What is anticyclogenesis?

Anticyclogenesis refers to the development or strengthening of an anticyclonic circulation pattern in the Earth's atmosphere. These high-pressure systems are typically associated with lighter winds and clear skies. The process is the direct opposite of anticyclolysis and has a cyclonic counterpart known as cyclogenesis.

What we know

• Anticyclogenesis is defined as the development or strengthening of an anticyclonic circulation in the atmosphere. [2]
• Anticyclogenesis is the opposite process of anticyclolysis, which is the dissolution or weakening of an anticyclone, and relates to meteorological terminology found in atmospheric science glossaries. [2, 3]
• Anticyclones, which are formed through anticyclogenesis, are alternatively referred to as high pressure systems. [2]

Where to go next

• compared withWhat is anticyclolysis?
• how it workedHow does cyclogenesis work?
• the bigger pictureWhat is a glossary of meteorology?
• compared withWhat are low-pressure areas?
• whoWho was Carl-Gustaf Rossby?
• an unexpected connectionWho receives the Carl-Gustaf Rossby Research Medal?The highest award in atmospheric science is named after the pioneer who contributed significantly to the understanding of atmospheric waves that govern weather systems like highs and lows.

Sources

• [1]anticyclogenesis (Wikidata Q2853177) · CC0 1.0
• [2]Anticyclogenesis · CC BY-SA 4.0
• [3]Glossary of meteorology · CC BY-SA 4.0
• [4]Low-pressure area · CC BY-SA 4.0
• [5]Carl-Gustaf Rossby Research Medal · CC BY-SA 4.0