In rivers which formed multi-row bars or braided rivers, riverbanks often have wavy shape on a scale of several times of river width. In such rivers, a wide width part (anti-node) and a narrow part (node) appear by turns in the longitudinal direction. The elucidation of this phenomenon accompanied by bank erosion is very important on river management works. However, the formation mechanism of a gourd type channel has not been clarified. This research conducts a linear stability analysis as the first step which clarifies the formation mechanism of such channels. As a result, it became clear that a gourd type wavelength is changed with hydraulic conditions
1982Final Report, Jan. -Oct. 1981Gilje, Stephen A.PDFTech ReportFHWA/RD-82/021P.O. No. DTFH61-81-P-3...
Our objective is to understand general causes of different river channel patterns. In this paper we ...
Rivers have been trained for centuries by channel narrowing and straightening. This caused important...
In order to stably maintain a river channel, the river channel form needs to suit its origin. Theref...
In this paper we propose a new theoretical model to investigate the influence of temporal changes in...
We study the steady three-dimensional flow field and bed topography in a channel with sinusoidally v...
Fluid Dynamics provides a sound insight to the geomorphologist interested in the ubiquitous formatio...
Rivers self-organize their pattern/planform through feedbacks between bars, channels, floodplain and...
The number of bars that form in an alluvial channel cross section can be determined from a physics-b...
The paper presents a linear perturbation analysis of a horizontal two-dimensional mathematical model...
The morphological behaviour of bifurcations in rivers is a poorly understood problem with which many...
A three dimensional quasi-analytical model is introduced to determine the flow field and the altimet...
A linear stability analysis of the governing equations for the bed and flow topography in straight a...
Channel network configurations are changed by hydraulic conditions. The characteristic of a river ch...
Braided rivers are characterized by multiple, unstable channel and ephemeral bars formed by intense ...
1982Final Report, Jan. -Oct. 1981Gilje, Stephen A.PDFTech ReportFHWA/RD-82/021P.O. No. DTFH61-81-P-3...
Our objective is to understand general causes of different river channel patterns. In this paper we ...
Rivers have been trained for centuries by channel narrowing and straightening. This caused important...
In order to stably maintain a river channel, the river channel form needs to suit its origin. Theref...
In this paper we propose a new theoretical model to investigate the influence of temporal changes in...
We study the steady three-dimensional flow field and bed topography in a channel with sinusoidally v...
Fluid Dynamics provides a sound insight to the geomorphologist interested in the ubiquitous formatio...
Rivers self-organize their pattern/planform through feedbacks between bars, channels, floodplain and...
The number of bars that form in an alluvial channel cross section can be determined from a physics-b...
The paper presents a linear perturbation analysis of a horizontal two-dimensional mathematical model...
The morphological behaviour of bifurcations in rivers is a poorly understood problem with which many...
A three dimensional quasi-analytical model is introduced to determine the flow field and the altimet...
A linear stability analysis of the governing equations for the bed and flow topography in straight a...
Channel network configurations are changed by hydraulic conditions. The characteristic of a river ch...
Braided rivers are characterized by multiple, unstable channel and ephemeral bars formed by intense ...
1982Final Report, Jan. -Oct. 1981Gilje, Stephen A.PDFTech ReportFHWA/RD-82/021P.O. No. DTFH61-81-P-3...
Our objective is to understand general causes of different river channel patterns. In this paper we ...
Rivers have been trained for centuries by channel narrowing and straightening. This caused important...