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Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows
Capability and reliability of
models for reproducing the
physical processes associated
to debris flows phenomena
Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows
Schematic 2D view of a debris flow
event occurrence and development
Deposition
Debris flows commonly occur
in channels draining small
steep rock basins located in
the upper part of the slopes
where high intensity, short
duration rainfalls, rapidly
generate high runoff
discharges , that are able to
entrain large debris material
laying at the bottom of
channel, forming a solid-liquid
wave
RUNOFF
Firehose effect
debris flow triggering
Formation of an immature
debris flow
Debris flow increases its velocity
and erodes sediment s laying on
the bed
Formation of a mature debris flow
with sediment sorting along the
profile
Debris flow slows and
sediment deposition
starts
Rock
cliffs
Scree
sediment
Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows
Schematic 3D view of a debris flow
event occurrence and development
Initiation
area
Transport
area
deposition
area
Debris
material
availability
Very high
slopes
Abundant
runoff
Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows
In brief, a debris flow results from three different physical
processes
1. Abundant runoff production after high intensity
precipitation
2. Entrainment of debris material laying on the bottom of
channels with formation of a solid-liquid wave
3. Downstream routing of the solid-liquid wave
We need three different models for debris flow simulations:
1. Hydrologic model (Rainfall-Runoff) for rocky headwater
basins
2. Triggering model for determining the solid-liquid
hydrograph
3. Hydraulic model for downstream routing
Physical processes associated to debris flow
Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows
Reliability of the results of a simulation, mainly depends, on
model capabilities of reproducing measured quantities
(discharge, erosion and deposition depths, maximum reached
levels, routing times) of past-occurred events.
Hydrological models should be tested against discharge
measurements taken as close as possible to the feet of rocky
cliffs. Hydraulic models should be tested by comparing
simulated and measured/estimated erosion and depositon
depths, as well as the maximum levels reached by the mixture
free surface and routing times. Hydraulic models that do not
directly simulate erosion and deposition should not be
considered.
Models have to be tested

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04 affidabilita modelli_per colata_en

  • 1. Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows Capability and reliability of models for reproducing the physical processes associated to debris flows phenomena
  • 2. Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows Schematic 2D view of a debris flow event occurrence and development Deposition Debris flows commonly occur in channels draining small steep rock basins located in the upper part of the slopes where high intensity, short duration rainfalls, rapidly generate high runoff discharges , that are able to entrain large debris material laying at the bottom of channel, forming a solid-liquid wave RUNOFF Firehose effect debris flow triggering Formation of an immature debris flow Debris flow increases its velocity and erodes sediment s laying on the bed Formation of a mature debris flow with sediment sorting along the profile Debris flow slows and sediment deposition starts Rock cliffs Scree sediment
  • 3. Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows Schematic 3D view of a debris flow event occurrence and development Initiation area Transport area deposition area Debris material availability Very high slopes Abundant runoff
  • 4. Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows In brief, a debris flow results from three different physical processes 1. Abundant runoff production after high intensity precipitation 2. Entrainment of debris material laying on the bottom of channels with formation of a solid-liquid wave 3. Downstream routing of the solid-liquid wave We need three different models for debris flow simulations: 1. Hydrologic model (Rainfall-Runoff) for rocky headwater basins 2. Triggering model for determining the solid-liquid hydrograph 3. Hydraulic model for downstream routing Physical processes associated to debris flow
  • 5. Carlo Gregoretti25/5/2017 Mekelle University - Debris Flows Reliability of the results of a simulation, mainly depends, on model capabilities of reproducing measured quantities (discharge, erosion and deposition depths, maximum reached levels, routing times) of past-occurred events. Hydrological models should be tested against discharge measurements taken as close as possible to the feet of rocky cliffs. Hydraulic models should be tested by comparing simulated and measured/estimated erosion and depositon depths, as well as the maximum levels reached by the mixture free surface and routing times. Hydraulic models that do not directly simulate erosion and deposition should not be considered. Models have to be tested