Especially in mountainous environments, the prediction of sediment dynamics is important for managing natural hazards, assessing in-stream habitats and understanding geomorphic evolution. We present the new modelling tool {sedFlow} for simulating fractional bedload transport dynamics in mountain streams. sedFlow is a one-dimensional model that aims to realistically reproduce the total transport volumes and overall morphodynamic changes resulting from sediment transport events such as major floods. The model is intended for temporal scales from the individual event (several hours to few days) up to longer-term evolution of stream channels (several years). The envisaged spatial scale covers complete catchments at a spatial discretisation of s...
textUnderstanding how individual grains and populations of grains move through alluvial systems is i...
Geschiebeführende Hochwässer haben ein hohes Schadenspotential. Insbesondere bewohnte Schwemmkegel s...
The paper shows a mathematical model for the evaluation of the morphological changes in the transiti...
Especially in mountainous environments, the prediction of sediment dynamics is important for m...
Fully validated numerical models specifically designed for simulating bedload transport dynamics in ...
Sediment yield from mountain basins and solid transport in rivers are widely studied and still repre...
In mountain regions, steep streams play an important role in water and sediment connectivity. In the...
Large, episodically occurring sediment supply events may temporarily dominate channel morphology and...
Researchers and managers have sought for centuries to model the dynamics of river systems for hazard...
In mountain streams, bedload transport rates are prone to strong variability. Indeed an increasing n...
Sediment transport is one of the main morphodynamic processes in mountain streams. Understanding bed...
Rivers and streams with the flow, sediment, and habitat seasonality are termed as intermittent river...
Describing bedload transport as a stochastic process is an idea that emerged in the 1930s with the p...
The numerical 1-D HEC-RAS modelling tool was supported by the estimation of the sieve curve changes ...
The transport of coarse material strongly controls the stability and evolution of mountain fluvial s...
textUnderstanding how individual grains and populations of grains move through alluvial systems is i...
Geschiebeführende Hochwässer haben ein hohes Schadenspotential. Insbesondere bewohnte Schwemmkegel s...
The paper shows a mathematical model for the evaluation of the morphological changes in the transiti...
Especially in mountainous environments, the prediction of sediment dynamics is important for m...
Fully validated numerical models specifically designed for simulating bedload transport dynamics in ...
Sediment yield from mountain basins and solid transport in rivers are widely studied and still repre...
In mountain regions, steep streams play an important role in water and sediment connectivity. In the...
Large, episodically occurring sediment supply events may temporarily dominate channel morphology and...
Researchers and managers have sought for centuries to model the dynamics of river systems for hazard...
In mountain streams, bedload transport rates are prone to strong variability. Indeed an increasing n...
Sediment transport is one of the main morphodynamic processes in mountain streams. Understanding bed...
Rivers and streams with the flow, sediment, and habitat seasonality are termed as intermittent river...
Describing bedload transport as a stochastic process is an idea that emerged in the 1930s with the p...
The numerical 1-D HEC-RAS modelling tool was supported by the estimation of the sieve curve changes ...
The transport of coarse material strongly controls the stability and evolution of mountain fluvial s...
textUnderstanding how individual grains and populations of grains move through alluvial systems is i...
Geschiebeführende Hochwässer haben ein hohes Schadenspotential. Insbesondere bewohnte Schwemmkegel s...
The paper shows a mathematical model for the evaluation of the morphological changes in the transiti...