2009
DOI: 10.1016/j.margeo.2009.01.007
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Deposition and flux of sediment from the Po River, Italy: An idealized and wintertime numerical modeling study

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Cited by 48 publications
(35 citation statements)
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“…The most significant contribution is from the Po River, with an annual mean flow rate of 1700 m 3 /s [28]. The Po river plume largely affects the deposition of sediments and causes a reduction in salinity from freshwater discharge [26,29]. Owing to river runoff and oceanographic conditions, the region also exhibits a decreasing trend of nutrient concentration and production from North to South and from West to East [30], see the mean concentration of Chlorophyll-a in Figure 3.…”
Section: Environment and Biotamentioning
confidence: 99%
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“…The most significant contribution is from the Po River, with an annual mean flow rate of 1700 m 3 /s [28]. The Po river plume largely affects the deposition of sediments and causes a reduction in salinity from freshwater discharge [26,29]. Owing to river runoff and oceanographic conditions, the region also exhibits a decreasing trend of nutrient concentration and production from North to South and from West to East [30], see the mean concentration of Chlorophyll-a in Figure 3.…”
Section: Environment and Biotamentioning
confidence: 99%
“…Prevailing winds and circulation patterns affect the transport and distribution of the plume [28,29] showed that the plume is generally confined to the North of Ravenna. There are also regional environmental discontinuities along an inshore-offshore axis, related to differences in depth, wave-induced shear stress, sediment deposits and human impacts [29,31].…”
Section: Environment and Biotamentioning
confidence: 99%
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“…Namely, the influence of coastal and bottom currents, which are able to transport the eroded material, re-suspend sediments and rebuild the bottom topography, appeared to be of primary importance , Bever et al 2009). …”
Section: The Study Areamentioning
confidence: 99%
“…In consequence, preferential depositional patterns during river floods can partially explain long-term fine deposits observed on the sea floor (Ogston et al 2000). On longer time-scales, advection of sediment by shelf currents can redistribute sediment and determine final deposition patterns (Sherwood et al 1994, Harris et al 2008, Bever et al 2009, Xu et al, 2011, Xue et al 2013.…”
Section: Introductionmentioning
confidence: 99%