To explain the genesis, dynamics, morphology, and evolution of bedforms found in sandy inner-shelf environments, with emphasis on those bedforms that affect the penetration of sound into the seabed. OBJECTIVES We seek to improve our understanding of the relationships between hydrodynamics and sediment motion near the seabed, as well as develop models for nearshore sediment transport derived from our understanding of the relevant physical processes. This requires coupling between hydrodynamic forcing, bedform response and feedback, bedload sediment transport response, and the suspended sediment response. APPROACH We use a combination of field observations, laboratory experiments, and numerical modeling to determine the relationships between ...
Bedform roughness, caused by ripples on the seabed, plays an important role in controlling sediment ...
The long-range goals of this program are to improve our understanding of the processes and physical ...
Trembanis, Arthur C.The complex morphodynamics of the inner continental shelf present challenges to ...
To understand the physics of sediment transport by waves and currents and to use that understanding ...
Sediment bedload transport and bedform formation are considered for both steady and oscillatory flow...
The littoral zone plays an integral role in the success of today’s thriving society, providing a sta...
Understanding the behaviour of bedforms and the related sediment transport is a key issue in coastal...
Trembanis, Arthur C.The hydrodynamics and seabed morphodynamics on the inner continental shelf are h...
Ripple formation beneath sea waves is analyzed both by experimental and analytical means when the bo...
529-537Laboratory experiments using a wave flume were designed to examine the characteristics of rip...
International audiencePredicting the evolution of mound formations in the nearshore, both natural (e...
Sea ripples are small-scale bedforms which originate from the interaction of an oscillatory flow wit...
The focus of this thesis is on the morphodynamics of shoreface-connected sand ridges, which are larg...
Observations of bedforms, suspended sediment and water velocities were used to examine sediment tran...
[1] We investigate the spatial and temporal distribution of suspended sediment and the associated hy...
Bedform roughness, caused by ripples on the seabed, plays an important role in controlling sediment ...
The long-range goals of this program are to improve our understanding of the processes and physical ...
Trembanis, Arthur C.The complex morphodynamics of the inner continental shelf present challenges to ...
To understand the physics of sediment transport by waves and currents and to use that understanding ...
Sediment bedload transport and bedform formation are considered for both steady and oscillatory flow...
The littoral zone plays an integral role in the success of today’s thriving society, providing a sta...
Understanding the behaviour of bedforms and the related sediment transport is a key issue in coastal...
Trembanis, Arthur C.The hydrodynamics and seabed morphodynamics on the inner continental shelf are h...
Ripple formation beneath sea waves is analyzed both by experimental and analytical means when the bo...
529-537Laboratory experiments using a wave flume were designed to examine the characteristics of rip...
International audiencePredicting the evolution of mound formations in the nearshore, both natural (e...
Sea ripples are small-scale bedforms which originate from the interaction of an oscillatory flow wit...
The focus of this thesis is on the morphodynamics of shoreface-connected sand ridges, which are larg...
Observations of bedforms, suspended sediment and water velocities were used to examine sediment tran...
[1] We investigate the spatial and temporal distribution of suspended sediment and the associated hy...
Bedform roughness, caused by ripples on the seabed, plays an important role in controlling sediment ...
The long-range goals of this program are to improve our understanding of the processes and physical ...
Trembanis, Arthur C.The complex morphodynamics of the inner continental shelf present challenges to ...