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The Spalte Glacier was a large floating glacier located in Crown Prince Christian Land, northeastern Greenland. The glacier broke up and completely disintegrated in July 2020. The glacier broke up and completely disintegrated in July 2020.
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 ...
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 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]
The event produced an unprecedented very long period (VLP) seismic event observable on seismic stations worldwide for up to nine days. [6] The wave was caught in a narrow fjord which caused the wave to continue to slosh back and forth off the walls for the entire time, [ 7 ] resulting in a global seismic vibration, picked up all over the world ...
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 ...
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 glacier has been in a quiescent state since, although there are suggestions it will reach the required pre-surge conditions by 2027–2030. Grounding-line retreat is noted by the same article to be approximately 400m/yr, and the "dynamic cycling" of temperature and precipitation (which alters glacier mass-balance) is thought to be causing this.
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