In what direction do you think the weather moves in the Antarctic in the pole? Why?
Answers
Temperature
Antarctica’s average annual temperature ranges from about −10 °C on the coast to −60 °C at the highest parts of the interior.
Antarctica’s average annual temperature ranges from about −10 °C on the coast to −60 °C at the highest parts of the interior.Near the coast, the temperature can exceed +10 °C in summer and fall to below −40 °C in winter. Over the elevated inland, it can rise to about −30 °C in summer but fall below −80 °C in winter.
Antarctica’s average annual temperature ranges from about −10 °C on the coast to −60 °C at the highest parts of the interior.Near the coast, the temperature can exceed +10 °C in summer and fall to below −40 °C in winter. Over the elevated inland, it can rise to about −30 °C in summer but fall below −80 °C in winter.The lowest temperature ever recorded on the Earth’s surface was −89.2 °C at Vostok station on 21 July 1983.
Wind
Antarctica’s environment has special conditions that make it the windiest continent on Earth.
Antarctica’s environment has special conditions that make it the windiest continent on Earth.Antarctica is usually surrounded by a belt of low pressure which contains multiple low centres. This is called the ‘circumpolar trough’. But the interior of the continent is dominated by high pressure. These conditions set the scene for the formation of katabatic winds.
Katabatic winds are created when radiative cooling over the elevated Antarctic ice sheet produces very cold, dense air. The cold, dense air flows downhill, and is replaced by subsiding air from above. The resulting katabatic winds accelerate downhill, enhanced by the confluence of glacial valleys.
Katabatic winds are created when radiative cooling over the elevated Antarctic ice sheet produces very cold, dense air. The cold, dense air flows downhill, and is replaced by subsiding air from above. The resulting katabatic winds accelerate downhill, enhanced by the confluence of glacial valleys.Katabatic winds blow with great consistency over large areas. At the coast they lose their driving force and soon dissipate offshore.
Katabatic winds are created when radiative cooling over the elevated Antarctic ice sheet produces very cold, dense air. The cold, dense air flows downhill, and is replaced by subsiding air from above. The resulting katabatic winds accelerate downhill, enhanced by the confluence of glacial valleys.Katabatic winds blow with great consistency over large areas. At the coast they lose their driving force and soon dissipate offshore.Low-pressure systems near the coast can interact with katabatic winds to increase their strength. Resulting wind speeds can exceed 100 km/h for days at a time. Wind gusts well over 200 km/h have been measured.
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