The surfaces of alluvial fans and river deltas (collectively fans) are often dissected by a small number of channels radiating from the fan apex. On long timescales, channels migrate via avulsion, the process of channel bed deposition and abandonment that often results in catastrophic flooding and loss of life on densely populated fans. We present results of an experimental fan that creates realistic channel patterns by avulsion. The avulsion cycle occurs with a period that is predictable from conservation of mass. Selection of a new flow path is inherently stochastic; however, once a network of 4–5 channels is established, flow oscillates among these channels indefinitely. We demonstrate that a directed random walk model with memory quanti...
Alluvial fans, conic depositional landforms that develop where headwater streams outlet into a main ...
Fan deltas are excellent recorders of fan-building processes because of their high sedimentation rat...
Abstract. The stochastic field of sediment supply to the channel network of a drainage basin depends...
The surfaces of alluvial fans and river deltas (collectively fans) are often dissected by a small nu...
River deltas and alluvial fans have channelization and deposition dynamics that are not entirely und...
The dynamic behaviour of channels on alluvial fans can present hazards to infrastructure and human l...
Alluvial fans develop their semi-conical shape by quasi-cyclic avulsions of their geomorphologically...
Dryland river fans form by repeated switching (avulsion) of an ephemeral stream as it progrades and ...
Shifts in the active channel on a debris-flow fan, termed avulsions, pose a large threat because new...
Debris flows are water-laden masses of sediment that move rapidly through channel networks and over ...
Debris-flow fans form by shifts of the active channel, termed avulsions. Field and experimental evid...
Decades of historic levels of urbanization and expansion of the built environment on to existing all...
A digital model based on a random walk was used in an experiment to determine how well such a model ...
A digital model based on a random walk was used in an experiment to determine how well such a model ...
This thesis presents the investigation of a series of patterns observed on the Earth\u27s surface, w...
Alluvial fans, conic depositional landforms that develop where headwater streams outlet into a main ...
Fan deltas are excellent recorders of fan-building processes because of their high sedimentation rat...
Abstract. The stochastic field of sediment supply to the channel network of a drainage basin depends...
The surfaces of alluvial fans and river deltas (collectively fans) are often dissected by a small nu...
River deltas and alluvial fans have channelization and deposition dynamics that are not entirely und...
The dynamic behaviour of channels on alluvial fans can present hazards to infrastructure and human l...
Alluvial fans develop their semi-conical shape by quasi-cyclic avulsions of their geomorphologically...
Dryland river fans form by repeated switching (avulsion) of an ephemeral stream as it progrades and ...
Shifts in the active channel on a debris-flow fan, termed avulsions, pose a large threat because new...
Debris flows are water-laden masses of sediment that move rapidly through channel networks and over ...
Debris-flow fans form by shifts of the active channel, termed avulsions. Field and experimental evid...
Decades of historic levels of urbanization and expansion of the built environment on to existing all...
A digital model based on a random walk was used in an experiment to determine how well such a model ...
A digital model based on a random walk was used in an experiment to determine how well such a model ...
This thesis presents the investigation of a series of patterns observed on the Earth\u27s surface, w...
Alluvial fans, conic depositional landforms that develop where headwater streams outlet into a main ...
Fan deltas are excellent recorders of fan-building processes because of their high sedimentation rat...
Abstract. The stochastic field of sediment supply to the channel network of a drainage basin depends...