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An image from the European Space Agecny’s Copernicus Sentinel-2 image shows the Jakobshavn Isbræ Glacier in Greenland — one of the fastest and most active glaciers in the world.
The documentary includes scenes from a glacier calving event that took place at Jacobshavn Isbræ in Greenland, lasting 75 minutes, the longest such event ever captured on film. [ 2 ] [ 3 ] Two EIS videographers waited several weeks in a small tent overlooking the glacier and, finally, witnessed 7.4 cubic kilometres (1.8 cu mi) of ice crashing ...
The glacier was a northern offshoot of the Nioghalvfjerdsbrae glacier as it split either side of Hovgaard Island. [1] The main flow of the Nioghalvfjerdsbrae flows eastward out into Nioghalvfjerd Fjord while a smaller branch, the Spalte Glacier, flowed north into Dijmphna Sound.
As part of a comprehensive survey of Greenland's glaciers that was published in 2006, scientists documented that the mass balance—the sum of gains through snow accumulation and losses through iceberg calving and melting—of Kong Oscar and Greenland's other north-western glaciers was strongly negative between 1996 and 2005: they lost more ice than they gained. [2]
The Greenland Ice Sheet lost 5,091 sq km (1930 sq miles) of area between 1985 and 2022, according to a study in the journal Nature published on Wednesday, the first full ice-sheet wide estimate of ...
Scientists noticed the rift while looking at satellite images. Normally, cracks in a glacier wouldn't be much cause for concern, but this one is troubling. Scientists don't know what caused a ...
This glacier is located in the Lauge Koch Coast of Melville Bay, north of the Upernavik Archipelago. It drains the Greenland ice sheet ( Greenlandic : Sermersuaq ) and flows southwestwards between the King Oscar Glacier to the northwest and the Sverdrup Glacier to the southeast.
The Steensby Glacier originates in the Greenland Ice Sheet. It is roughly north–south oriented and has its terminus between Nyeboe Land and Warming Land at the head of the Saint George Fjord. The fjord is free from ice in the summer, and the glacier forms a floating tongue within the fjord that has shrunk since it was measured in 1963. [2] [3]