Eady edge waves, frontal wave-trains and type-B cyclogenesis

Eady edge waves (EEWs) propagate on surface baroclinic zones and they resemble synoptic and sub-synoptic scale frontal wave-trains. The wave-trains are frequently depicted on surface charts, and occur per se on a front with a local baroclinicity extremum. The possible linkage of EEWs to frontal wave...

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Auteur principal: Huw C. Davies
Format: article
Langue:EN
Publié: Taylor & Francis Group 2021
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Accès en ligne:https://doaj.org/article/5aaa7f26fb614969b3ca13eee9f05107
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