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Ice Island Survives Run-In With Joe Island

✇NASA Breaking News
1 September 2026 at 00:00
AUGUST 24
AUGUST 23

A satellite view shows the iceberg after it pivoted out of the fjord into Nares Strait, wedged against a small, brown island.
A satellite view shows the iceberg after it pivoted out of the fjord into Nares Strait, wedged against a small, brown island.
NASA Earth Observatory / Lauren Dauphin

A satellite view shows a large tabular iceberg at the junction of its home fjord and Nares Strait.
A satellite view shows a large tabular iceberg at the junction of its home fjord and Nares Strait.
NASA Earth Observatory / Lauren Dauphin

A satellite view shows the iceberg after it pivoted out of the fjord into Nares Strait, wedged against a small, brown island.
A satellite view shows the iceberg after it pivoted out of the fjord into Nares Strait, wedged against a small, brown island.
NASA Earth Observatory / Lauren Dauphin
A satellite view shows a large tabular iceberg at the junction of its home fjord and Nares Strait.
A satellite view shows a large tabular iceberg at the junction of its home fjord and Nares Strait.
NASA Earth Observatory / Lauren Dauphin

AUGUST 24

AUGUST 23


An iceberg from Petermann Glacier encounters Joe Island in northwestern Greenland, visible in images captured by the OLI (Operational Land Imager) on Landsat 9 on August 23, 2026 (right), and August 24, 2026 (left). NASA Earth Observatory images by Lauren Dauphin.

Summer is prime iceberg season in Greenland’s glacier-fed fjords, and 2026 was no exception. Especially notable was the berg that broke from the Petermann Glacier along Greenland’s northwest coast in August. Roughly the size of St. Thomas in the U.S. Virgin Islands, it was the largest calving event by any Arctic glacier since 2020.

Iceberg calving is a routine part of an outlet glacier’s life cycle. Scientists watch the process closely, however, along with numerous other observations of the ice and its environment, for longer-term signs of instability. Petermann is one of Greenland’s largest marine-terminating glaciers and acts as a gatekeeper for ice flowing from the ice sheet into the ocean. Its future stability has implications for sea level rise.

The calving event of summer 2026 was spotted on August 4 by Adam Garbo, a doctoral student in glaciology at the University of Ottawa, in imagery from the European Space Agency’s Sentinel-1 mission. Garbo and an international team of colleagues have been using remote sensing to study and track the glacier’s ice tongue.

The team reported that the large tabular iceberg, or “ice island,” measured just over 76 square kilometers (29 square miles) at the time it calved—the largest to break from the glacier since the ice island of 2012 (130 square kilometers). The 2012 calving followed earlier major events in 2008 (31 square kilometers) and 2010 (just over 250 square kilometers).

The August 2026 event could have been even bigger. Garbo and colleagues had been expecting a major calving once one of the large rifts they were monitoring finally cut all the way across Petermann’s ice tongue. “What surprised us was that the calving instead followed a different fracture, producing a smaller ice island than we had originally anticipated,” Garbo said. As of late August, two large rifts remained and were expected to eventually produce new ice islands of roughly 94 square kilometers and 84 square kilometers, though the timing remained uncertain.

A detailed satellite view shows the iceberg wedged against the small, brown island, with sea ice packed densely to its left and more sparsely to its right.
August 24, 2026
NASA Earth Observatory/Lauren Dauphin

Glaciologist Mauri Pelto of Nichols College has also been tracking the iceberg, using images from NASA-USGS Landsat satellites, as it drifted down Petermann Fjord toward Nares Strait. In the week since it calved, the berg drifted an average of 3 kilometers per day. It continued toward the fjord’s junction with Nares Strait, where it rammed into a small rocky outcrop known as Joe Island (Joe Ø). The brief encounter is visible in images captured by the OLI (Operational Land Imager) on Landsat 9 on August 23 (top right) and August 24 (top left). A detailed view of the August 24 image is shown above.

Joe Island sits at the mouth of Petermann Fjord, making it one of the first obstacles a departing ice island meets. Collisions with it—like the one that split the 2010 ice island in two—often mark the start of a berg’s breakup. Petermann bergs tend to be thinner and more fragile than those calved by glaciers such as Greenland’s Jakobshavn and Helheim, and thinner still than Antarctica’s behemoths, Pelto noted.

“We were certainly watching closely as it interacted with Joe Island and were impressed that it survived the interaction without further fragmentation,” Garbo said.

The ice island was estimated to be less than 150 meters thick at the time of calving. Wind and surface currents have swept it out of the fjord, and satellite images show it pivoting away from Joe Island and continuing southwest through Nares Strait. As it drifts, it will fracture into smaller pieces as tides, winds, currents, and melting continue to weaken the ice.

Thicker bergs that calve from tidewater glaciers without floating ice-shelf extensions can drag and even become grounded on the seafloor within the fjord, while ice islands, like those from Petermann, might run aground later in their drift. Many ice islands have become “grounded” off the coasts of Coburg and Baffin islands.

Garbo and colleagues noted that ice islands and their fragments have been known to travel considerable distances, posing potential hazards to marine activities and infrastructure while also distributing freshwater through the ocean as they melt.

NASA Earth Observatory images by Lauren Dauphin, using Landsat data from the U.S. Geological Survey. Story by Kathryn Hansen.

Downloads

A satellite view shows a large tabular iceberg at the junction of its home fjord and Nares Strait.

August 23, 2026

JPEG (12.59 MB)

A satellite view shows the iceberg after it pivoted out of the fjord into Nares Strait, wedged against a small, brown island.

August 24, 2026

JPEG (10.23 MB)

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An Uncommon Drifter in the Denmark Strait

✇NASA Breaking News
20 August 2026 at 00:00
A satellite image shows the dark blue waters of the Denmark Strait with swirling sea ice to the right of eastern Greenland. A bright white iceberg sits amid the sea ice in the middle-left of the scene.
An iceberg drifts through the Denmark Strait in this image acquired on June 12, 2026, by the OLI (Operational Land Imager) on Landsat 9.
NASA Earth Observatory/Lauren Dauphin

Greenland’s jagged coastline is lined with fjords, many of them cradling marine-terminating glaciers that routinely calve icebergs into the water. It’s common to see these bergs, small and large, drifting in the island’s fjords each summer once the sea ice breaks up. In summer 2026, one exceptionally large berg turned up in the Denmark Strait—more than a thousand kilometers south of where it apparently originated. 

These images, captured by the OLI (Operational Land Imager) on Landsat 9, show the iceberg on June 12 as it drifted in the strait between Greenland and Iceland. It was just south of Kangikajiip Appalia, a cape on Greenland’s east coast visible in the scene’s upper left, amid a mixture of sea ice and berg fragments known as “mélange.”

Alexis Denton, oceanographer and chief scientist with the International Ice Patrol, noted that several clues indicate it is an iceberg rather than thick, multi-year sea ice: its proximity to shore, its whiter color, and larger size compared to the surrounding sea ice. Measuring roughly 17 square kilometers (7 square miles) on June 12, the iceberg was about five times the area of New York City’s Central Park. That’s modest compared to the behemoth bergs that calve from Antarctic glaciers and ice shelves but large by Greenland standards.

Keld Quistgaard, a senior ice advisor with the Danish Meteorological Institute’s Greenland Ice Service, noted that it originated in Jøkelbugten—a bay in northeastern Greenland. The berg’s precise origin within that bay, however, remains something of a mystery. It’s possible that the berg broke off from Zachariæ Isstrøm or its adjacent remnant ice shelf. The ice shelf, which together with Zachariæ Isstrøm once filled the bay, was abandoned after the glacier rapidly retreated in the early 2000s.

Tracing its path back through satellite imagery is challenging. Through spring, the bay and surrounding coastal areas are choked with sea ice and berg fragments, making individual bergs hard to distinguish, especially if covered in bright snow. In late May, for instance, the berg was surrounded by numerous look-alikes. Only later in the season, as it drifted farther south and the ice around it thinned out, did it become distinct enough to easily spot.

A detailed view shows the iceberg's bright white surface pocked with light blue meltwater ponds. Broken pieces of sea ice float around the iceberg in otherwise dark blue ocean water.
The iceberg’s bright white surface is pocked with light blue meltwater ponds in this detailed view of the image, acquired on June 12, 2026, by the OLI (Operational Land Imager) on Landsat 9.
NASA Earth Observatory/Lauren Dauphin

Its size and striking network of blue meltwater ponds offer some clues to its origin, according to Christopher Shuman, a retired University of Maryland glaciologist. Shuman thinks the berg broke from the remnant ice shelf rather than the glacier itself. Bergs calved from Zachariæ Isstrøm tend to be smaller, he said. Also, the berg’s surface—pocked with meltwater ponds, “like Swiss cheese”—closely resembles the remnant shelf ice. Past satellite images show pieces of that shelf ice drifting south and getting trapped among islands bordering the bay, where winds and tides have jostled them for years.

As of mid-August, the berg was about 1,500 kilometers (900 miles) from the bay, drifting south on the Greenland Coastal Current into the North Atlantic. Quistgaard expected the iceberg to gradually disintegrate throughout the month. Recent satellite imagery suggested it was doing just that.

Breaking up in the Denmark Strait means that remnants of the berg are unlikely to drift into busier shipping lanes that go past the southern tip of Greenland. “Its journey is a reminder of the dynamic Earth,” Shuman said, “as well as the seasonal variability of the ice in this part of the North Atlantic.”

NASA Earth Observatory images by Lauren Dauphin, using Landsat data from the U.S. Geological Survey. Story by Kathryn Hansen.

Downloads

A satellite image shows the dark blue waters of the Denmark Strait with swirling sea ice to the right of eastern Greenland. A bright white iceberg sits amid the sea ice in the middle-left of the scene.

June 12, 2026

JPEG (16.74 MB)

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Sensing the Poles’ Hidden Heat

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Surface temperatures across Earth’s poles pulse with the seasons, as seen in this animation based on two years of data collected by NASA’s PREFIRE (Polar Radiant Energy in the Far-InfraRed Experiment) mission.
NASA/Chad Greene

At the top and bottom of the planet, the seasons arrive on a schedule all their own. Satellite data from a mission measuring infrared energy reveal just how differently—and how dramatically—surface temperatures swing across two full years at the poles.

In this animation, surface temperatures across the Arctic and Antarctic pulse between cold (dark blue) and milder to warm (lighter blue to red). Data for the animation come from NASA’s PREFIRE (Polar Radiant Energy in the Far-InfraRed Experiment) satellites. The mission’s twin CubeSats began collecting science data in July 2024 and have now captured two complete seasonal cycles at each pole.

Because the two poles sit in opposite hemispheres, their seasons occur at opposite times—and the swing between seasons differs, too. In the Arctic, cold, dark winters give way to summers warm enough to thaw vast stretches of tundra and sea ice. In Antarctica, Earth’s coldest continent, summer temperatures rarely climb above freezing before the bitter cold of winter returns.

Surface temperatures, and how they fluctuate, offer a window into Earth’s energy budget, the net flow of energy into and out of the Earth system. Sunlight absorbed by the surface is re-radiated as infrared heat, which bounces between Earth’s surface and atmosphere before escaping to space. The poles play an important role in this process. Atmospheric and ocean circulation carries excess heat absorbed in the tropics toward the poles, where it radiates away to space, helping regulate the planet’s temperature.

“By measuring invisible heat radiating from Earth’s coldest places, PREFIRE is helping scientists understand why the poles are changing so rapidly, and what those changes might mean for the rest of the planet,” said Chad Greene, a glaciologist at NASA’s Jet Propulsion Laboratory.

Scientists have long known that far-infrared radiation accounts for nearly 60 percent of the energy Earth loses to space, but that portion of the spectrum—invisible to human eyes—had never been comprehensively measured on a global scale. By directly tracking this invisible energy in near-real-time, the PREFIRE mission is helping scientists refine models and gain a better understanding of the Earth system.

“Weather systems, river flows, shipping routes, and ice sheet stability are all influenced by energy movement in a part of the spectrum that only PREFIRE can see,” said Tristan L’Ecuyer, an atmospheric scientist at the University of Wisconsin-Madison and principal investigator of the PREFIRE mission. “Now that the invisible has been made visible, we can begin to improve weather and climate predictions that industries, our national defense, and Arctic communities rely on.”

Maps courtesy of Chad Greene, NASA/JPL, using data from NASA’s PREFIRE mission. Story by Kathryn Hansen.

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