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Arctic sea ice has reached its peak extent for this winter, clocking in as the joint-smallest in a satellite record going back almost half a century.
Provisional data from the US National Snow and Ice Data Center (NSIDC) shows that sea ice extent peaked at 14.29m square kilometres (km2) on 15 March.
This is slightly smaller than the previous record for the annual maximum – set just last year – but it counts as a statistical tie, the NSIDC says.
The annual maximum is a key marker in a cycle that sees sea ice extent grow through the cold, dark winter, before melting in spring and summer to a yearly minimum.
The joint record marks a “very alarming” winter for Arctic sea ice, Dr Zack Labe – a scientist at Climate Central – tells Carbon Brief.
And there is more “grim news”, Labe says, as the thickness of the ice is near record lows – meaning that Arctic sea ice is “entering late winter in one of its weakest states in the satellite record”.
‘Unusually warm’
The past six months has seen Arctic sea ice extent “at record or near-record lows, alongside unusually warm conditions” across much of the region, says Dr Lettie Roach, a polar climate scientist at the Alfred Wegener Institute.
These go “hand in hand”, Roach tells Carbon Brief, as “warmer air and ocean temperatures help melt the ice and with less ice, the ocean absorbs more heat, which further speeds up warming”.
The chart below shows Arctic sea ice extent in 2025 (dark blue) and 2026 (red) so far. For comparison, the chart shows decadal averages (dotted lines) as well as 2012 (mid blue), the year of the smallest summer sea-ice minimum on record.
Recent months have seen “strong temperature contrasts” over the northern hemisphere, continues Roach:
“In addition to large parts of the Arctic, temperatures were unusually warm in the western US, southern Europe and eastern Eurasia, while northern Eurasia, northern Canada and the north-eastern US experienced unusually cold conditions.
“That’s linked to a more ‘wavy’ jet stream, which can push cold Arctic air southward while bringing warmer air into the Arctic.”
These conditions have contributed to “particularly bad” sea ice levels in regions such as the Sea of Okhotsk, Baffin Bay, Barents Sea and Kara Sea, says Labe. He adds that “one of the only regions with more sea ice relative to normal is across the eastern Bering Sea around Alaska”.
‘Long-term downward trend’
This year’s winter peak is the latest milestone in the “long-term downward trend we’ve observed” in Arctic sea ice since the start of satellite observations in the late 1970s, says Roach.
According to the NSIDC, the 2026 maximum extent is 1.36km2 smaller than the 1981-2010 average. That is “equivalent to about twice the size of Texas”, the centre says.
Arctic sea ice is “not just shrinking in extent”, says Roach, it is “also much thinner and more fragile than it used to be”.
Labe notes the “grim news” that sea ice “near the north pole has had record-low thickness for several months now”, adding:
“In February, total Arctic sea ice volume was the second lowest on record. Taken together, Arctic sea ice is entering late winter in one of its weakest states in the satellite record.”
While there is a “lot of year-to-year variability due to natural fluctuations in the atmosphere and ocean”, this long-term decline is “mainly due to human-caused climate change”, says Roach.
Labe adds:
“Human-caused climate change is completely reshaping the polar environment and this is already having wide-ranging consequences.”
The chart below shows the annual winter maxima (blue) and summer minima (red) since the start of the satellite record.
The chart highlights that the annual maximum has “shown a relatively steady decline over the past 40 years, with the [previous] record low occurring as recently as last year”, says Dr Mika Rantanen, a researcher at the Finnish Meteorological Institute.
This is in “sharp contrast to the annual minimum, where the record [low] still dates back to 2012”, he tells Carbon Brief. This indicates that the summer minimum is “more prone” to yearly ups and downs of natural variability, he explains.
It is for this reason that “it is still too early to say” what the low winter peak means for the forthcoming summer melt season as “regional weather can change quickly”, adds Labe:
“But winter of 2025-26 is another clear signal of just how fast the Arctic is shifting.”
‘Average’ Antarctica
At the Earth’s other pole, sea ice around Antarctica has been melting through the southern-hemisphere summer.
It reached its annual minimum extent of 2.58m km2 on 26 February, the NSIDC says, placing this year as the 16th smallest on record.
For most of the summer, Antarctic sea ice has been “below average”, Dr Clare Eayrs, a postdoctoral researcher at the Korea Polar Research Institute (KOPRI), tells Carbon Brief. However, she continues:
“That changed in January and February, when a shift in surface winds slowed the retreat. Southerly winds over the Weddell Sea pushed existing sea ice northward, keeping coverage higher than expected in that region, while sea ice cover in the Bellingshausen Sea remained low.”
These winds were mostly “redistributing ice rather than new ice forming in these regions”, Eayrs notes:
“This was enough to keep the summer sea ice coverage much closer to average than in the previous four years…It is a reminder that where a season starts does not always determine where it ends.”
Recent years have seen a series of record-low extents in the sea ice that surrounds Antarctica.
While it is “likely” that climate change is influencing Antarctic sea ice, scientists “remain uncertain about the extent and precise mechanisms involved”, says Eayrs:
“This uncertainty is itself an important part of the story. Antarctic sea ice has always been highly variable and its variability has masked any emerging long-term signal for much of the satellite era.”
However, recent research points to a recent “structural change” in Antarctica’s sea ice system, Eayrs notes. This is marked by a greater persistence of low sea ice and a “weaker tendency for the system to return to its earlier mean state”.
In other words, says Eayrs, “when sea ice drops to unusual lows, it no longer bounces back as readily as it once did”.
The post ‘Very alarming’ winter sees Arctic sea ice hit record-low for second year running appeared first on Carbon Brief.
‘Very alarming’ winter sees Arctic sea ice hit record-low for second year running
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An older teaching about land acknowledgement
As I have come to understand the spirit and intention of land acknowledgement, I often return to fond memories of my grandmother and her words of wisdom. She taught that the health of the places we call home comes first, because the wellbeing of the people depends on it.
In her teaching, land acknowledgement began with the land. Long before it became a paragraph read at the start of a meeting, it was a way of recognizing a homeland: its waters, its species, its seasons, and the spirit that revealed whether the place was well.
Her teaching echoes a practice found across many Indigenous Nations. Haudenosaunee gatherings, for example, have long opened with the Ohén:ton Karihwatéhkwen, the Thanksgiving Address, often translated as “the words that come before all else.” The speaker greets and gives thanks to the people, the earth, the waters, the plants, the animals, the winds, the sun, the moon and the stars. Only after everything that sustains life has been acknowledged does the gathering turn to its own business.
That order changes what an acknowledgement is for. Its purpose was to share the story of a place with neighbours and to draw them into the work of tending it. People entered the story second, as the ones responsible for what had just been named.
Understood this way, an acknowledgement does more than open a meeting. It asks us to reconsider where we stand, and what we owe the ground beneath us.
Nations among nations
In her teaching, people are one nation among many. The salmon are a nation. So are the cedars, the bison, the medicine plants, and the pollinators. Each belongs to a place, carries its own responsibilities, and offers gifts no other nation can give.
This idea of kinship runs through many Indigenous philosophies. The phrase “all my relations,” heard in ceremonies and gatherings across Turtle Island, is a reminder that family extends beyond people to the animals, plants, waters and lands that make life possible. Some Indigenous languages carry the same understanding in their grammar, speaking of many plants, animals and natural forces as living beings rather than objects.
Sovereignty, understood through this relationship, is a kind of standing more than a form of control. Each nation belongs fully to its place and carries its share of that place’s life. No nation thrives alone, and none thrives by taking over the whole.
The land is also the source of instruction. Over generations, people watched how a river valley or a stretch of prairie kept itself well: who arrived when, who fed whom, and how much could be taken before the giving stopped. In my grandmother’s telling, those observations became instructions, and those instructions helped shape law and protocol. They guided when to harvest, where to camp, how to enter a neighbour’s territory, and what was owed in return.
Indigenous legal scholars today often describe this as law that comes from the land itself, learned by watching how living systems sustain one another. A plainer name for it is knowing how to live somewhere.
The host and the guest
One of the clearest teachings in this understanding of the world is the relationship between host and guest. My grandmother invited us to recognize that relationship in the lives of plants and animals.
A host prepares the place before anyone arrives. A beaver family dams a stream, and the pond becomes a home for fish, frogs, birds and plants. A fallen tree becomes a nurse log, feeding the next generation of seedlings as it returns to the soil.
A host offers first. A flowering plant sets out nectar. A berry bush ripens fruit. These provisions come in their own season, not whenever a visitor happens to want them.
A host also makes its presence known. Birdsong, scent and the marks left along a trail tell newcomers that a place is already inhabited. The visitor does not arrive in an empty world.
The guest has responsibilities too. A guest attends to the season and to what the place can offer. A guest does not assume that everything within reach is theirs to take. A guest leaves something that helps sustain the relationship.
A bee takes nectar and carries pollen. Read through this teaching, that exchange offers an image of visiting well: receiving a gift while helping the host continue its life.
Many Indigenous harvesting protocols carry the same ethic into daily practice: ask before taking, take only what is needed, offer thanks, and leave enough for others and for the plant or animal to recover.
None of this suggests that every relationship in nature is peaceful or generous. These are ways of seeing responsibilities that people can learn to carry.
Everyone is both
No being is only a host or only a guest.
A tree makes room for other life while depending on soil, water, sunlight, fungi, and relationships beyond itself. People, too, may welcome others into their homes while remaining dependent on the larger homeland that sustains them.
The distinction between host and guest is therefore about roles, not ranks. Everyone receives. Everyone has something to give.
The question is whether the exchange sustains the place.
A visitor who takes without restraint leaves less for those who come next. A host who neglects the place has less to offer. Both have responsibilities, and neither can fulfil them alone.
This is the heart of reciprocity, a principle found across Indigenous philosophies: relationships stay healthy when gifts move in both directions. The Haudenosaunee teaching of the seventh generation extends that exchange across time, asking that decisions made today leave the place well for those not yet born.
Mutual benefit begins here, with the recognition that different beings carry different gifts and obligations.
What people carry forward
My grandmother’s teaching connects these relationships to the ways people meet their neighbours.
The host prepares a place, offers food and rest, and explains where the visitor has arrived. The guest makes themselves known, explains why they have come, listens to the terms of the visit, and brings something in return. The gift may be material. It may also be labour, knowledge, news, or a commitment to help.
Nations around the Great Lakes carried this ethic into treaty. The Dish with One Spoon, an agreement among the Haudenosaunee, Anishinaabe and allied Nations, describes shared hunting grounds as a single dish. Everyone eats from it with one spoon, takes only what they need, leaves enough for others, and keeps the dish clean. The Two Row Wampum, between the Haudenosaunee and European newcomers, shows two vessels travelling side by side on the same river, each keeping its own ways and neither steering the other.
In this understanding, acknowledgement is more than naming the people associated with a territory. It is learning enough about a homeland to behave responsibly within it.
Whose home is this? What sustains it? What laws and agreements guide our presence? What can we receive, and what must we return?
These questions make acknowledgement a relationship rather than a recital.
They also make it diplomatic. A guest who recognizes the host’s homeland recognizes that they have entered a place with its own relationships and responsibilities. A host who welcomes the guest makes room for an encounter governed by those relationships.
Neither arrives without standing. Neither arrives without obligations.
Beginning with place
I write from the shores of the Bay of Quinte. Here, the teaching asks me to begin with the water, the shoreline, and the life they sustain. Before I describe myself, I must attend to where I am.
That does not make people or history less important. It places them within the homeland that gives them meaning. The people, their laws, their agreements, and their responsibilities all belong to the place.
In a time of longer fire seasons, troubled waters, and uncertainty about what the next season will bring, this teaching asks something difficult and useful of us: pay attention before you speak.
An acknowledgement cannot tell the story of a place if the speaker has stopped noticing it.
The land came first. Beginning there again means learning to name what sustains us, and accepting that what sustains us also asks something of us.
By Rye Karonhiowanen Barberstock
Photo by Andrik Langfield on Unsplash
The post The Land Came First appeared first on Indigenous Climate Hub.
Carbon dioxide (CO2) emissions from fossil fuels and cement are projected to fall by around 0.4% in 2026 to 38.2bn tonnes of CO2 (GtCO2), according to new figures from the Global Carbon Project.
This guest post is by:
- Dr Zeke Hausfather, Carbon Brief’s climate science contributor
- Prof Pierre Friedlingstein, chair of mathematical modelling of climate systems at the University of Exeter and part of the Global Carbon Project team.
Carbon dioxide (CO2) emissions from fossil fuels and cement are projected to fall by around 0.4% in 2026 to 38.2bn tonnes of CO2 (GtCO2), according to new figures from the Global Carbon Project.
The 21st edition of the annual “global carbon budget” report, published today, says that this small decline is largely due to a 1.9% drop in emissions from oil and the energy shock triggered by the Iran conflict and the closure of the strait of Hormuz.
Emissions from coal continue to increase slightly.
The Global Carbon Project’s projections for fossil fuel and cement CO2 emissions in 2026 are preliminary, with a range that spans a fall of -1.5% to a rise of +0.6%.
This means a small increase in emissions can not be ruled out.
Emissions from land-use change, such as deforestation, are projected to rise in 2026.
This is primarily driven by peat fires and forest degradation in south-east Asia and is linked to the development of a strong El Niño event this year.
As a result, total CO2 emissions from fossil fuels and land use are projected to reach a record high of 43.3GtCO2 in 2026 – marginally above 42.8GtCO2 in 2025.
Research published alongside the report by the same team in Nature Climate Change finds that the growth in solar, wind and electric vehicles (EVs) now offsets around two-thirds of the emissions that would otherwise come from rising energy demand.
However, the deployment of these technologies is not yet enough to push global emissions into a sustained decline, according to the study.
The 2026 global carbon budget report also estimates that:
- Fossil emissions are projected to fall in China (-0.9%), the US (-1.3%) and the EU (-1.5%) in 2026, but rise by 4.4% in India.
- Oil emissions are projected to fall in every major region, with the largest drop in China (-4.6%).
- Land-use emissions averaged 4.9GtCO2 per year over 2016-25, around 21% lower than the decade before.
- Total CO2 emissions (fossil and land-use) grew by an average 0.3% per year over the past decade (2016-25), compared with 1.7% per year over the decade before.
- The remaining carbon budget to limit warming to 1.5C is 150GtCO2, or less than four years of current emissions.
- The land sink in 2025 was the highest on record, rebounding after being weakened during the 2023-24 El Niño. The current El Niño is expected to weaken the land sink in 2027.
- The concentration of CO2 in the atmosphere is set to reach 427.7 parts per million (ppm) in 2026, 54% above pre-industrial levels.
(For more on previous editions of the Global Carbon Project’s annual report, see Carbon Brief’s coverage in 2025, 2024, 2023 and 2022.)
Total emissions edge up as land-use emissions rise
Total global CO2 emissions, which combines fossil fuels and land-use change, are projected to reach a record high of 43.3GtCO2 in 2026, up from 42.8GtCO2 in 2025.
The increase in 2026 comes entirely from a projected rise in land-use emissions, which are more challenging to estimate than fossil emissions.
(The global carbon budget groups emissions from fossil fuels and cement production as “fossil emissions”. Carbon Brief follows this convention throughout this piece.)
If land-use emissions had stayed at 2025 levels, total emissions would have fallen slightly in 2026 to around 42.6GtCO2.
Each edition of the global carbon budget updates the historical record as new data and methods become available. The chart below shows total emissions in this year’s budget compared with the five previous editions.
This year’s estimates of historical fossil emissions are around 0.3GtCO2 per year higher than in last year’s budget.
This is largely because the report now estimates a smaller “cement carbonation” sink in the wake of research published this year in Communications Sustainability. In other words, it estimates that cement is able to slowly reabsorb less CO2 over its lifetime than previously thought.
Estimates of land-use emissions have also been revised, including a spike in 2018 – visible in the chart above – linked to updated cropland data for Colombia.
The updated numbers show that total emissions have grown by 0.3% per year over the past decade (2016-25), compared with 1.7%