Antarctic oasis

Geology

In Antarctica there are, in addition to mountaintops and nunataks, other natural snow- and ice-free areas often referred to as "Antarctic oases" or "dry valleys". These areas are surrounded by the Antarctic ice sheet or, in coastal areas, are situated between the ice sheet and the Antarctic ice shelves.

Antarctic oases and dry valleys develop in areas with particular regional weather patterns and geography. These areas have very low humidity and precipitation. Although these areas are very cold, sufficient solar energy is absorbed by the ground to melt what little snow does fall, or else it is scoured or sublimated by katabatic winds, leaving the underlying rock exposed.

Despite usually extreme aridity, some plants, in the form of bryophytes and lichens, can survive in Antarctic oases.

Geography

The larger oases (with their respective areas) are:

• McMurdo Dry Valleys (approx. 4900 km2), Victoria Land
• Cape Hallett, northern Victoria Land
• Bunger Hills (approx. 950 km2), between Wilkes Land and Queen Mary Land
• Holme Bay, Mac. Robertson Land
• Vestfold Hills (approx. 420 km2), Princess Elizabeth Land
• Larsemann Hills, Princess Elizabeth Land
• Stillwell Hills (approx. 96 km2), Kemp Land
• Schirmacher Oasis (approx. 34 km2), Princess Astrid Coast, Queen Maud Land

References

References

1. Kouznetsov, R. D.. (2008). "The structure of the lower ABL over antarctic oasis during the summer". IOP Conf. Ser.: Earth Environ. Sci..
2. Hince, Bernadette. (2000). "The Antarctic dictionary: a complete guide to Antarctic English". CSIRO Publishing.