On October 29, 2018 a very severe storm affected Northern Italy, including the Adriatic Sea. The ensuing surge and wave conditions at and in front of Venice stand at the extreme tail of the respective historical return period distributions. The large set of available measured data, at the coast and at the offshore oceanographic tower, coupled with detailed numerical simulations, allows a keen analysis of the storm, its predictability and in particular of the ensuing enhanced coastal processes. These include the coastal set-up, the input information for tidal prediction in Venice, the documented passage of an atmospheric cold front and, using the local tidal data, the derived possibility of estimating the surface wind stress, the evidence of reflected waves from the coast and the associated seismometers signal 40 km inland. The highest crest and wave heights measured at the tower are beyond what is suggested by non-linear statistics. The relative out-of-scale magnitude of the three major storms since 1966 suggests the possibility that they belong to a self-standing family of events.
The October 29, 2018 storm in Northern Italy - An exceptional event and its modeling
Cavaleri L;Bajo M;Barbariol F;Bastianini M;Benetazzo A;Bertotti L;Chiggiato J;Davolio S;Ferrarin C;Pezzutto P;Pomaro A;Umgiesser G
2019
Abstract
On October 29, 2018 a very severe storm affected Northern Italy, including the Adriatic Sea. The ensuing surge and wave conditions at and in front of Venice stand at the extreme tail of the respective historical return period distributions. The large set of available measured data, at the coast and at the offshore oceanographic tower, coupled with detailed numerical simulations, allows a keen analysis of the storm, its predictability and in particular of the ensuing enhanced coastal processes. These include the coastal set-up, the input information for tidal prediction in Venice, the documented passage of an atmospheric cold front and, using the local tidal data, the derived possibility of estimating the surface wind stress, the evidence of reflected waves from the coast and the associated seismometers signal 40 km inland. The highest crest and wave heights measured at the tower are beyond what is suggested by non-linear statistics. The relative out-of-scale magnitude of the three major storms since 1966 suggests the possibility that they belong to a self-standing family of events.File | Dimensione | Formato | |
---|---|---|---|
prod_413289-doc_184488.pdf
accesso aperto
Descrizione: The October 29, 2018 storm in Northern Italy - An exceptional event and its modeling. https://doi.org/10.1016/j.pocean.2019.102178
Tipologia:
Documento in Pre-print
Licenza:
Altro tipo di licenza
Dimensione
2.86 MB
Formato
Adobe PDF
|
2.86 MB | Adobe PDF | Visualizza/Apri |
prod_413289-doc_188610.pdf
solo utenti autorizzati
Descrizione: The October 29, 2018 storm in Northern Italy - An exceptional event and its modeling
Tipologia:
Versione Editoriale (PDF)
Licenza:
NON PUBBLICO - Accesso privato/ristretto
Dimensione
22.22 MB
Formato
Adobe PDF
|
22.22 MB | Adobe PDF | Visualizza/Apri Richiedi una copia |
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.