Polar vortex
The polar vortex is a large, persistent circulation of frigid air located in the stratosphere and typically centred near the Earth’s poles.
It is characterized by a strong wind current that circulates from west to east, trapping cold air within the polar regions during the winter months.
The polar vortex plays a crucial role in maintaining the polar climate and can influence weather patterns in mid-latitude regions.
Occasionally, disruptions in the polar vortex can occur, leading to phenomena such as sudden stratospheric warming events, which can result in shifts in weather patterns and colder temperatures in regions outside of the polar areas.
The polar vortex is a large, persistent circulation of frigid air located in the stratosphere and typically centred near the Earth’s poles.
It is characterized by a strong wind current that circulates from west to east, trapping cold air within the polar regions during the winter months.
The polar vortex plays a crucial role in maintaining the polar climate and can influence weather patterns in mid-latitude regions.
Occasionally, disruptions in the polar vortex can occur, leading to phenomena such as sudden stratospheric warming events, which can result in shifts in weather patterns and colder temperatures in regions outside of the polar areas.