2000
DOI: 10.1016/s1464-1909(00)00028-9
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Tidal propagation in Ria de Aveiro Lagoon, Portugal

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Cited by 176 publications
(116 citation statements)
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“…Tides are semi-diurnal, ranging, at the ocean boundary, from 0.6 m at neap tide to 3.2 m at spring tide, with an average amplitude of 2 m (IH, 2014). The tidal phase lag, relative to the ocean boundary, is in the order of 6 h in the upper reaches of the channels; whilst the water residence time in the lagoon varies from less than 2 days near the ocean boundary, to more than 1 week in the upstream channels (Dias et al, 2000a). The average depth of the lagoon is 1 m, except in navigation channels where dredging operations are frequently carried out to maintain the depths of about 20 m in the ocean boundary and 7 m in the navigation channels (Dias et al, 2000a).…”
Section: Hydrological Regimementioning
confidence: 99%
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“…Tides are semi-diurnal, ranging, at the ocean boundary, from 0.6 m at neap tide to 3.2 m at spring tide, with an average amplitude of 2 m (IH, 2014). The tidal phase lag, relative to the ocean boundary, is in the order of 6 h in the upper reaches of the channels; whilst the water residence time in the lagoon varies from less than 2 days near the ocean boundary, to more than 1 week in the upstream channels (Dias et al, 2000a). The average depth of the lagoon is 1 m, except in navigation channels where dredging operations are frequently carried out to maintain the depths of about 20 m in the ocean boundary and 7 m in the navigation channels (Dias et al, 2000a).…”
Section: Hydrological Regimementioning
confidence: 99%
“…The Ria Lagoon is part of the Vouga River basin area, and is approximately 45 km long (NNE-SSW) and 10 km wide (Dias et al, 2000a). The lagoon forms a unique mesotidal wetland area, characterized by four main channels with several branches forming islands, inner basins and mudflats.…”
Section: Characterization Of the Ria De Aveiro Lagoonmentioning
confidence: 99%
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“…Despite the fact that rivers have a small contribution in terms of water input, when compared to the tidal prism, they may have a long-term influence in the residual transport (Dias et al 2003). Dias et al (2000) and showed that the tide is strongly distorted as it progresses from the mouth toward the end of each channel of the lagoon, due to the channels geometry and bathymetry. The general characteristics of the tidal wave are those of a damped progressive wave.…”
Section: The Study Areamentioning
confidence: 99%
“…The lagoon has been also studied through numerical modelling. These studies were performed to investigate topics as the tidal propagation in the lagoon (Dias et al 2000), the lagrangian transport of particles ) and studies of sediment particles Dias et al 2003).…”
Section: Introductionmentioning
confidence: 99%