2016
DOI: 10.2112/si75-026.1
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Variability of Salinity in Pará River Estuary: 2D Analysis with Flexible Mesh Model

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Cited by 17 publications
(12 citation statements)
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“…The Amazon estuarine complex and adjacent coastal zones (AE) covered in this study belong to the Northern and Eastern coast of Marajó Island (i.e., Marajó Bay), as well as the Eastern coast of the state of Pará. Marajó Bay is formed mainly by Pará discharges and the Araguaia-Tocantins River Basin can be considered as the main freshwater source to this bay 59 . This area receives a superficial saline intrusion during low river discharge 60 and undergoes a macrotidal regime, with maximum tides around 4 m on both sides of the bay 61 .…”
Section: Methodsmentioning
confidence: 99%
“…The Amazon estuarine complex and adjacent coastal zones (AE) covered in this study belong to the Northern and Eastern coast of Marajó Island (i.e., Marajó Bay), as well as the Eastern coast of the state of Pará. Marajó Bay is formed mainly by Pará discharges and the Araguaia-Tocantins River Basin can be considered as the main freshwater source to this bay 59 . This area receives a superficial saline intrusion during low river discharge 60 and undergoes a macrotidal regime, with maximum tides around 4 m on both sides of the bay 61 .…”
Section: Methodsmentioning
confidence: 99%
“…oligohaline character (salinity between 0 and 5) throughout the entire estuary and the year (ROSA FILHO et al, 2018). Accordingly, in the river Pará's stretch and the study period, surface water salinity ranged from 0.01 to 0.05 (ROSÁRIO et al, 2016;COSTA et al, 2016a;2016b).…”
Section: Composition and Spatio-temporal Variationsmentioning
confidence: 94%
“…Mosqueiro Island is directly influenced by the Pará River estuary processes, which are governed by the seasonal variability of other river basins, such as the Guamá, that bathes the city of Belém (Prestes et al, 2020), and local tides. River discharges and tides control two important processes in the estuary, saline intrusion (Rosário et al, 2016) and suspended sediment transport (Carneiro et al, 2020). The tide is characterized by the macrotidal regime at the mouth of the estuary, with amplitudes of 5 meters (Prestes et al, 2017), in the region that comprises Marajó Bay.…”
Section: Introductionmentioning
confidence: 99%