Vertical swimming in wave-induced currents as a control mechanism of intertidal migration by a sand-beach isopod

1991 ◽  
Vol 111 (1) ◽  
pp. 49-54 ◽  
Author(s):  
C. G. Warman ◽  
T. J. O'Hare ◽  
E. Naylor
Keyword(s):  
Control Mechanism ◽  
Sand Beach ◽  
Induced Currents ◽  
Wave Induced

scholarly journals Numerical simulation of the three-dimensional wave-induced currents on unstructured grid

2017 ◽  
Vol 31 (5) ◽  
pp. 539-548
Author(s):  
Ping Wang ◽  
Ning-chuan Zhang ◽  
Shuai Yuan ◽  
Wei-bin Chen
Keyword(s):  
Numerical Simulation ◽  
Unstructured Grid ◽  
Three Dimensional ◽  
Induced Currents ◽  
Wave Induced ◽  
Dimensional Wave

scholarly journals Predictive model for wave-induced currents and 3D beach evolution based on FAVOR Method

2010 ◽  
Vol 2 (2) ◽  
pp. 68-74
Author(s):  
Masamitsu Kuroiwa ◽  
Mazen Abualtayef ◽  
Tetsushi Takada ◽  
Ahmed Khaled Sief ◽  
Yuehi Matsubara
Keyword(s):  
Predictive Model ◽  
Induced Currents ◽  
Wave Induced

Sediment Resuspension and Transport by Internal Solitary Waves

2019 ◽  
Vol 51 (1) ◽  
pp. 129-154 ◽  
Author(s):  
Leon Boegman ◽  
Marek Stastna
Keyword(s):  
Internal Waves ◽  
Laboratory Experiments ◽  
Sediment Resuspension ◽  
Vital Role ◽  
Continental Margins ◽  
Scale Models ◽  
Key Driver ◽  
Induced Currents ◽  
Wave Induced ◽  
Oriented Research

Large-amplitude internal waves induce currents and turbulence in the bottom boundary layer (BBL) and are thus a key driver of sediment movement on the continental margins. Observations of internal wave–induced sediment resuspension and transport cover significant portions of the world's oceans. Research on BBL instabilities, induced by internal waves, has identified several mechanisms by which the BBL is energized and sediment may be resuspended. Due to the complexity of the induced currents, process-oriented research using theory, direct numerical simulations, and laboratory experiments has played a vital role. However, experiments and simulations have inherent limitations as analogs for oceanic conditions due to disparities in Reynolds number and grid resolution, respectively. Parameterizations are needed for modeling resuspension from observed data and in larger-scale models, with the efficacy of parameterizations based on the quadratic stress largely determining the accuracy of present field-scale efforts.

Waves transformations on the continental shelf and wave induced currents

2017 ◽  
pp. 99-133
Author(s):  
Valéria Souza Rego ◽  
Gabriel Clauzet ◽  
Murray Burling ◽  
Clarissa Brelinger de Luca ◽  
Eduardo Ayres Yassuda
Keyword(s):  
Continental Shelf ◽  
Induced Currents ◽  
Wave Induced
Sign in / Sign up

Export Citation Format

Share Document