Bedload transport remains largely unpredictable in steep slope rivers. Comparing experimental data obtained in a steep slope flume and a stochastic model, we show that bedload discharge statistics strongly depend on the measurement time and spatial scale. We base our talk on a flume experiment that resolved 7 orders of magnitude in time (from 10-2s to 105s) of solid discharge. Computing the variance of the mean solid discharge depending on the sampling time, we distinguished three successive time scales: (1) intermittent (2) correlated and (3) white noise limit. The intermittent time scale is the shortest and is characterized by long periods of time without any transport. Then, we observe a correlation time scale that spread over 3 order of...
The shaping of river beds by flowing water is an important problem in geophysics. Often, the process...
It is known that bedload fluctuates over time in steep rivers with wide grain size distributions, ev...
International audienceIn gravel bed rivers, bed load transport exhibits considerable variability in ...
Among the recent experimental studies focusing on the stochastic nature of bedload transport, some r...
Steep slope streams show large fluctuations of sediment discharge across several time scales. These ...
Large fluctuations in the sediment transport rate are observed in rivers, particularly in mountain s...
The use of geo-sensors in mountain rivers becomes more and more frequent. It provides valuable conti...
Sediment transport is one of the main morphodynamic processes in mountain streams. Understanding bed...
Bed load transport, the movement of sediment by water or air in close proximity to the river bed or ...
Describing bedload transport as a stochastic process is an idea that emerged in the 1930s with the p...
In mountain streams, bedload transport rates are prone to strong variability. Indeed an increasing n...
In mountain regions, steep streams play an important role in water and sediment connectivity. In the...
Temporal dynamics of sediment transport in steep channels using two experiments performed in a stee...
The transport of coarse material strongly controls the stability and evolution of mountain fluvial s...
During the last 20 years, numerous sediment transport flume experiments have shown that grain sortin...
The shaping of river beds by flowing water is an important problem in geophysics. Often, the process...
It is known that bedload fluctuates over time in steep rivers with wide grain size distributions, ev...
International audienceIn gravel bed rivers, bed load transport exhibits considerable variability in ...
Among the recent experimental studies focusing on the stochastic nature of bedload transport, some r...
Steep slope streams show large fluctuations of sediment discharge across several time scales. These ...
Large fluctuations in the sediment transport rate are observed in rivers, particularly in mountain s...
The use of geo-sensors in mountain rivers becomes more and more frequent. It provides valuable conti...
Sediment transport is one of the main morphodynamic processes in mountain streams. Understanding bed...
Bed load transport, the movement of sediment by water or air in close proximity to the river bed or ...
Describing bedload transport as a stochastic process is an idea that emerged in the 1930s with the p...
In mountain streams, bedload transport rates are prone to strong variability. Indeed an increasing n...
In mountain regions, steep streams play an important role in water and sediment connectivity. In the...
Temporal dynamics of sediment transport in steep channels using two experiments performed in a stee...
The transport of coarse material strongly controls the stability and evolution of mountain fluvial s...
During the last 20 years, numerous sediment transport flume experiments have shown that grain sortin...
The shaping of river beds by flowing water is an important problem in geophysics. Often, the process...
It is known that bedload fluctuates over time in steep rivers with wide grain size distributions, ev...
International audienceIn gravel bed rivers, bed load transport exhibits considerable variability in ...