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A simple model for the break-up of marine aggregates by turbulent shear ArchiMer
Ruiz, Jean-eric; Izquierdo, A.
A simple model for the break-up, by turbulent shear, of marine aggregates is proposed. Three factors are considered to control the rupture of aggregates of different sizes. First, turbulence exerts stronger shear forces on bigger aggregates. Second, big aggregates are weaker than small ones because their porosity increases. Third, the rate of rupture of an aggregate is considered to be dependent on the point in the aggregate where the rupture takes place. This third factor allows the determination of the size distribution resulting from aggregate break-up. By considering these factors the model predicts the break-up rates of aggregates of different sizes and the aggregates' size-distribution resulting from this break-up. Therefore, the model represents an...
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Ano: 1997 URL: http://archimer.ifremer.fr/doc/00093/20417/18084.pdf
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Vertical structure of the semidiurnal tidal currents at Camarinal Sill, the strait of Gibraltar ArchiMer
Bruno, M; Mananes, R; Alonso, Jj; Izquierdo, A; Tejedor, L; Kagan, Ba.
The dynamical mode decomposition (DMD) technique is applied to the data of currentmeter and CTD measurements taken during the 1985-1986 Gibraltar Experiment and the 1989 survey so as to clarify features of the vertical structure of the M(2) and S(2) tidal currents at the Camarinal Sill. It is shown that in conformity with the inference made on the basis of the empirical orthogonal function (EOF) decomposition technique, these currents are mainly due to the M(2) and S(2) barotropic modes. At the same time the first three baroclinic modes are responsible not only for the vertical variability of the tidal currents but also for the velocity acid density amplitude variances at semidiurnal frequencies. Certain quantitative discrepancies between the values of...
Tipo: Text Palavras-chave: Modes barotrope et barocline; Courant de marée; Décomposition en mode dynamique; Détroit de Gibraltar; Barotropic and baroclinic modes; Tidal current; Dynamical mode decomposition; Strait of Gibraltar.
Ano: 2000 URL: http://archimer.ifremer.fr/doc/00325/43574/44042.pdf
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