The winds that blow off the ice sheets of Antarctica and Greenland are known as katabatic winds. These downslope winds are dense and cold, originating from the high ice sheets and flowing towards lower elevations due to gravity. Katabatic winds can have significant impacts on local weather and climate.
Katabatic winds are downslope winds that flow from high elevation to low elevation due to cooling of air that becomes denser and heavier. Anabatic winds, on the other hand, are upslope winds that flow from low elevation to high elevation due to heating of air that becomes lighter and rises. Both types of winds are influenced by local topography and can be significant in mountainous regions.
From Wikipedia:"A katabatic wind, from the Greek word katabatikosmeaning "going downhill", is the technical name for a drainage wind, a wind that carries high density air from a higher elevation down a slope under the force of gravity."In Antarctica, katabatic winds swirl down to the beach -- about 750 miles -- from the elevated South Pole, which sits at an elevation of 9,300' (2900m), however the equivalent pressure elevation, based on polar atmospheric conditions, will vary from 10,800 (3300m) to 13,120 (4,000m).
Trade Winds blow fast and in Pretty much any direction. That's why sailors try to sail there often.
Winds blowing over a large area create powerful, high, and fast waves.
The winds that blow off the ice sheets of Antarctica and Greenland are known as katabatic winds. These downslope winds are dense and cold, originating from the high ice sheets and flowing towards lower elevations due to gravity. Katabatic winds can have significant impacts on local weather and climate.
Blizzards are constant on the Antarctic continent, specifically caused by Katabatic winds that blow off the polar plateau, and which are driven by the rotation of the Earth.
Katabatic winds are downslope winds that flow from high elevation to low elevation due to cooling of air that becomes denser and heavier. Anabatic winds, on the other hand, are upslope winds that flow from low elevation to high elevation due to heating of air that becomes lighter and rises. Both types of winds are influenced by local topography and can be significant in mountainous regions.
A little ove 750 mph that is
katabatic winds
Katabatic winds can howl across the continent, down the polar plateau, and achieve hurricane force. These winds move ice crystals around the continent and sometimes force scientists to remain indoors until the winds subside.
110 m/s
I have no idea
From Wikipedia:"A katabatic wind, from the Greek word katabatikosmeaning "going downhill", is the technical name for a drainage wind, a wind that carries high density air from a higher elevation down a slope under the force of gravity."In Antarctica, katabatic winds swirl down to the beach -- about 750 miles -- from the elevated South Pole, which sits at an elevation of 9,300' (2900m), however the equivalent pressure elevation, based on polar atmospheric conditions, will vary from 10,800 (3300m) to 13,120 (4,000m).
You're thinking of katabatic winds, driven by the rotation of the hearth and the rush of cold air flowing downhill from the 9,000 ft-above-sea level polar plateau.
Around 100 m/s.
There may be a typo in your question. Antarctica is often called home of the wind, because of the strong, constant Katabatic winds that blow to the coasts from high on the polar plateau.