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)
Pagina inizio
  • 1083 (literal)
Pagina fine
  • 1095 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 72 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 13 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 4 (literal)
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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