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Jakobshavn Glacier (Danish: Jakobshavn Isbræ), also known as Ilulissat Glacier (Greenlandic: Sermeq Kujalleq), is a large outlet glacier in West Greenland. It is located near the Greenlandic town of Ilulissat (colonial name in Danish : Jakobshavn ) and ends at the sea in the Ilulissat Icefjord .
A NASA study revealed a glacier that was one of the fastest-shrinking ice and snow masses on Earth is making an unexpected comeback. Greenland's glacier, named Jakobshavn, was retreating roughly 1 ...
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 ...
Rink Glacier, west Greenland NASA picture of the southern part of Romer Lake with the Elephant Foot Glacier. This is a list of glaciers in Greenland. Details on the size and flow of some of the major Greenlandic glaciers are listed by Eric Rignot and Pannir Kanagaratnam (2006) Ice sheets and caps Greenland Ice Sheet Ad Astra Ice Cap Christian Erichsen Ice Cap Flade Isblink Geikie Plateau ...
Ilulissat Icefjord. The fjord contains the Jacobshavn Isbræ (Greenlandic: Sermeq Kujalleq), the most productive glacier in the Northern Hemisphere.The glacier flows at a rate of 20–35 m (66–115 ft) per day, resulting in around 20 billion tonnes of icebergs calved off and passing out of the fjord every year.
Normally, cracks in a glacier wouldn't be much cause for concern, but this one is troubling. Scientists noticed the rift while looking at satellite images. Normally, cracks in a glacier wouldn't ...
A 2021 analysis of sub-glacial sediment at the bottom of a 1.4 kilometres (0.87 mi) Greenland ice core finds that the Greenland ice sheet melted away at least once during the last million years, and therefore strongly suggests that its tipping point is below the 2.5 °C (4.5 °F) maximum temperature increase over the preindustrial conditions ...
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]