Greenland is closing in on three decades of continuous annual ice loss, with 1995-96 being the last year in which the giant ice sheet grew in size.
With another melt season over, Greenland lost 105bn tonnes of ice in 2024-25.
The past year has seen some notable events, including ongoing ice melt into the month of September – well beyond the end of August when Greenland’s short summer typically draws to a close.
In a hypothetical world not impacted by human-caused climate change, ice melt in Greenland would rarely occur in September – and, if it did, it would generally be confined to the south.
In this article, we explore how Greenland’s ice sheets fared over the 12 months to August 2025, including the evidence that the territory’s summer melting season is lengthening.
(For our previous analyses of Greenland’s ice cover, see coverage in 2024, 2023, 2022, 2021, 2020, 2019, 2018, 2017, 2016 and 2015.)
Surface mass balance
The seasons in Greenland are overwhelmingly dominated by winter.
The bitterly cold, dark winter lasts up to ten months, depending on where you are. In contrast, the summer period is generally rather short, starting in late May in southern Greenland and in June in the north, before ending in late August.
Greenland’s annual ice cycle is typically measured from 1 September through to the end of August.
This is because the ice sheet largely gains snow on the surface from September, accumulating ice through autumn, winter and into spring.
Then, as temperatures increase, the ice sheet begins to lose more ice through surface melt than it gains from snowfall, generally from mid-June. The melt season usually continues until the middle or end of August.
Over this 12-month period, scientists track the “surface mass balance” (SMB) of the ice sheet. This is the balance between ice gains and losses at the surface.
To calculate ice gain and losses, scientists use data collected by high-resolution regional climate models and Sentinel satellites.
The SMB does not consider all ice losses from Greenland – we will come to that later – but instead provides a gauge of changes at the surface of the ice sheet.
According to our calculations, Greenland ended the year 2024-25 with an overall SMB of about 404bn tonnes. This is the 15th highest SMB in a dataset that goes back 45 years, exceeding the 1981-2010 average by roughly 70bn tonnes.
This year’s SMB is illustrated in the maps and charts below, based on data from the Polar Portal.
The blue line in the upper chart shows the day-to-day SMB. Large snowfall events become visible as “spikes”. The blue line in the lower chart depicts the accumulated SMB since 1 September 2024. In grey, the long-term average and its variability are shown. For comparison, the red line shows the record-low year of 2011-12.
The map shows the geographic spread of SMB gains (blue) and losses (red) for 2024-25, compared to the long-term average.
It illustrates that southern and north-western Greenland had a relatively wet year compared to the long-term average, while there was mass loss along large sections of the coast, in particular in the south-west. The spikes of snow and melt are clearly visible in the graphs on the right.
Lengthening summer
Scientists have traditionally pinned the start of the “mass balance year” in Greenland to 1 September, given that this is when the ice sheet typically starts to gain mass.
However, evidence has started to emerge of a lengthening of the summer season in Greenland – as predicted some time ago by climate models.
The start of the 2024-25 mass balance year in Greenland saw ice melt continuing into September. This included a particularly unusual spike in ice melt in the northern part of the territory in September as well as all down the west coast.
In a world without human-caused climate change, ice melt in September would be very rare – and generally confined to the south.
Greenland also saw an early start to the summer melt season in 2025. The onset of the melting season, defined as the first of at least three days in a row with melting over more than 5% of the ice sheet, was on 14 May. This is 12 days earlier than the 1981-2025 average.
The maps below show the extent of melt (red shading) across the ice sheet on 24 September 2024 (left) and 20 May 2025 (right). The blue lines in charts beneath show the percentage melt in 2024 (left) and 2025 (right), up to these dates, compared to the 1981-2010 average (grey).
The melt season began with a significant spike of melting across the southern part of the ice sheet. This happened in combination with sea ice breaking up particularly early in north-west Greenland, allowing the traditional narwhal hunt to start much earlier than usual.
Surface melt
The ablation season, which covers the period in the year when Greenland is losing ice, started a little late. The onset of the season – defined as the first of at least three days in a row with an SMB below -1bn tonnes – began on 15 June, which is two days later than the 1981-2010 average.
Overall, during the 2025 summer, a remarkably large percentage of the ice sheet was melting at once. This area was larger than the 1981-2010 average for three and a half months (mid-June to end of September).
In mid-July, melting occurred over a record area. For three days in a row, melting was present over more than 80% of the area of the ice sheet – peaking at 81.2%. This is the highest value in our dataset, which started in 1981.
The red shading in the maps below shows the extent of melting across Greenland on 19 July (left) and 30 September (right) 2025. The charts beneath show the daily extent of melting through 2025 (blue line), up to these dates, compared to the 1981-2010 average.
Snowfall
However, the SMB is not just about ice melt.
There was a lack of snowfall in the early winter months (September to January), particularly in south-east Greenland, which is typically the wettest part of the territory. The months that followed then saw abundant snow, which brought snowfall totals up closer to average by the start of summer.
A cold period at the end of May and in June protected the ice sheet from excessive ice loss. Melt then continued rather weakly until mid-July.
This was followed by strong melting rates in the second half of July and again in mid-August.
Overall, with both ice melt and snowfall exceeding their historical averages for the year as a whole, the SMB of the Greenland ice sheet ended above the 1981-2010 average.
These increases in snowfall and melt are in line with what scientists expect in a warming climate. This is because air holds more water vapour as it warms – leading to more snowfall and rain. Warmer temperatures also lead to more ice melt.
Total mass balance
The surface mass balance is just one component of the “total” mass balance (TMB) of the Greenland ice sheet.
The total mass balance of Greenland is the sum of the SMB, the marine mass balance (MMB) and basal mass balance (BMB). In other words, it brings together calculations from the surface, sides and base of the ice sheet.
The MMB measures the impact of the breaking off – or “calving” – of icebergs, as well as the melting of the front of glaciers where they meet the warm sea water. The MMB is always negative and has increased towards more negative values over the last decades.
BMB refers to ice losses from the base of the ice sheet. This makes a small negative contribution to the TMB.
(The only way for the ice sheet to gain mass is through snowfall.)
The continued mass loss observed in Greenland is primarily due to a weakening of the SMB – caused by rising melt combined with insufficient compensation of lost ice through snowfall.
The figure below shows how much ice the Greenland ice sheet has lost (red) going back to 1987, which includes the SMB (dark blue), MMB (mid blue) and BMB (light blue). The analysis, which uses data from three models, is based on 2021 research published in Earth System Science.
Despite a relatively high SMB, high calving rates meant that Greenland lost 105bn tonnes of ice over the 12-month period.
This means that 2024-25 was the 29th year in a row with a Greenland ice sheet overall mass loss. As the chart shows, Greenland last saw an annual net gain of ice in 1996.
Satellite data
The mass balance of the Greenland ice sheet can also be measured by looking at the Earth’s gravitational field, using data captured by the Grace and Grace-FO satellite missions – a joint initiative from NASA and the German Aerospace Center.
The Grace satellites are twin satellites that follow each other closely at a distance of about 220km, which is why they are nicknamed “Tom and Jerry”. The distance between the two depends on gravity – which is, in turn, related to changes in mass on Earth, including ice loss.
Therefore, the distance between the two satellites, which can be measured very precisely, can be used to calculate loss of mass from the Greenland ice sheet.
Overall, the satellite data reveals that Greenland’s ice sheet lost around 55bn tonnes of ice over the 2024-25 season.
There is reasonably good agreement between the Grace satellite data and the model data, which, as noted above, finds that 105bn tonnes of ice was lost in Greenland over the same period.
However, the alignment of the two datasets – which are fully independent of each other – becomes more clear once a longer time period is considered.
In the 22-year period between April 2002 and May 2024, the Grace data shows that Greenland lost 4,911bn tonnes of ice. The modelling approach, on the other hand, calculates that 4,766bn tonnes of ice was lost.
The figure below shows gain and loss in the total mass of ice of the Greenland ice sheet, calculated using Grace satellite measurements. It reveals that, over the past 23 years, there has been mass loss in the order of several metres along the coasts of Greenland, with the most significant losses seen on the western coast. Over the central parts of the ice sheet, there has been a small mass gain.
The lower figure shows the contribution of Greenland mass change to sea level rise over the last 23 years, according to the satellite data. It illustrates that more than 5,000bn tonnes of ice have been lost over the time period – contributing to roughly 1.5cm of sea level rise.
Warm over Europe and North America, cool over Greenland
As always, the weather systems across the northern hemisphere play a key role in the melt and snowfall that Greenland sees each year.
As in previous years, multiple heatwaves were observed in southern Europe and North America over the summer of 2025.
And, just like in 2024, there was only modest heat in northern Europe – with the notable exception of Arctic Scandinavia – with a comparably cool and rainy July followed by a warmer and sunnier August.
The high-pressure weather systems that bring heatwaves have a wide-ranging impact on weather extremes across the northern hemisphere.
Strong blocking patterns over North America and Europe were repeatedly present in the course of the summer of 2025. In such a blocked flow, the jet stream – fast-moving winds that blow from west to east high in the atmosphere – is shaped like the Greek capital letter Omega (Ω).
The jet stream bulged up to the north over Canada and northern Europe. West and east of these ridges, low pressure troughs were found at both “feet” of the Omega. One of these troughs was located over Greenland (top left panel in next figure).
This resulted in widespread heat near the cores of these high-pressure systems, fuelling fires in several countries, including large wildfires in Canada. Smoke from these wildfires reached Greenland and Europe in late May.
Unlike in previous years, no heavy precipitation events were observed near the “feet” of the Omega.
If the Omega pattern is displaced by half a wavelength, the opposite – warm over Greenland, with cool continents – is also possible.
This circulation pattern occurred in August 2025 and is shown in the top right panel of the figure below. The bottom panel depicts the large temperature variability in May 2025.
The post Guest post: How the Greenland ice sheet fared in 2025 appeared first on Carbon Brief.
Climate Change
Threads of Earth’s Underground Fungal Networks Are Long Enough to Reach Beyond the Solar System
For the first time ever, researchers have quantified the length and mass of arbuscular mycorrhizal fungal networks globally and mapped the ecosystems where they are densest.
Hidden underground around the world lie 110 quadrillion kilometers of arbuscular mycorrhizal fungal networks—webs of ultra-thin threads that, if connected in a single line, would stretch almost a billion times thge distance between the Earth and the sun, according to new research published in Science on Thursday.
Threads of Earth’s Underground Fungal Networks Are Long Enough to Reach Beyond the Solar System
The number of journalists registered to attend the annual climate negotiations in Bonn has declined this year, as climate reporters have been let go and media coverage of climate issues falls around the world.
Data from UN Climate Change, which runs the two weeks of talks, shows that just 135 media representatives have signed up to attend. Climate Home News analysis of previous data shows this is the lowest figure since 2021, when COVID-19 restrictions limited travel and the Bonn talks were held in a hybrid format to enable online participation.
The number of journalists that actually attend the talks will not be known until later this month but is typically significantly less than are registered. Press conferences, held back-to-back each day by campaign groups, have been sparsely attended in the first few days and often filled mainly with climate campaigners and researchers rather than journalists.
Alexandra Endres, a reporter for German-language website Table Briefings, told Climate Home News in Bonn there are fewer German journalists covering the conference in-person. “I think it is important to have more journalists covering the negotiations because when the climate coverage increases, the interest of the public grows,” she said.
Media outlets that have registered fewer journalists than previous years, or no journalists, include global heavyweights like Reuters, Bloomberg and the BBC, as well as German outlets like Deutsche Welle and ZDF television, and specialist publications like business information service Argus and climate broadcaster We Don’t Have Time.
Activist Harjeet Singh, who is in Bonn advising the Fossil Fuel Treaty Initiative, said that “the empty press seats here in Bonn are a warning signal. While the world’s gaze is often fixed on the annual COP summits, the real-world consequences of the climate crisis—from financing the fossil fuel transition to protecting vulnerable populations—are being shaped, or ignored, in these mid-year negotiations right now.”
“Journalists are the essential eyes and ears of the public,” he said. “We need them to shine a light on these rooms: hold negotiators accountable, defend the principles of equity and historical responsibility, and ensure that ‘technical’ negotiations do not become an excuse for delay.”
UN Climate Change said they could not comment on the situation at this point in the Bonn talks.
Climate coverage is falling
Outside of Bonn and the official UN climate negotiations, coverage of climate change is falling to lows not seen since the start of the COVID-19 pandemic, according to analysis of newspapers and television reporting conducted by the Media and Climate Change Observatory (MECCO).
MECCO’s head Max Boykoff told Climate Home News that climate coverage in the first five months of 2025 was 35% down on the same period of 2025 and 41% less than in 2021. New analysis by the Yale Programme on Climate Change Communication found a similar fall in climate coverage in 2026.
Boykoff said media attention has been drawn away from climate change to issues like the Iran war and now the World Cup getting underway in North America.
While both stories have climate implications, he said, the media have “failed to connect the dots” on the conflict in the Middle East, with coverage focusing on the politics, air strikes and violence of the war. “Reporters have been pulling up short,” he said.
He added that since 2025 there have been cuts to climate teams at US outlets like the Washington Post, CBS, National Public Radio and the Los Angeles Times. On top of this, the Thomson Reuters Foundation’s Context website has been shut down and Politico recently folded specialist environmental outlet E&E News into its broader energy coverage.
Mark Hertsgaard, head of global journalism collaboration Covering Climate Now, also said that fewer reporters at Bonn is “part of a larger pattern”. He said no US television network sent reporters to the recent Santa Marta conference on transitioning away from fossil fuels “and as a result they missed covering what turned out to be a landmark development in the climate story”.
-
COP31 leaders unveil global targets, with spotlight on electrification
Co-hosts Türkiye and Australia want countries to sign on to global targets in three of their priority areas for this year’s COP climate negotiations -
Bonn Bulletin: Tackling climate crisis is “hardest” challenge ever, Stiell says
The June Climate Meetings open with a reminder to delegates of the tough but ever-clearer imperative of shifting away from fossil fuels to clean energy
“No one can know if the Bonn talks will yield something similar until the [they] actually take place and conclude. But the fewer journalists that are on the scene, the less the world’s people and policymakers will know about that. And that’s a problem,” he said.
Media may also have been put off from attending by a new registration system which is more complicated, especially for freelance journalists. In addition, the rise in jet fuel prices has made travelling by plane to Bonn much more expensive than last year and reporters from many developing countries continue to face hurdles getting visas to enter the Schengen area, of which Germany is part.
Diego Arguedas Ortiz, who led the Oxford Climate Journalism Network from 2022 until it was shut down by the Reuters Institute for the Study of Journalism in 2025, said journalists can’t cover the talks so well remotely.
While press conferences, plenaries and open negotiating sessions are broadcast for the public to watch on the UNFCCC’s website, Ortiz said relying solely on this means “you miss the interviews in the hall”.
“You can´t catch scientists and ministers as they leave the rooms. And the audience is back home suffering. Because audiences are relying on reporters and editors to explain how these seemingly abstract negotiations have daily implications for them,” he explained.
The post Fewer journalists register for Bonn talks, as cuts to climate reporting bite appeared first on Climate Home News.
Fewer journalists register for Bonn talks, as cuts to climate reporting bite
Despite skyrocketing demand driven by data center development, the industry says it is not the cause of increasing costs for consumers.
Advocates for lower electricity prices in Pennsylvania said Wednesday their goals can be achieved by requiring large-load users like data centers to supply their own power rather than taking it from the grid, by reducing utility profits and by speeding up the interconnection of new clean-energy projects.
Pennsylvania Activists Urge Lawmakers to Help Curb Soaring Electric Bills
-
Climate Change10 months ago
Guest post: Why China is still building new coal – and when it might stop
-
Greenhouse Gases10 months ago
Guest post: Why China is still building new coal – and when it might stop
-
Greenhouse Gases2 years ago嘉宾来稿：满足中国增长的用电需求 光伏加储能“比新建煤电更实惠”
-
Climate Change2 years ago嘉宾来稿：满足中国增长的用电需求 光伏加储能“比新建煤电更实惠”
-
Climate Change2 years ago
Bill Discounting Climate Change in Florida’s Energy Policy Awaits DeSantis’ Approval
-
Renewable Energy8 months agoSending Progressive Philanthropist George Soros to Prison?
-
Carbon Footprint2 years agoUS SEC’s Climate Disclosure Rules Spur Renewed Interest in Carbon Credits
-
Greenhouse Gases11 months ago
嘉宾来稿：探究火山喷发如何影响气候预测