The ice around the emperors
The emperor penguin was listed as Endangered in 2026 for sea-ice loss. This is what the satellite record actually shows, measured colony by colony rather than continent-wide: over the 1979–2024 record 57 of 67 emperor colonies show no measurable change in their sea ice, and only 10 carry a trend that survives both gates — clear of twice its own uncertainty, and still clear once the low-reading pre-1988 sensor is dropped. 5 of those fall. 4 rise — one fewer than the fitted lines suggest, because at Mertz Glacier the apparent gain is a single level shift in 2011 rather than a trend, and allowing it reverses the slope. The loss is real and regional, not continental. The listing rests on projected future ice, and the observed record says so plainly.
A third gate, and it costs this page a number
The two gates above both assume the record is a straight line with noise on it. On 13 August every fitted series on this site was made to nominate its own worst break year — the year at which the level of the record changed rather than its slope — against a Monte Carlo null, with no event supplied. 5 of the April–November trends published here came back flagged, and 5 of them are trends this page calls robust.
| Colony | Region | Break | Plain %/decade | With one step | Step points | Verdict |
|---|---|---|---|---|---|---|
| Gould | Queen Elizabeth Land | 1987 | +4.17 | +1.12 | +16.25 ± 1.85 | same sign |
| Mertz Glacier | Victoria Land | 2011 | +1.31 | -2.04 | +8.78 ± 2.49 | sign reverses |
| Barrier Bay | Princess Elizabeth Land | 1994 | -3.51 | +0.47 | -13.89 ± 4.21 | sign reverses |
| Rupert Coast | Marie Byrd Land | 1987 | +3.91 | +1.91 | +10.66 ± 3.61 | same sign |
| West Ice Shelf | Princess Elizabeth Land | 1994 | -2.65 | +0.00 | -9.25 ± 3.22 | sign reverses |
They are not all the same kind of problem, and the differences decide what may still be quoted.
1987 is the satellite. The breaks at Gould and Rupert Coast land on the instrument change this page's own second gate already exists for: their robust verdict is fitted 1988 onward and survives, while the 46-year slope in the table below is the one carrying the step. That is the third independent route to a conclusion this site reached in July.
1994 is one place, not two. Barrier Bay and West Ice Shelf are 75.2 km apart, inside the radius at which two sea-ice records stop being independent, so they are one measurement made twice — and it steps down. The year is not an instrument, not an iceberg anybody knows of, and turns up in scattered places a thousand kilometres away, so no cause may be named for it.
2011 is the one that changes a published number. At Mertz Glacier the April–November ice fits a rise of +1.31 points per decade from 1988 and this page published it as robust. Allow the series one level shift and the slope is -2.04 with a step of +8.78 — sign reversed, and the step is seven times the slope it replaces. The scan picked 2011 out of 21 candidate years knowing nothing about icebergs; it is the first full ice year after B09B grounded in Commonwealth Bay. So the count of colonies gaining ice on this page is 4 and not 5.
Which year did the ice change? — all 5,686 series asked the same question →
Where the ice is going, and where it is coming
Grouped into the five standard sea-ice sectors. The Bellingshausen–Amundsen sector is the only one whose colonies average a loss; the Ross Sea sector averages +1.38 points a decade — a gain, at 8 colonies out of 11. A colony sitting near a sector bound falls on one side of a line drawn by convention rather than by geography, which is why the map above is the better read of this.
| Sector | Longitudes | Colonies | Mean %/decade | Falling | Rising |
|---|---|---|---|---|---|
| Bellingshausen–Amundsen | 130°W–60°W | 15 | -0.13 | 4 | 5 |
| Indian Ocean | 20°E–90°E | 16 | +0.21 | 3 | 6 |
| Western Pacific | 90°E–160°E | 12 | +0.61 | 0 | 4 |
| Weddell Sea | 60°W–20°E | 13 | +0.64 | 0 | 3 |
| Ross Sea | 160°E–130°W | 11 | +1.38 | 1 | 8 |
The steepest fall of all 67 is at the one colony known to have been lost
Emperor Island is the Dion Islands site in Marguerite Bay, first surveyed in 1948 and gone by about 2009. Its April–November sea ice fits 76% in 1979 down to 51% in 2024 — 4.0 standard errors clear of zero, the largest decline of any emperor colony on the continent — and the series drops into the low forties right around the years the colony stopped breeding.
That is a coincidence worth stating and not a cause worth claiming. A 25 km grid cell cannot see why a colony failed, and this measurement is the sea around the site rather than the ice under the birds. What it does establish is that the metric points at the right place without being told where to look.
The same coast, measured a second way
Everything above is how much ice a colony has. Read daily rather than monthly, the same archive answers a different question: when that ice goes. What ends a breeding season is not a low annual average — it is the sea opening before a chick can swim, and that is a date. Measured at 61 colonies, the retreat now runs significantly earlier at 9 and later at 6, and the geography is the one on the map above, arrived at independently. At Bear Peninsula the sea used to clear around 20 Jan and now clears around 22 Oct — 90 days.
A check nobody tuned for
Five Bellingshausen colonies were published as catastrophic 2022 breeding failures. Ranking all 67 colonies by how far their 2022 fledging-window ice fell below their own record — a measurement built without reference to that work — puts every one of those five in the top seven. The first 9 places on the ranking are one continuous stretch of coast, from the Antarctic Peninsula round to Marie Byrd Land, before a colony from anywhere else appears. Rothschild Island read 0.2% against its own 80% average, 5.3 standard deviations down.
5 colonies had their lowest fledging-window ice of the entire 45-year record in that one year. An independently reported event, reproduced by a metric that was not fitted to it — the strongest external check anything on this site has passed.
All 8 colonies losing ice
Every one of these has an April–November slope more than twice its own standard error below zero. The solid line is the April–November mean, the dashed grey the November–December fledging window, and the orange rule the fitted trend. Same fixed 0–100% axis in each, so the panels can be read against one another.
Every colony, ranked
| Colony | Region | Apr–Nov %/decade | Mean ice | Nov–Dec %/decade | 2022 σ | Verdict |
|---|---|---|---|---|---|---|
| Emperor Island | Southwest Antarctic Peninsula | -5.64 ± 2.83 | 63% | -5.96 | -2.6 | losing |
| Barrier Bay | Princess Elizabeth Land | -3.52 ± 1.22 | 70% | -11.55 | -0.6 | losing step at 1994 |
| West Ice Shelf | Princess Elizabeth Land | -2.65 ± 0.87 | 79% | -7.24 | -1.1 | losing step at 1994 |
| Rothschild Island | Palmer Land | -2.32 ± 2.21 | 70% | -1.77 | -5.3 | losing |
| Bryan Coast | Ellsworth Land | -1.57 ± 0.94 | 91% | -4.24 | -2.9 | losing |
| Flutter/Cape Darnley | Mac. Robertson Land | -1.42 ± 0.48 | 76% | -3.02 | -0.6 | losing |
| Verleger Point | Marie Byrd Land | -1.16 ± 0.71 | 88% | -7.40 | -3.8 | losing |
| Bear Peninsula | Marie Byrd Land | -1.12 ± 0.96 | 74% | -4.48 | -1.5 | losing |
| Snow Hill Island | Northeast Antarctic Peninsula | -1.09 ± 1.25 | 85% | -2.39 | -0.7 | no change |
| Smyley | Palmer Land | -0.92 ± 1.16 | 85% | -2.13 | -5.0 | no change |
| Point Geologie | Adelie Land | -0.51 ± 0.88 | 86% | +0.10 | -1.6 | no change |
| Cape Gates | Marie Byrd Land | -0.40 ± 0.44 | 93% | -4.12 | -1.5 | no change |
| Sanae | Queen Maud Land | -0.40 ± 0.92 | 83% | -0.58 | -0.4 | no change |
| Dibble Glacier | Wilkes Land | -0.34 ± 0.62 | 82% | -2.13 | -0.1 | no change |
| Pfrogner Point | Ellsworth Land | -0.33 ± 0.73 | 92% | -2.15 | -2.7 | no change |
| Cape Washington | Victoria Land | -0.18 ± 0.36 | 90% | -2.25 | 0.7 | no change |
| Peterson Bank | Wilkes Land | -0.05 ± 0.55 | 78% | -1.95 | -1.9 | no change |
| Haswell Island | Queen Mary Land | -0.02 ± 0.60 | 81% | -2.36 | -0.1 | no change |
| Franklin Island | Victoria Land | +0.05 ± 0.29 | 93% | +0.61 | 3.1 | no change |
| Lazarev | Queen Maud Land | +0.07 ± 0.57 | 85% | -0.99 | 0.1 | no change |
| Luitpold | Coats Land | +0.11 ± 0.24 | 95% | +0.89 | -1.5 | no change |
| Halley | Coats Land | +0.11 ± 0.51 | 89% | -2.00 | -1.1 | no change |
| Lazarev North | Queen Maud Land | +0.11 ± 0.54 | 86% | -0.74 | -0.2 | no change |
| Ninnis Bank | Victoria Land | +0.11 ± 0.63 | 87% | -1.34 | -2.3 | no change |
| Dolleman | Palmer Land | +0.14 ± 0.29 | 98% | +0.12 | 0.7 | no change |
| Cape Poinsett | Wilkes Land | +0.16 ± 0.59 | 79% | -0.85 | -1.0 | no change |
| Riiser-Larsen | Queen Maud Land | +0.18 ± 0.70 | 90% | +3.68 | 0.7 | no change |
| Dawson-Lambton | Coats Land | +0.18 ± 0.59 | 88% | -2.82 | -1.1 | no change |
| Auster Islands | Mac. Robertson Land | +0.20 ± 0.35 | 89% | +1.26 | -0.6 | no change |
| Amundsen Bay | Enderby Land | +0.22 ± 0.65 | 84% | -0.40 | 1.1 | no change |
| Atka | Queen Maud Land | +0.23 ± 0.64 | 84% | +2.20 | -0.3 | no change |
| Astrid | Queen Maud Land | +0.29 ± 0.85 | 84% | -0.35 | -0.8 | no change |
| Kloa Point | Kemp Land | +0.29 ± 0.51 | 90% | +1.19 | -0.9 | no change |
| Thurston Glacier, Mount Siple | Marie Byrd Land | +0.30 ± 0.58 | 84% | -2.95 | -2.7 | no change |
| Coulman Island | Victoria Land | +0.35 ± 0.31 | 95% | +2.44 | 0.7 | gaining |
| Cape Darlington | Palmer Land | +0.35 ± 0.31 | 96% | +0.44 | 0.9 | gaining |
| Posadowsky Bay | Queen Mary Land | +0.45 ± 0.46 | 90% | +0.47 | -2.3 | no change |
| Porpoise Bay | Wilkes Land | +0.51 ± 0.83 | 87% | +0.52 | -1.1 | no change |
| Verdi Inlet | Palmer Land | +0.51 ± 1.53 | 74% | -1.33 | -4.0 | no change |
| Ragnhild | Queen Maud Land | +0.63 ± 0.84 | 80% | -1.45 | 0.3 | no change |
| Taylor Glacier | Mac. Robertson Land | +0.64 ± 0.39 | 89% | +1.47 | -0.3 | gaining |
| Umebosi | Queen Maud Land | +0.67 ± 0.93 | 86% | -0.15 | 0.1 | no change |
| Beaufort Island North | Victoria Land | +0.71 ± 0.45 | 89% | +0.71 | 2.4 | gaining |
| Sabrina Coast | Wilkes Land | +0.72 ± 0.73 | 82% | +0.01 | 0.4 | no change |
| Casey Bay West | Enderby Land | +0.77 ± 0.83 | 84% | +0.20 | 0.5 | no change |
| Amanda Bay | Princess Elizabeth Land | +0.81 ± 0.57 | 85% | +3.34 | 1.2 | gaining |
| Fold Island | Kemp Land | +0.84 ± 0.45 | 90% | +1.54 | -0.6 | gaining |
| Drescher | Queen Maud Land | +0.87 ± 0.61 | 90% | +5.85 | 0.9 | gaining |
| Bowman Island | Wilkes Land | +1.14 ± 0.59 | 83% | +0.12 | -1.0 | gaining |
| Brownson Islands | Marie Byrd Land | +1.23 ± 0.88 | 83% | -2.33 | -2.0 | gaining |
| Shackleton Ice Shelf | Queen Mary Land | +1.38 ± 1.16 | 69% | -0.64 | -0.2 | gaining |
| Karelin Bay | Princess Elizabeth Land | +1.40 ± 0.66 | 85% | -0.13 | -1.8 | gaining |
| Vanhoeffen | Princess Elizabeth Land | +1.80 ± 0.70 | 86% | +0.18 | -1.7 | gaining |
| Cruzen Island | Marie Byrd Land | +1.86 ± 0.73 | 87% | -2.52 | -3.0 | gaining |
| Mertz Glacier | Victoria Land | +2.03 ± 0.73 | 73% | +0.31 | 0.1 | gaining step at 2011 |
| Gunnerus | Queen Maud Land | +2.19 ± 0.84 | 81% | +0.99 | 1.5 | gaining |
| Davies Bay | Victoria Land | +2.23 ± 0.92 | 89% | +1.93 | 0.4 | gaining |
| Yule Bay | Victoria Land | +2.24 ± 0.76 | 94% | +1.73 | -0.1 | gaining |
| Noville Peninsula | Ellsworth Land | +2.26 ± 0.99 | 85% | +2.54 | 0.5 | gaining |
| Cape Colbeck, Edward VII Peninsula | Marie Byrd Land | +2.30 ± 0.77 | 85% | -1.44 | -0.1 | gaining |
| Cape Roget | Victoria Land | +2.37 ± 0.81 | 90% | +4.79 | -0.0 | gaining |
| Jason Peninsula | Palmer Land | +2.53 ± 1.49 | 89% | -0.19 | 0.9 | gaining |
| Cape Crozier | Victoria Land | +2.77 ± 0.83 | 80% | +1.63 | 3.2 | gaining |
| Smith | Palmer Land | +3.04 ± 0.97 | 86% | +3.91 | 1.2 | gaining |
| Stancomb | Coats Land | +3.51 ± 1.53 | 80% | +7.18 | 0.8 | gaining |
| Rupert Coast | Marie Byrd Land | +3.91 ± 1.03 | 82% | +0.49 | -1.1 | gaining step at 1987 |
| Gould | Queen Elizabeth Land | +4.17 ± 1.13 | 90% | +5.63 | 0.9 | gaining step at 1987 |
Slopes are quoted ± two standard errors. A trend is called significant only above twice its standard error.
How this is measured, and what it is not
What it is. Mean sea-ice concentration over a fixed set of ocean cells within 100 km of the colony. Two windows are reported: April–November, the months a colony needs a platform, and November–December, when an early break-out takes the chicks before they can swim. A trend is called significant only above twice its standard error.
It is not fast ice. At 25 km the land-attached ice emperors breed on is narrower than one cell and cannot be resolved. This is the sea around the colony, not the platform under it.
It is not current. The record ends 2024-12-31. It is an archive, not a feed, and must never be presented as the current state of the ice. The live daily figure on the wire is a different product and the two are never blended.
Two sensitivity tests, reported rather than tuned away. Passive microwave suffers land spillover in coastal cells. Repeating every fit with all land-touching cells dropped keeps the sign at 31 of 34 significant colonies; the ones that move are weak positives, and no significant decline changes sign.
A straight line over 46 years is a poor model of a record that changed regime around 2016. Refitting on 1996-2024 alone keeps the sign at roughly three quarters of colonies, so single-colony slopes are weaker evidence than the regional pattern they form.
1 colony is left out entirely: Gipps Ice Rise has 7 ocean cells within 100 km, fewer than 8 ocean cells within 100 km, so no figure is published for it at all.
https://noaa-cdr-sea-ice-concentration-pds.s3.amazonaws.com/data/final/south/monthly/
And still no count of the birds themselves
This is the first number a colony page on this site has ever been able to carry, and it is a number about ice rather than about penguins. There are no population figures anywhere on this site: detecting colony size from satellite imagery does not work yet — our own detector correlates at r = −0.16 against ground counts across eight colonies. All all 729 breeding sites are mapped, and none of them are counted.
The continent behind these colonies
The same archive summed over the whole hemisphere rather than read at a colony says something that sounds like a contradiction and is not. Across all 46 years Antarctic sea-ice extent trends -0.063 ± 0.057 million km² per decade — 1.1 times its own standard error, and from 1988 onwards 1.9, so there is no trend this record can defend on either gate. And 345 of the 366 calendar dates in the year have their lowest reading of all 46 since 2016. A hemisphere with no trend in it is made of coasts moving in opposite directions, which is exactly what these colonies are. See the whole record →