1973
DOI: 10.4319/lo.1973.18.5.0705
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Dispersal Processes of Freshwaters in the Po River Coastal Area1

Abstract: Tidal effects on the vertical structure and dynamic pattern of the freshwater plume in the PO River coastal area were evaluated.A large vertical density gradient just below the surface and a lateral density front separate the fresh and seawatcrs. The horizontal extent of the river waters was followed by the continuous analysis of nitrate, whose conservative behavior, evidenced by a linear relationship with salinity, is justified by the observed trophic conditions.

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Cited by 21 publications
(6 citation statements)
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“…The northern Adriatic is the shallowest and most dynamic region of the Adriatic Sea. The coastal water mass circulation in this region is strongly influenced by freshwater outflow from the Po river which spreads in the surface layer, forming a plume that is separated from more saline Adriatic waters and giving rise to a frontal system (Grancini & Cescon 1973). This system is established in the northern basin for most of the year (Franco 1983, Fonda Umani et al 1992; the system clearly separates neritic, eutrophic waters from oligo-mesotrophic offshore waters, producing 2 independent and ecologically different environments (Franco 1984, Smodlaka 1986, Fonda Umani et al 1994, Alberighi et al 1997.…”
Section: Methodsmentioning
confidence: 99%
“…The northern Adriatic is the shallowest and most dynamic region of the Adriatic Sea. The coastal water mass circulation in this region is strongly influenced by freshwater outflow from the Po river which spreads in the surface layer, forming a plume that is separated from more saline Adriatic waters and giving rise to a frontal system (Grancini & Cescon 1973). This system is established in the northern basin for most of the year (Franco 1983, Fonda Umani et al 1992; the system clearly separates neritic, eutrophic waters from oligo-mesotrophic offshore waters, producing 2 independent and ecologically different environments (Franco 1984, Smodlaka 1986, Fonda Umani et al 1994, Alberighi et al 1997.…”
Section: Methodsmentioning
confidence: 99%
“…An estuarine plume is commonly observed to incline itself to either side of the coast, the Coriolis force as a driving factor, more typically against the coast to the right, facing downstream in the northern hemisphere [21]. Dynamics of the estuarine river plumes have been extensively studied through field observation [1,5,9,12,22,26,34,35,40,60,63,66,76,82], theoretical study [13,14,31,32,39,57,58,88], and numerical modeling [3, 4, 10, 11, 16-20, 28, 36, 37, 41, 43, 49, 54, 62, 64, 65, 70, 84, 89-93, 98, 99]. There has been considerable work done to understand how plume scales (along and across shore) depend on river discharge, as well as the importance of tides in modifying the plume dynamics.…”
Section: Introductionmentioning
confidence: 99%
“…DisCUssion the northern adriatic is the shallowest and most dynamic area of the adriatic sea. the coastal circulation is strongly influenced by the considerable, but pulsing freshwater outflow from the Po river which spreads at the surface, generating a plume during the stratified periods (spring to summer) (grancini and Cescon, 1973). in autumn-winter the mixed coastal waters are confined in a narrow belt, and the frontal system clearly separates neritic, eutrophic waters from offshore oligo-mesotrophic waters, producing two ecologically different environments (Franco, 1984;Fonda Umani et al, 1994).…”
Section: Prey Selectivitymentioning
confidence: 99%