Anticyclogenesis

/ˌæntɪˌsaɪkloʊˈdʒɛnəsɪs/ noun

The process by which an anticyclone (a high-pressure weather system) develops and forms in the atmosphere.

From anti- (opposite) + cyclogenesis (formation of a cyclone). Cyclogenesis comes from Greek 'kyklos' (circle) and '-genesis' (creation). The term emerged in meteorology in the 20th century as scientists studied opposite weather patterns.

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