The role of a developing upper diffluent trough in surface cyclogenesis over central Mediterranean
An attempt is made to investigate the role of the jet streaks upstream an upper tropospheric diffluent trough in its evolution. A proof of the relationship that controls the rate of change of the mean absolute vorticity in the region of the diffluent trough is provided. It is demonstrated that for c...
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| Autors principals: | , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Borntraeger
1997-07-01
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| Col·lecció: | Meteorologische Zeitschrift |
| Matèries: | |
| Accés en línia: | http://dx.doi.org/10.1127/metz/6/1997/108 |
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