We consider a deterministic model of landscape evolution through the mechanism of overland flow over an erodible substrate, using the St. Venant equations of hydraulics together with the Exner equation for hillslope erosion. A novelty in the model is the allowance for a nonzero bedload layer thickness, which is necessary to distinguish between transport limited and detachment limited sediment removal. It has long been known that transport limited uniform flow is unstable when the hillslope topography is geomorphologically concave (i.e., the center of curvature is above ground). In this paper, we show how finite amplitude development of the consequent channel flow leads to an evolution equation for its depth h of the form ht = h3/2 + (h3/2)Y...
A topographic steering river meandering (TSRM) model based on continuity of a simplified flow field ...
The importance of including floodplain effects in one-dimensional river channel hydraulic computatio...
The bank-full depths, widths, depth-averaged water velocities, and along-channel slopes of alluvial ...
We consider a deterministic model of landscape evolution through the mechanism of overland flow over...
We consider a deterministic model of landscape evolution through the mechanism of overland flow over...
Abstract. We consider a deterministic model of landscape evolution through the mechanism of overland...
peer-reviewedWe consider a deterministic model of landscape evolution through the mechanism of overl...
The study of overland flow of water over an erodible sediment leads to a coupled model describing th...
The landscape around us has been formed over periods of million, s of years by the erosion of the la...
The study of overland flow of water over an erodible sediment leads to a coupled model describing th...
The study of overland flow of water over an erodible sediment leads to a coupled model describing th...
A coupled model describing the evolution of the topographic elevation and the depth of the overland ...
A coupled model describing the evolution of the topographic elevation and the depth of the overland ...
This is a poster presented on May 23rd, 2018 at the Community Surface Dynamics Modeling System (CSDM...
ABSTRACT. The geomorphic evolution of many landscapes is fundamentally deter-mined by the evolution ...
A topographic steering river meandering (TSRM) model based on continuity of a simplified flow field ...
The importance of including floodplain effects in one-dimensional river channel hydraulic computatio...
The bank-full depths, widths, depth-averaged water velocities, and along-channel slopes of alluvial ...
We consider a deterministic model of landscape evolution through the mechanism of overland flow over...
We consider a deterministic model of landscape evolution through the mechanism of overland flow over...
Abstract. We consider a deterministic model of landscape evolution through the mechanism of overland...
peer-reviewedWe consider a deterministic model of landscape evolution through the mechanism of overl...
The study of overland flow of water over an erodible sediment leads to a coupled model describing th...
The landscape around us has been formed over periods of million, s of years by the erosion of the la...
The study of overland flow of water over an erodible sediment leads to a coupled model describing th...
The study of overland flow of water over an erodible sediment leads to a coupled model describing th...
A coupled model describing the evolution of the topographic elevation and the depth of the overland ...
A coupled model describing the evolution of the topographic elevation and the depth of the overland ...
This is a poster presented on May 23rd, 2018 at the Community Surface Dynamics Modeling System (CSDM...
ABSTRACT. The geomorphic evolution of many landscapes is fundamentally deter-mined by the evolution ...
A topographic steering river meandering (TSRM) model based on continuity of a simplified flow field ...
The importance of including floodplain effects in one-dimensional river channel hydraulic computatio...
The bank-full depths, widths, depth-averaged water velocities, and along-channel slopes of alluvial ...