air which transport heat and moisture from the tropics to the mid-latitudes and poles.
Rain in Antarctica is significant, not only because it is a stark indicator of climate change, but because it remains an under-studied phenomenon which could impact ice shelves.
Ice shelves in Antarctica are important gatekeepers of sea level rise.
They act as a buffer for glaciers that flow off the vast ice sheet, slowing the rate at which ice is released into the ocean.
In the study, we explore the causes of rain falling on ice shelves in the Amundsen Sea embayment region, which stand in front of the critically important Thwaites and Pine Island glaciers.
Researchers have warned the collapse of ice shelves in this region could trigger the loss of the entire West Antarctic ice sheet over several centuries.
Rivers in the sky
Atmospheric rivers are typically associated with bringing extreme rainfall to the mid-latitudes, but, in the frigid Antarctic, they can deliver metres of snow in just a few days.
In West Antarctica, atmospheric rivers deliver a disproportionate quantity of the year’s snowfall. Research shows they account for around 13% of annual snowfall totals, despite occurring on just a few days per year.
But what makes atmospheric rivers in Antarctica so interesting is that snow is only part of the story. In extreme cases, they can also bring rain.
To explore how extreme precipitation affects the Amundsen Sea embayment region, we focused on two events associated with atmospheric rivers in 2020. The summer case took place over a week in February and the winter case over six days in June.
We used three regional climate models to simulate the two extreme weather events around the Thwaites and Pine Island ice shelves, then compared the results with snowfall observations.
During both the winter and summer cases, we find that atmospheric rivers dumped tens of metres of snow over the course of a week or so.
Meanwhile, the quantities of rain driven by these events were not insignificant. We observed up to 30mm of rain on parts of the Thwaites ice shelf in summer and up to 9mm in winter.
A mountain to climb
Antarctica’s cold climate and steep, icy topography make it unique. It also makes the region prone to rain in sub-zero temperatures.
The first reason for this is the foehn effect, which is when air forced over a mountain range warms as it descends on the downward slope.
Commonly observed across Antarctica, it is an important cause of melting over ice shelves on the Antarctic peninsula, the northernmost point of the continent.
When air passes over the mountainous terrain of the West Antarctic ice sheet during atmospheric river events, temperatures near the surface of the ice shelves can climb above the melting point of 0C.
This can accentuate the formation of rain and drizzle that stays liquid below 0C – also known as “supercooled drizzle”.
Another factor which leads to liquid drizzle, rather than snow, in sub-zero conditions is a lack of dust and dirt – particles which are usually needed to trigger the formation of ice crystals in clouds.
In the pristine Antarctic, these particles – which act as “ice nuclei” – are few and far between. That means that pure liquid water can exist even when temperatures are below 0C.
The origins of rain over ice shelves
It is easy to assume that rain that reaches the surface in Antarctica is just snow that has melted after falling through a warm layer of air caused by the foehn effect. Indeed, this is what we initially supposed.
But our research shows that more rain reaches the surface of Antarctica when the air near the ground is within a few degrees of freezing.
At times when the foehn effect is strongest, there is often little or no rainfall, because it evaporates before it gets a chance to reach the surface.
However, we saw rain falling well above the warm layer of air near the surface, where temperatures were universally below 0C – and, in some cases, as low as -11C.
Rare rain
Rain in Antarctica is a rare occurrence. The region’s normally frigid temperatures mean that most precipitation over the continent falls as snow.
However, exactly how rare rain is in the region remains relatively unknown, because there are virtually zero measurements of rainfall in Antarctica.
There are a number of reasons for this – rain falls infrequently, and it is very difficult to measure in the hostile Antarctic environment.
Our results show that extreme events such as atmospheric rivers can bring rain. And it is likely that rain will become a more common occurrence in the future as temperatures rise and extreme weather events occur more frequently.
However, until rain starts being measured in Antarctica, scientists will have to rely entirely on models to predict rain, as we did in this research.
It is also not yet known exactly how rain could impact ice in Antarctica.
We do know that rain falling on snow darkens the surface, which can enhance melting, leading to greater ice losses. Meanwhile, rain that refreezes in the snowpack or trickles to the base of the ice can change the way that glaciers flow, impacting the resilience of ice shelves to fracture.
So, if we want to understand the future of the frozen continent, we need to start thinking about rain too. Because while rain may be rare now, it may not be for long.
The post Guest post: How atmospheric rivers are bringing rain to West Antarctica appeared first on Carbon Brief.
Guest post: How atmospheric rivers are bringing rain to West Antarctica
China’s carbon dioxide (CO2) emissions fell by 3.1% in the third quarter of 2026, as the Hormuz crisis continued to hit oil demand and coal use also dropped.
This guest post is by:
Lauri Myllyvirta, lead analyst at the Centre for Research on Energy and Clean Air
This was the largest quarterly reduction since the 2022 Covid lockdowns and means that China’s CO2 emissions have now fallen by an estimated 0.5% in the year to date.
The new analysis for Carbon Brief, based on official figures and commercial data, shows that coal use fell by 3% year-on-year in the third quarter of 2026, while oil was down 4%.
The main drivers were a fall in power-sector coal consumption, a continued sharp reduction in transport oil consumption and slowing growth in the coal-to-chemical industry.
The sharp decline in China’s CO2 emissions extends a “flat or falling” trend that began in March 2024 and has now lasted more than two years, as shown in the figure below.
The outlook for China’s CO2 emissions depends on the balance between rising energy demand, clean-energy growth and the government response to a GDP slowdown.
Decline drivers
Key drivers of the fall in CO2 in the third quarter of 2026 included a 3.3% drop in coal-power generation, after demand growth slowed and the amount of “wasted” wind and solar fell.
Power generation from solar, wind and nuclear increased by 110 terawatt hours (TWh) year-on-year, more than twice as much as the growth in total electricity demand. This added clean-power generation equal to Germany’s total power output in the same time period.
The fall in coal-power output and CO2 emissions came despite the fact that China continues to build new coal-power capacity at near-record rates. This means that average running hours for coal plants are falling even faster than total generation, eroding their profits.
Meanwhile, transport oil consumption continued to fall sharply, down 9% year-on-year in the third quarter of 2026. Electric vehicles (EVs) continued to gain market share, hitting a record 67% of passenger car sales and 50% of heavy trucks in September.
The amount of electricity used by EVs grew by 53%, much faster than the number of EVs on the road, showing increased usage of the existing fleet in preference to fuelled vehicles.
Elsewhere, growth in the coal-to-chemical industry continued to slow down in the third quarter of 2026. The sector has been a key source of emissions growth, but high coal prices have weakened profitability and higher output prices hurt downstream demand.
Finally, CO2 emissions from cement and steel production continued to fall in the third quarter, as the contraction in construction volumes accelerated.
Outlook for emissions
Energy consumption growth has been falling after a period of exceptionally high growth during Covid, while clean-power growth has been robust.
This makes it likely that the growth in clean-power generation will exceed total energy demand growth this year, maintaining the structural fall in fossil-fuel use.
Looking ahead, this balance also relies on progress in removing barriers to new solar and wind power being added to the grid, which result in some clean electricity being “wasted”.
The recent slowdown in energy demand growth is partly – but not fully – explained by exceptionally mild weather in the third quarter.
Another key factor is weaker GDP growth. Since reported GDP growth remains within target, however, there is reduced pressure for further stimulus policies.
The focus of the economic stimulus announced to date is “six networks”, which includes the power grid and the transportation network.
These networks are highly relevant for energy and emissions – and they are already covered by policies that emphasise “green” and zero-carbon solutions.
The post Analysis: China’s quarterly CO2 falls 3% in largest drop since Covid appeared first on Carbon Brief.
Analysis: China’s quarterly CO2 falls 3% in largest drop since Covid
Climate Change
Coles, Woolworths grilled as beef buyers receive fail grade on new deforestation scorecard
MELBOURNE, Friday 6 November 2026 — As Coles holds its Annual General Meeting today, Greenpeace Australia Pacific has branded the major supermarkets with a fail grade on their commitment to source deforestation-free beef, with an updated scorecard revealing none of the major beef buyers are following through on forest sustainability commitments.
It comes after Woolworths’s AGM last week where the board copped a grilling by environmentalists and shareholders over its failed sustainability commitments. Both Coles and Woolworths committed to eliminating deforestation in their supply chains by the end of 2025, but a year past the deadline, neither company could guarantee that their beef was not sourced from deforested pastures.
From outside the Coles AGM, Adele Chasson, Nature Policy Lead at Greenpeace Australia Pacific, said:
“This is a report card Coles and Woolworths should be ashamed to take home. While all major beef buyers had promised to take deforestation off the shelves, none of them followed through. Shareholders and the public demanded answers from Woolworths last week and from Coles today, and we will continue to hold their feet to the fire on their promises.
“Beef is the leading cause of deforestation in Australia, and Coles and Woolworths keep putting off action while koalas continue losing their homes. Aussies must be able to get their groceries without having to worry if their dinner is contributing to the bulldozing of forests or driving extinction of iconic Australian animals.
“Without strong, rapid implementation plans, these companies continue with business as usual, flying in the face of Australia’s deforestation crisis. Big beef buyers like Coles and Woolworths must stop the bulldozers now, make good on their sustainability promises and play their part in stopping Australian forest destruction.”
The scorecard assesses how eight of Australia’s largest beef buyers stack up against a conversion and deforestation-free target. It charts whether the major supermarkets, Aldi, McDonalds, Hungry Jacks, Teys, Metcash/IGA and JBS are taking proper action to end Australia’s deforestation crisis. They all failed.
-ENDS-
Media contact: Kimberley Bernard on 0407 581 404 or kbernard@greenpeace.org
Coles, Woolworths grilled as beef buyers receive fail grade on new deforestation scorecard
Özgür Özel is the leader of Turkey’s main opposition “New Party” and a member of parliament from Manisa.
The world is running out of time to deliver on the Paris Agreement. The UN Environment Programme’s latest Emissions Gap Report concludes that the chance of keeping warming below 1.5C without overshooting it is gone. Even if every country delivers its current national pledges, the planet is heading for about 2.6C of warming this century.
This is the backdrop as governments and their leaders gather in Antalya for COP31, ten years after the Paris Agreement took effect. Turkey lies in the Mediterranean, one of the regions most exposed to climate change, and hosting the summit is a real opportunity.
It is also a responsibility, and that responsibility begins at home. The world does not lack targets. What it has lacked – almost everywhere – is delivery. If Antalya is remembered for anything, it should be for shifting the focus from what countries promise to what they actually do.
For many people in Turkey, the climate crisis is already part of daily life. In 2021, forests in Manavgat, a district of Antalya, burned for more than a week. Last year, wildfires forced more than 50,000 people from their homes around the western coast city of Izmir. This October, Istanbul had its heaviest rainfall in more than 80 years, with the floods killing at least eight people.
COP31 Briefing: What to expect from the Antalya climate summit?
Electrification, the fossil fuel transition, adaptation to rising impacts, climate science and trade are key themes as governments gather for COP31 in TürkiyeBrazil’s fossil fuel roadmap sketches out first global timetable
The COP30 presidency’s voluntary timetable asks countries to plan first, then build up clean energy – only turning to oil and gas supplies from 2031
Measurable outcomes
Two weeks of climate negotiations cannot deliver everything that is needed to resolve the crisis, but COP31 can push for a few things that can be measured. The first is a voluntary fossil-fuel transition roadmap, with national milestones for 2030 and 2035 reported in the same format every year.
The second is a stronger commitment to protecting forests, with progress tracked over time. The third is yearly reporting on progress towards the agreed $1.3 trillion a year in climate finance by 2035, backed by a financial roadmap.
On adaptation, the indicators agreed in Belém should become funded national plans. By COP32, we should be able to see how many countries have an adaptation plan and the financial commitment behind each one.
Regional resilience partnership
The summit also has an unusual shape. Turkey hosts, Australia leads the negotiations, and the Pacific island nations play a central role. Climate diplomacy now sits at the centre of energy security, trade and development, and Turkey, which bridges developed and developing economies, is well placed to help build consensus between them. The lasting value of its presidency will depend on the practical partnerships it leaves behind.
One such partnership could connect two very different regions. On a map, the Mediterranean and the Pacific seem to have little in common, but their problems look similar: eroding coastlines, salt creeping into aquifers, failing harvests, fishing towns with fewer fish.
Turkey and Australia could launch a Mediterranean–Pacific Climate Resilience Partnership, linking coastal cities, scientists, institutions including development banks and island governments. It does not need a new bureaucracy. It can start with a few projects: shared satellite data and early-warning systems, better coastal flood defences, and trials of water-saving farming in the communities most at risk. What matters is visible results on the ground, not a ceremony.
Turkey’s track record
Turkey does have progress to point to. It has committed to net zero by 2053, and its solar and wind capacity has grown fast. The sunshine, the wind and the industrial base are all there. But the long-term direction of the energy mix is still unclear.
Turkey also signed the Glasgow Leaders’ Declaration on Forests and Land Use at COP26, pledging to halt and reverse forest loss by 2030. With four years left, COP31 is a chance to show how that promise will be kept.