Antarctic oasis

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".[1][2] 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.

The larger oases (with their respective areas) are:

• McMurdo Dry Valleys (approx. 4,900 km² (1,900 sq mi)), Victoria Land
• Cape Hallett, northern Victoria Land
• Bunger Hills (approx. 950 km² (370 sq mi)), between Wilkes Land and Queen Mary Land
• Holme Bay, Mac. Robertson Land
• Vestfold Hills (approx. 420 km² (160 sq mi)), Princess Elizabeth Land
• Larsemann Hills, Princess Elizabeth Land
• Stillwell Hills (approx. 96 km² (37 sq mi)), Kemp Land
• Schirmacher Oasis (approx. 34 km² (13 sq mi)), Princess Astrid Coast, Queen Maud Land

• Riffenburgh, Beau Encyclopedia of the Antarctic, vol II (Routledge, New York, 2007, ISBN 0-415-97024-5)

• Rostislav D. Kouznetsov, The structure of the lower ABL over antarctic oasis during the summer, IOP Conf. Series: Earth and Environmental Science 1 (2008) 012035 doi:10.1088/1755-1307/1/1/012035
• Bernadette Hince, The Antarctic Dictionary: A Complete Guide to Antarctic English, P 19

• About Antarctic oases and Dry valleys, British Antarctic Survey