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- W72231008 abstract "Abstract The lagoon Ebrie, in Ivory Coast, is formed of different bays and branches before communicating by an artificial canal with the Gulf of Guinea. The two principal lateral branches are quite different: the western channel forms a natural prolongation of the central channel while the eastern channel begins with a constriction. Observed at the eastern and western entrances of the lagoon, the circulation is statistically different, particularly in the upper layer and during ebb-tide. The eastern channel shows, at times, anomalies of residual velocity profiles which determine the relative asymmetry: there is often a seaward jet in the mid layer. The stronger residual anomalies are connected with sensible departures from the semi-diurnal period, involving the existence of beats between the tides and other subtidal frequencies. A decrease of Richardson number occurs during the anomalous profiles. The vertical mixing, its asymmetry and anomalies could be explained by a criterion for the maintenance of turbulence, depending on transient stages of river discharges and on the wind at the subtidal frequencies." @default.
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- W72231008 date "1978-01-01" @default.
- W72231008 modified "2023-09-23" @default.
- W72231008 title "Asymmetry and Anomalies of Circulation and Vertical Mixing in the Branching of a Lagoon-Estuary" @default.
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- W72231008 doi "https://doi.org/10.1016/s0422-9894(08)71279-0" @default.
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