A Major Collapse of Kangerlussuaq Glacier's Ice Tongue Between 1932 and 1933 in East Greenland
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A Major Collapse of Kangerlussuaq Glacier's Ice Tongue Between 1932 and 1933 in East Greenland. / Vermassen, Flor; Bjørk, Anders A.; Sicre, Marie Alexandrine; Jaeger, John M.; Wangner, David J.; Kjeldsen, Kristian K.; Siggaard-Andersen, Marie Louise; Klein, Vincent; Mouginot, Jeremie; Kjær, Kurt H.; Andresen, Camilla S.
In: Geophysical Research Letters, Vol. 47, No. 4, e2019GL085954, 2020.Research output: Contribution to journal › Letter › Research › peer-review
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TY - JOUR
T1 - A Major Collapse of Kangerlussuaq Glacier's Ice Tongue Between 1932 and 1933 in East Greenland
AU - Vermassen, Flor
AU - Bjørk, Anders A.
AU - Sicre, Marie Alexandrine
AU - Jaeger, John M.
AU - Wangner, David J.
AU - Kjeldsen, Kristian K.
AU - Siggaard-Andersen, Marie Louise
AU - Klein, Vincent
AU - Mouginot, Jeremie
AU - Kjær, Kurt H.
AU - Andresen, Camilla S.
PY - 2020
Y1 - 2020
N2 - In recent years, several large outlet glaciers in Greenland lost their floating ice tongue, yet little is known regarding their stability over a longer timescale. Here we compile historical documents to demonstrate a major ice tongue collapse of Kangerlussuaq Glacier between 1932 and 1933. This event resulted in a 9-km retreat, exceeding any of the glacier's recent major retreat events. Sediment cores from the fjord are used to reconstruct sea surface temperatures and to investigate a potential sedimentological trace of the collapse. During the 1920s, local and regional sea surface temperatures and air temperatures increased rapidly, suggesting a climatic trigger for the collapse. Fjord bathymetry played an important role too, as the (partially) pinned ice tongue retreated off a submarine moraine during the event. This historical analogue of a glacier tongue collapse emphasizes the fragility of remaining ice tongues in North Greenland within a warming climate.
AB - In recent years, several large outlet glaciers in Greenland lost their floating ice tongue, yet little is known regarding their stability over a longer timescale. Here we compile historical documents to demonstrate a major ice tongue collapse of Kangerlussuaq Glacier between 1932 and 1933. This event resulted in a 9-km retreat, exceeding any of the glacier's recent major retreat events. Sediment cores from the fjord are used to reconstruct sea surface temperatures and to investigate a potential sedimentological trace of the collapse. During the 1920s, local and regional sea surface temperatures and air temperatures increased rapidly, suggesting a climatic trigger for the collapse. Fjord bathymetry played an important role too, as the (partially) pinned ice tongue retreated off a submarine moraine during the event. This historical analogue of a glacier tongue collapse emphasizes the fragility of remaining ice tongues in North Greenland within a warming climate.
KW - alkenones
KW - Glacier retreat
KW - historical documents
KW - IRD
KW - Kangerlussuaq Glacier
U2 - 10.1029/2019GL085954
DO - 10.1029/2019GL085954
M3 - Letter
AN - SCOPUS:85081088257
VL - 47
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 4
M1 - e2019GL085954
ER -
ID: 238377190