Accurate debris-flow modelling depends on the ability to simulate surging and pulsing behaviour. However, our understanding of these phenomena is starved of observational constraints. Here we propose the use of seismic measurements, which resolve the arrival of coarse-grained roll wave fronts in debris flows at Illgraben, Switzerland. Roll waves likely play a key role in flow pulses but are typically only observed with point measurements like depth gauges. We compare in-torrent force plate measurements with near-torrent seismic records and discuss how these data can test existing roll wave theories
International audienceIn the upper part of mountain river catchments, large amounts of loose debris ...
International audienceIn seismology, the signal is usually analysed for earthquake data, but earthqu...
Data and movies of experiments described in De Haas et al. (2021): Deciphering seismic and normal-fo...
Accurate debris-flow modelling depends on the ability to simulate surging and pulsing behaviour. How...
In natural debris flows, even if the critical Froude number is almost always exceeded, the formation...
Debris flows induce seismic ground unrest detectable over large distances. However, recent theoretic...
Quantifying debris-flow characteristics remains a key challenge in natural hazard research. Recent s...
Heavy precipitation can mobilize tens to hundreds of thousands of cubic meters of sediment in steep ...
International audienceHeavy precipitation can mobilize tens to hundreds of thousands of cubic meters...
Debris flows are gravity-driven mass movements that are common natural hazards in mountain regions w...
The objective of this contribution is to analyse the formation of debris waves in natural channels. ...
Debris flows generate seismic waves as they travel downslope and can become more dangerous as they e...
International audienceAn experimental approach to examine the instabilities present on free surfaces...
International audienceIn the upper part of mountain river catchments, large amounts of loose debris ...
International audienceIn seismology, the signal is usually analysed for earthquake data, but earthqu...
Data and movies of experiments described in De Haas et al. (2021): Deciphering seismic and normal-fo...
Accurate debris-flow modelling depends on the ability to simulate surging and pulsing behaviour. How...
In natural debris flows, even if the critical Froude number is almost always exceeded, the formation...
Debris flows induce seismic ground unrest detectable over large distances. However, recent theoretic...
Quantifying debris-flow characteristics remains a key challenge in natural hazard research. Recent s...
Heavy precipitation can mobilize tens to hundreds of thousands of cubic meters of sediment in steep ...
International audienceHeavy precipitation can mobilize tens to hundreds of thousands of cubic meters...
Debris flows are gravity-driven mass movements that are common natural hazards in mountain regions w...
The objective of this contribution is to analyse the formation of debris waves in natural channels. ...
Debris flows generate seismic waves as they travel downslope and can become more dangerous as they e...
International audienceAn experimental approach to examine the instabilities present on free surfaces...
International audienceIn the upper part of mountain river catchments, large amounts of loose debris ...
International audienceIn seismology, the signal is usually analysed for earthquake data, but earthqu...
Data and movies of experiments described in De Haas et al. (2021): Deciphering seismic and normal-fo...