This study presents the small scale bedform states found off the South-Holland coast during a 31+ days field observation of seabed acoustic imagery and near the bed velocities. Six main bed states were encountered: current ripples (C), wave ripples (W), combined wave-current ripples (WC), current ripples with subordinate wave ripples (Cw), wave ripples with subordinate current ripples (Wc) and poorly developed ripples (P). Direct visual detection of the bed state from the images showed good agreement with a simple predictor based on the mobility number. The most frequent type of bedform was C which is governed by the tidal currents. Wave ripple prevailed only during a storm with waves higher than 2 m. The combined Cw, WC and Wc types compri...
Sand grains, bedforms and the wave boundary layer cause roughness for tidal currents. This paper rep...
Hydrodynamic, suspension and bed-form measurements were made 2 km off the Dutch coast near Noordwijk...
Abstract. For the first time a prediction model of regular morphological patterns on the seabed was ...
Sandy beds of shallow tidal seas often exhibit a range of rhythmic patterns, from small‐scale ripple...
Ebb-tidal deltas are highly dynamic environments affected by both waves and currents that approach t...
Small-scale beach morphology (scales < 5 m) height variations were measured by combining the CRAB su...
This report presents data on forty three bedforms generated onmedium to coarse sandy beds under natu...
Sorted bedforms can be found in coastal shelf seas worldwide. These spatially-grain-size-sorted bedf...
Large bedforms were studied along a 20 km transect from upper shoreface (12 m depth) to upper shelf ...
The lower shoreface, with water depths between about 8 and 20 m, forms the transition between the in...
Sorted bedforms are ubiquitous on the inner continental shelves worldwide. They are described as spa...
The ability to predict the presence and physical properties of small-scale sand ripples on the sea b...
Self-recording current meter data have revealed patterns of water movement in the vicinity of the Br...
Sandy shallow seas, like the North Sea, are very dynamic. Several morphological features are present...
Trembanis, Arthur C.The hydrodynamics and seabed morphodynamics on the inner continental shelf are h...
Sand grains, bedforms and the wave boundary layer cause roughness for tidal currents. This paper rep...
Hydrodynamic, suspension and bed-form measurements were made 2 km off the Dutch coast near Noordwijk...
Abstract. For the first time a prediction model of regular morphological patterns on the seabed was ...
Sandy beds of shallow tidal seas often exhibit a range of rhythmic patterns, from small‐scale ripple...
Ebb-tidal deltas are highly dynamic environments affected by both waves and currents that approach t...
Small-scale beach morphology (scales < 5 m) height variations were measured by combining the CRAB su...
This report presents data on forty three bedforms generated onmedium to coarse sandy beds under natu...
Sorted bedforms can be found in coastal shelf seas worldwide. These spatially-grain-size-sorted bedf...
Large bedforms were studied along a 20 km transect from upper shoreface (12 m depth) to upper shelf ...
The lower shoreface, with water depths between about 8 and 20 m, forms the transition between the in...
Sorted bedforms are ubiquitous on the inner continental shelves worldwide. They are described as spa...
The ability to predict the presence and physical properties of small-scale sand ripples on the sea b...
Self-recording current meter data have revealed patterns of water movement in the vicinity of the Br...
Sandy shallow seas, like the North Sea, are very dynamic. Several morphological features are present...
Trembanis, Arthur C.The hydrodynamics and seabed morphodynamics on the inner continental shelf are h...
Sand grains, bedforms and the wave boundary layer cause roughness for tidal currents. This paper rep...
Hydrodynamic, suspension and bed-form measurements were made 2 km off the Dutch coast near Noordwijk...
Abstract. For the first time a prediction model of regular morphological patterns on the seabed was ...