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Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ Anais da ABC (AABC)
SALVADOR,MARCUS VINICIUS S.; SILVA,MARIA AUGUSTA M. DA.
Bathymetric and sedimentological data from water depths between 3 and 28 meters are the basis of a detailed bathymetric map of the Itaipú Embayment and an understanding of its sedimentary dynamics. Shallower than 16 meters the contours are parallel to the shoreline whereas the morphology of the deeper bottom is influenced by the Menina, Mãe, and Pai islands. Medium sand is prevalent, with local variations in more protected or less protected areas. Minor amount of black mud possibly derives from the Itaipú Lagoon. Siliciclastic granules and pebbles may be relict. The Itaipú Embayment’s bottom morphology is controlled by stormy waves and the calmer easternmost part of the embayment presents a tendency to accumulate finer sediments.
Tipo: Info:eu-repo/semantics/article Palavras-chave: Coastal dynamics; Coastal sedimentation; Geomorphology; Quaternary.
Ano: 2002 URL: http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652002000100009
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Coastal numerical modelling of tides: Sensitivity to domain size and remotely generated internal tide ArchiMer
Ponte, Aurelien; Cornuelle, Bruce D..
The propagation of remotely generated superinertial internal tides constitutes a difficulty for the modelling of regional ocean tidal variability which we illustrate in several ways. First, the M2 tidal solution inside a control region located along the Southern California Bight coastline is monitored while the extent of the numerical domain is increased (up to 512 x 512 km). While the amplitude and phase of sea level averaged over the region is quasi-insensitive to domain size, a steady increase of kinetic energy, predominantly baroclinic, is observed with increasing domain size. The increasing flux of energy into the control region suggests that this trend is explained by the growing contribution from remote generation sites of internal tide which can...
Tipo: Text Palavras-chave: Barotropic tide; Baroclinic tide; Internal tide; Coastal dynamics; Domain size sensitivity; Energy budgets.
Ano: 2013 URL: http://archimer.ifremer.fr/doc/00124/23566/21467.pdf
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A numerical modeling study of the Southern Senegal upwelling shelf: Circulation and upwelling source waters ArchiMer
Ndoye, S; Capet, Xavier; Estrade, Philippe; Machu, Eric; Kounta, L; Sow, B; Diakhate, M; Gayet, At.
The regional ocean circulation along the Southern Senegal shelf is studied using a numerical model for varying forcing fields during the upwelling season (November-May). The main objective is to study the shelf circulation of the marine environment in the Southern Senegal Upwelling Shelf (SSUS), the Lagrangian pathways by which waters are transported to the surface in the upwelling tongue and the fate of these waters. Model results are compared with hydrographic measurements during UPSEN2-ECOAO survey and satellite images datasets. The upwelling source waters and also the warm nearshore waters are analyzed, from a Lagrangian point of view, by computing the paths of particles that are passively advected by the regional ocean model velocity field (ROMS). It...
Tipo: Text Palavras-chave: Upwelling; Ocean circulation; Modeling; Coastal dynamics; Shelf; ROMS..
Ano: 2018 URL: https://archimer.ifremer.fr/doc/00472/58346/60900.pdf
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Morphologie et dynamique actuelle de la côté duTogo OceanDocs
Blivi, A.B..
Le littoral togolais, lorrg de 50 km et de topographie absolument plane, est constitué de deux générations de cordons séparés du bassin côtier tertiaire par un système continu de lagunes....
Tipo: Journal Contribution Palavras-chave: Coastal dynamics; Coastal morphology.
Ano: 1993 URL: http://hdl.handle.net/1834/1233
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