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From Wikipedia, the free encyclopedia

The Karale Glacier is one of the major glaciers in the area north of Kuummiit in Eastern Greenland. [1] It began to recede around 1990. [2]

Karale Glacier
Map showing the location of Karale Glacier
Map showing the location of Karale Glacier
LocationGreenland
Coordinates 66°08′N 36°49′W / 66.13°N 36.81°W / 66.13; -36.81
Areaaround 60 square kilometres (23 sq mi)

See also

References

  1. ^ Biette, Melody; Jomelli, Vincent; Chenet, Marie; Braucher, Régis; Menviel, Laurie; Swingedouw, Didier; Rinterknecht, Vincent (2022). "Evidence of the largest Late Holocene mountain glacier extent in southern and southeastern Greenland during the middle Neoglacial from 10 Be moraine dating". Boreas. 51 (1): 61–77. Bibcode: 2022Borea..51...61B. doi: 10.1111/bor.12555. ISSN  0300-9483.
  2. ^ Pavelka, Karel; Šedina, Jaroslav; Pavelka, Karel (2021). "Knud Rasmussen Glacier Status Analysis Based on Historical Data and Moving Detection Using RPAS". Applied Sciences. 11 (2): 754. doi: 10.3390/app11020754. ISSN  2076-3417.


From Wikipedia, the free encyclopedia

The Karale Glacier is one of the major glaciers in the area north of Kuummiit in Eastern Greenland. [1] It began to recede around 1990. [2]

Karale Glacier
Map showing the location of Karale Glacier
Map showing the location of Karale Glacier
LocationGreenland
Coordinates 66°08′N 36°49′W / 66.13°N 36.81°W / 66.13; -36.81
Areaaround 60 square kilometres (23 sq mi)

See also

References

  1. ^ Biette, Melody; Jomelli, Vincent; Chenet, Marie; Braucher, Régis; Menviel, Laurie; Swingedouw, Didier; Rinterknecht, Vincent (2022). "Evidence of the largest Late Holocene mountain glacier extent in southern and southeastern Greenland during the middle Neoglacial from 10 Be moraine dating". Boreas. 51 (1): 61–77. Bibcode: 2022Borea..51...61B. doi: 10.1111/bor.12555. ISSN  0300-9483.
  2. ^ Pavelka, Karel; Šedina, Jaroslav; Pavelka, Karel (2021). "Knud Rasmussen Glacier Status Analysis Based on Historical Data and Moving Detection Using RPAS". Applied Sciences. 11 (2): 754. doi: 10.3390/app11020754. ISSN  2076-3417.



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