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Russian or German winds, depending upon which way they are blowing away from the Poles.

Catabatic winds are those that flow down slope from a cold region.

The cold air on the Antarctic Plateau for example, is about 3000 m high, and the air is hence dry (= heavier than moist air), very cold, and therefore dense. This flows towards the Antarctic coast in a continuous flow.

I seem to remember that at the French Adelie Station, the wind flow averaged a few tens of km per hour all the time. When they rebuilt the station after a fire, they built it mainly underground to escape this demoralizing effect.

Mawson had a few words on the subject also.

The NZ and the US bases at McMurdo Sound, are sufficiently remote from the mountains to escape this wind.

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