2002
DOI: 10.1016/s0278-4343(02)00033-x
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The Patos Lagoon hydrodynamics during an El Niño event (1998)

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Cited by 132 publications
(93 citation statements)
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“…In the central lagoon, the major effect of the river inflow is to establish a positive cross-shore pressure gradient, in agreement with the two-dimensional results of Fernandes et al (2002). Oscillatory motions generated after wind relaxation are attenuated by the river inflow, and are not sufficient to cause the flow to revert.…”
Section: Discussionsupporting
confidence: 85%
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“…In the central lagoon, the major effect of the river inflow is to establish a positive cross-shore pressure gradient, in agreement with the two-dimensional results of Fernandes et al (2002). Oscillatory motions generated after wind relaxation are attenuated by the river inflow, and are not sufficient to cause the flow to revert.…”
Section: Discussionsupporting
confidence: 85%
“…The positive cross-shore pressure gradient occurs everywhere along transects A and B for high discharges (not shown), even in the deeper parts, in contrast to the basic case experiment. This lateral set up/set down is consistent with the results of Fernandes et al (2002). As the wind decreases in intensity during the relaxation event, the alongshore pressure gradient in the lagoon is reversed (Fig.…”
Section: Dynamics In the Lagoon's Entrance Channelsupporting
confidence: 89%
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“…It is considered the largest choked coastal lagoon in the world 20 and similar to most choked coastal lagoon systems, the Patos Lagoon is wind forced rather than tidal driven. 21 The predominant NE-SW wind regime is the principal forcing factor and it decisively controls circulation, salinity distribution and water levels. 22 The only contact of the lagoon with the sea is through a relatively small inlet at its southern end, near the city of Rio Grande ( Figure 1).…”
Section: Study Sitesmentioning
confidence: 99%
“…Eventos episódicos de drenagem e intensidade dos ventos na escala intra-anual (North & Houde 2001), precipitação, pressão atmosférica, o regime, a intensidade e a direção dos ventos são fatores ambientais importantes para a dinâmica estuarina (Costa et al 1988, Garcia 1998, Fernandes et al 2001. Desta forma, estes fatores podem regular o período de desova e/ou influenciar a dispersão de larvas (North & Houde 2001).…”
Section: Introductionunclassified