Aajuitsup Tasia

Aajuitsup Tasia
A large lake surrounded by hills
Southern and northern shores of Aajuitsup Tasia
Aajuitsup Tasia is located in Greenland
Aajuitsup Tasia
Aajuitsup Tasia
Location within Greenland
LocationGreenland
Coordinates67°05′N 50°23′W / 67.083°N 50.383°W / 67.083; -50.383
Lake typeoligotroph
Max. length10 km (6.2 mi)
Max. width2 km (1.2 mi)
Average depth
32 m (105 ft)

Aajuitsup Tasia (old spelling: Aujuitsup Tasia; "long lake"[1]) is a large lake in central-western Greenland, in the Qeqqata municipality, just west of Russell Glacier. It is located approximately 12 km (7.5 mi) northeast of Kangerlussuaq. It is of elongated oval shape, with its western shore at 67°04′45″N 50°30′02″W / 67.07917°N 50.50056°W / 67.07917; -50.50056 and its eastern shore at 67°05′35″N 50°16′30″W / 67.09306°N 50.27500°W / 67.09306; -50.27500.[2] Aajuitsup Tasia is an oligotrophic lake of 32 m (105 ft) depth, covering an area of 1,350 hectares (3,300 acres).[3]

Geography

The 2 kilometres (1.2 mi) by 10 kilometres (6.2 mi)[2] lake is separated from the Akuliarusiarsuup Kuua valley and Kangerlussuaq in the south by a low tundra ridge−a part of the Kangaamiut dike swarm. To the west lies a sibling Sanningasoq twin lake. To the north-east lies the wide highland of Isunngua. The area around the north of the lake has multiple traces of paleolakes and its shorelines, especially at the northern shore, and water exchange through spillways.[1] The terraces around the lake suggests that the lake is subjected to gradual drainage, including a possible "catastrophic" recent drainage.[4] Beside the lake is around 1 kilometre (0.62 mi) of an outwash plain before the Russell Glacier is located.[5]

Its climate is characterized as having frigid winters with cool summers, and low annual precipitation, with most precipitation occurs during summer.[6]

Ecology

The area is characterized with Arctic shrubland, including shrub matrices and patches of tundra forbs and grasses usual among mountain non-carbonate substrate complexes, with common species include deciduous Salix, Betula, and Vaccinium uliginosum species, and evergreen Rhododendron groenlandicum and R. lapponicum.[6] Flies of Heterotrissocladius and Psectrocladius species were identified at the lake.[3]

References

  1. 1 2 Carrivick, Jonathan L.; Yde, Jacob; Russell, Andrew J.; Quincey, Duncan J.; Ingeman-Nielsen, Thomas; Mallalieu, Joseph (12 August 2016). "Ice-margin and meltwater dynamics during the mid-Holocene in the Kangerlussuaq area of west Greenland". Boreas. 46 (3): 369–387.
  2. 1 2 Vandrekort Vestgrønland: Kangerlussuaq (Map) (1996 ed.). Cartography by Compukort, Denmark. Greenland Tourism a/s.
  3. 1 2 Brodersen, Klaus Peter; Pedersen, Ole; Lindegaard, Claus; Hamburger, Kirsten (15 September 2004). "Chironomids (Diptera) and oxy‐regulatory capacity: an experimental approach to paleolimnological interpretation". Limnology and Oceanography. 49 (5): 1549–1559.
  4. ↑ Clarke, Amy (2002). Lake Records of Holocene Climate Change from West Greenland (PhD thesis). University of Liverpool.
  5. ↑ Binderup, Merete; Ahlstrøm, Andreas P.; Jakobsen, Peter R.; Jacobsen, Carsten S.; Gravesen, Peter; Jakobsen, Ole S. (2007). Glacier Ice as resource for freshwater export: Investigation of four glaciers from the Greenland Inland Ice. Field work and analysis (PDF) (Report).
  6. 1 2 Young, Amanda B.; Watts, David A.; Taylor, Alan H.; Post, Eric (March 2016). "Species and site differences influence climate-shrub growth responses in West Greenland". Dendrochronologia. 37: 69–78.