During the last ten years coherent characteristics of large scale turbulence in boundarylayers have been made clear. The results of these studies encouraged the authors to study thestructures of large scale turbulence with the intention of applying the result to practical riverengineering.On the other hand, it is suggested that there exist secondary flows in river flows and theyplay an important role in fluvial process. But it has been considered that a secondary flow isone thing and large scale turbulence is another.In this paper, a flow model is proposed, by which generation and development of turbu -lence as well as energy cascade process can be elucidated. Furthermore, it is shown that thesecondary flow is a phase of large scale turbule...
Turbulent flow in a rec;tangular channel flow is investigated to determine the scale and pattern of ...
An investigation into the behaviour of the turbulence during laboratory simulations of floods in riv...
River channels modify their boundaries by entrainment and transfer of sediment. The flow represents ...
The laboratory and full-scale experiments have been performed. The block diagrams of the river turbu...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Spur dikes provide significant control for flow regimes in river regulation engineering, which can h...
The study of turbulence has always been a challenge for scientists working on geophysical flows. Tur...
The study of turbulence has always been a challenge for scientists working on geophysical flows. Tur...
The study of turbulence has always been a challenge for scientists working on geophysical flows. Tur...
We investigate the flow dynamics around a rock vane, a widely used instream structure for stream res...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Direct numerical simulations were carried out to investigate the spatial features of large- and very...
Turbulent flow in a rec;tangular channel flow is investigated to determine the scale and pattern of ...
An investigation into the behaviour of the turbulence during laboratory simulations of floods in riv...
River channels modify their boundaries by entrainment and transfer of sediment. The flow represents ...
The laboratory and full-scale experiments have been performed. The block diagrams of the river turbu...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Spur dikes provide significant control for flow regimes in river regulation engineering, which can h...
The study of turbulence has always been a challenge for scientists working on geophysical flows. Tur...
The study of turbulence has always been a challenge for scientists working on geophysical flows. Tur...
The study of turbulence has always been a challenge for scientists working on geophysical flows. Tur...
We investigate the flow dynamics around a rock vane, a widely used instream structure for stream res...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Large-eddy simulation (LES) is a method for resolving the time-dependent structure of high Reynolds ...
Direct numerical simulations were carried out to investigate the spatial features of large- and very...
Turbulent flow in a rec;tangular channel flow is investigated to determine the scale and pattern of ...
An investigation into the behaviour of the turbulence during laboratory simulations of floods in riv...
River channels modify their boundaries by entrainment and transfer of sediment. The flow represents ...