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Non-linear channel-shoal dynamics in long tidal embayments
Schramkowski, G.; Schuttelaars, H.M.; de Swart, H.E. (2004). Non-linear channel-shoal dynamics in long tidal embayments. Ocean Dynamics 54: 399-407
In: Ocean Dynamics. Springer-Verlag: Berlin; Heidelberg; New York. ISSN 1616-7341; e-ISSN 1616-7228, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

    Motion > Tidal motion > Tides
    Motion > Water motion > Circulation > Water circulation > Shelf dynamics > Estuarine dynamics
    Sediment load > Suspended load
    Sedimentary structures > Bed forms
    Water bodies > Coastal waters > Coastal landforms > Coastal inlets > Estuaries
Author keywords
    Morphodynamics; Morfodynamica

Auteurs  Top 
  • Schramkowski, G.
  • Schuttelaars, H.M.
  • de Swart, H.E.

    The dynamics of finite-amplitude bed forms in a tidal channel is studied with the use of an idealized morphodynamic model. The latter is based on depthaveraged equations for the tidal flow over a sandy bottom. The model considers phenomena on spatial scales of the order of the tidal excursion length. Transport of sediment mainly takes place as suspended load. The reference state of this model is characterized by a spatially uniform M2 tidal current over a fixed horizontal bed. The temporal evolution of deviations from this reference state is governed by amplitude equations: these are a set of non-linear equations that describe the temporal evolution of bed forms. These equations are used to obtain new morphodynamic equilibria which may be either static or time-periodic. Several of these bottom profiles show strong similarity with the tidal bars that are observed in natural estuaries. The dependence of the equilibrium solutions on the value of bottom friction and channel width is investigated systematically. For narrow channels (width small compared to the tidal excursion length) stable static equilibria exist if bottom friction is slightly larger than rcr. For channel widths more comparable to the tidal excursion length, multiple stable steady states may exist for bottom friction parameter values below rcr. Regardless of channel width, stable time-periodic equilibria seem to emerge as the bottom friction is increased.

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