Etymology:
Meaning:
An anticyclone is a large-scale atmospheric circulation characterized by high pressure at its center, with the air circulating clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere.
Origin:
The term "anticyclone" was first coined by Francis Galton in 1883. He used the term to describe a counter-rotating atmospheric circulation that formed over the North Atlantic Ocean. Galton's initial definition of an anticyclone included both the high-pressure region and the surrounding area of descending air.
Over time, the term "anticyclone" has come to specifically refer to the high-pressure region at the center of the circulation. The surrounding area of descending air is now typically referred to as a subsidence inversion.
Characteristics:
Anticyclones are typically associated with:
Anticyclones form due to a combination of heating and cooling in the atmosphere, as well as the rotation of the Earth (Coriolis force). They are often found in the subtropics and over the oceans.
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