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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| Format: | article |
| Language: | EN |
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Taylor & Francis Group
2021
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| Online Access: | https://doaj.org/article/5aaa7f26fb614969b3ca13eee9f05107 |
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