Anticyclogenesis

anticyclogenesis

Any strengthening or development of anticyclonic circulation in the atmosphere; the opposite of anticyclolysis.

This applies to the development of anticyclonic circulation (or the initial appearance of a high) where previously it was nonexistent, as well as to intensification of existing anticyclonic flow. The most common application of this term is to the formation of a new anticyclone. Care should be taken, however, to distinguish the increase in anticyclonic circulation from the increase in atmospheric pressure (filling), although they usually occur simultaneously.
Compare cyclogenesis.

• INDEX
• A
• B
• C
• D
• E
• F
• G
• H
• I
• J
• K
• L
• M
• N
• O
• P
• Q
• R
• S
• T
• U
• V
• W
• X
• Y
• Z
• 0
• 1
• 2
• 3
• 4
• 5
• 6
• 7
• 8
• 9

Any strengthening or development of anticyclonic circulation in the atmosphere; the opposite of anticyclolysis.

Fluid motion having a sense of rotation about the local vertical opposite to that of the earth's rotation; that is, clockwise in the Northern Hemisphere, counterclockwise in the Southern Hemisphere, undefined at the equator.