The anticyclonic equivalent, the process of formation of high pressure areas, is anticyclogenesis.
2.
Anticyclogenesis, the process by which high pressure systems develop, usually gets less attention, given that highs are associated with fair weather.
3.
Cyclolysis is the opposite of cyclogenesis, and is the high-pressure system equivalent which deals with the formation of high-pressure areas Anticyclogenesis.
4.
All of these conditions lead to strong anticyclogenesis to the east of the Andes and thus, the high pressure system intensifies as it enters southern Argentina.
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