The upstream–downstream connection of North Atlantic and Mediterranean cyclones in semi-idealized simulations
<p>Cyclogenesis in the Mediterranean is typically triggered by the intrusion of a potential vorticity (PV) streamer over the Mediterranean. The intrusion of the PV streamer results from a preceding Rossby wave breaking (RWB) upstream over the North Atlantic. The ridge leading to the RWB is typically...
Gorde:
| Egile Nagusiak: | , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Copernicus Publications
2024-03-01
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| Saila: | Weather and Climate Dynamics |
| Sarrera elektronikoa: | https://wcd.copernicus.org/articles/5/419/2024/wcd-5-419-2024.pdf |
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