http://www.cnr.it/ontology/cnr/individuo/prodotto/ID288882
Wind-induced salt-wedge intrusion in the Tiber river mouth (Rome-Central Italy) (Articolo in rivista)
- Type
- Label
- Wind-induced salt-wedge intrusion in the Tiber river mouth (Rome-Central Italy) (Articolo in rivista) (literal)
- Anno
- 2014-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s12665-013-3024-5 (literal)
- Alternative label
Manca, Fabio; Capelli, Giuseppe; La Vigna, Francesco; Mazza, Roberto; Pascarella, Annalisa (2014)
Wind-induced salt-wedge intrusion in the Tiber river mouth (Rome-Central Italy)
in Environmental earth sciences (Print)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Manca, Fabio; Capelli, Giuseppe; La Vigna, Francesco; Mazza, Roberto; Pascarella, Annalisa (literal)
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- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Roma Tre University; ROMA CAPITALE Municipal Rome; Italian Natl Res Council IAC CNR (literal)
- Titolo
- Wind-induced salt-wedge intrusion in the Tiber river mouth (Rome-Central Italy) (literal)
- Abstract
- The wind effect on river water quality was illustrated by means of thermohaline measurements carried out in the Tiber River in May 2012. The survey was carried out using a boat, in stations located in the two Tiber branches: Fiumara Grande and Traiano Canal. Thermohaline variables (salinity and temperature) were used to describe the water-type patterns and to define the salt-wedge position. Although the river flow rate was rather high, saltwater intrusion happened. Wind data suggested that the more probable cause of salt-wedge intrusion was the wind action. Especially wind speeds higher than 4 m/s are able to dominate the sea current at surface layers, determining an increase in the sea level. Therefore, westerly winds determined a seawater inflow in the river mouths. (literal)
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