Debris-flow monitoring and warning: Review and examples

Debris flows represent one of the most dangerous types of mass movements, because of their high velocities, large impact forces and long runout distances. This review describes the available debris-flow monitoring techniques and proposes recommendations to inform the design of future monitoring and...

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Vydáno v:Earth-science reviews Ročník 199; s. 102981
Hlavní autoři: Hürlimann, Marcel, Coviello, Velio, Bel, Coraline, Guo, Xiaojun, Berti, Matteo, Graf, Christoph, Hübl, Johannes, Miyata, Shusuke, Smith, Joel B., Yin, Hsiao-Yuan
Médium: Journal Article
Jazyk:angličtina
Vydáno: Elsevier B.V 01.12.2019
Elsevier
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ISSN:0012-8252, 1872-6828
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Abstract Debris flows represent one of the most dangerous types of mass movements, because of their high velocities, large impact forces and long runout distances. This review describes the available debris-flow monitoring techniques and proposes recommendations to inform the design of future monitoring and warning/alarm systems. The selection and application of these techniques is highly dependent on site and hazard characterization, which is illustrated through detailed descriptions of nine monitoring sites: five in Europe, three in Asia and one in the USA. Most of these monitored catchments cover less than ∼10km2 and are topographically rugged with Melton Indices greater than 0.5. Hourly rainfall intensities between 5 and 15mm/h are sufficient to trigger debris flows at many of the sites, and observed debris-flow volumes range from a few hundred up to almost one million cubic meters. The sensors found in these monitoring systems can be separated into two classes: a class measuring the initiation mechanisms, and another class measuring the flow dynamics. The first class principally includes rain gauges, but also contains of soil moisture and pore-water pressure sensors. The second class involves a large variety of sensors focusing on flow stage or ground vibrations and commonly includes video cameras to validate and aid in the data interpretation. Given the sporadic nature of debris flows, an essential characteristic of the monitoring systems is the differentiation between a continuous mode that samples at low frequency (“non-event mode”) and another mode that records the measurements at high frequency (“event mode”). The event detection algorithm, used to switch into the “event mode” depends on a threshold that is typically based on rainfall or ground vibration. Identifying the correct definition of these thresholds is a fundamental task not only for monitoring purposes, but also for the implementation of warning and alarm systems.
AbstractList Debris flows represent one of the most dangerous types of mass movements, because of their high velocities, large impact forces and long runout distances. This review describes the available debris-flow monitoring techniques and proposes recommendations to inform the design of future monitoring and warning/alarm systems. The selection and application of these techniques is highly dependent on site and hazard characterization, which is illustrated through detailed descriptions of nine monitoring sites: five in Europe, three in Asia and one in the USA. Most of these monitored catchments cover less than ∼10km² and are topographically rugged with Melton Indices greater than 0.5. Hourly rainfall intensities between 5 and 15mm/h are sufficient to trigger debris flows at many of the sites, and observed debris-flow volumes range from a few hundred up to almost one million cubic meters. The sensors found in these monitoring systems can be separated into two classes: a class measuring the initiation mechanisms, and another class measuring the flow dynamics. The first class principally includes rain gauges, but also contains of soil moisture and pore-water pressure sensors. The second class involves a large variety of sensors focusing on flow stage or ground vibrations and commonly includes video cameras to validate and aid in the data interpretation. Given the sporadic nature of debris flows, an essential characteristic of the monitoring systems is the differentiation between a continuous mode that samples at low frequency (“non-event mode”) and another mode that records the measurements at high frequency (“event mode”). The event detection algorithm, used to switch into the “event mode” depends on a threshold that is typically based on rainfall or ground vibration. Identifying the correct definition of these thresholds is a fundamental task not only for monitoring purposes, but also for the implementation of warning and alarm systems.
Debris flows represent one of the most dangerous types of mass movements, because of their high velocities, large impact forces and long runout distances. This review describes the available debris-flow monitoring techniques and proposes recommendations to inform the design of future monitoring and warning/alarm systems. The selection and application of these techniques is highly dependent on site and hazard characterization, which is illustrated through detailed descriptions of nine monitoring sites: five in Europe, three in Asia and one in the USA. Most of these monitored catchments cover less than similar to 10 km(2) and are topographically rugged with Melton Indices greater than 0.5. Hourly rainfall intensities between 5 and 15 mm/h are sufficient to trigger debris flows at many of the sites, and observed debris-flow volumes range from a few hundred up to almost one million cubic meters. The sensors found in these monitoring systems can be separated into two classes: a class measuring the initiation mechanisms, and another class measuring the flow dynamics. The first class principally includes rain gauges, but also contains of soil moisture and pore-water pressure sensors. The second class involves a large variety of sensors focusing on flow stage or ground vibrations and commonly includes video cameras to validate and aid in the data interpretation. Given the sporadic nature of debris flows, an essential characteristic of the monitoring systems is the differentiation between a continuous mode that samples at low frequency ("non-event mode") and another mode that records the measurements at high frequency ("event mode"). The event detection algorithm, used to switch into the "event mode" depends on a threshold that is typically based on rainfall or ground vibration. Identifying the correct definition of these thresholds is a fundamental task not only for monitoring purposes, but also for the implementation of warning and alarm systems.
Debris flows represent one of the most dangerous types of mass movements, because of their high velocities, large impact forces and long runout distances. This review describes the available debris-flow monitoring techniques and proposes recommendations to inform the design of future monitoring and warning/alarm systems. The selection and application of these techniques is highly dependent on site and hazard characterization, which is illustrated through detailed descriptions of nine monitoring sites: five in Europe, three in Asia and one in the USA. Most of these monitored catchments cover less than ∼10km2 and are topographically rugged with Melton Indices greater than 0.5. Hourly rainfall intensities between 5 and 15mm/h are sufficient to trigger debris flows at many of the sites, and observed debris-flow volumes range from a few hundred up to almost one million cubic meters. The sensors found in these monitoring systems can be separated into two classes: a class measuring the initiation mechanisms, and another class measuring the flow dynamics. The first class principally includes rain gauges, but also contains of soil moisture and pore-water pressure sensors. The second class involves a large variety of sensors focusing on flow stage or ground vibrations and commonly includes video cameras to validate and aid in the data interpretation. Given the sporadic nature of debris flows, an essential characteristic of the monitoring systems is the differentiation between a continuous mode that samples at low frequency (“non-event mode”) and another mode that records the measurements at high frequency (“event mode”). The event detection algorithm, used to switch into the “event mode” depends on a threshold that is typically based on rainfall or ground vibration. Identifying the correct definition of these thresholds is a fundamental task not only for monitoring purposes, but also for the implementation of warning and alarm systems.
ArticleNumber 102981
Author Hürlimann, Marcel
Miyata, Shusuke
Bel, Coraline
Guo, Xiaojun
Yin, Hsiao-Yuan
Hübl, Johannes
Berti, Matteo
Coviello, Velio
Graf, Christoph
Smith, Joel B.
Author_xml – sequence: 1
  givenname: Marcel
  surname: Hürlimann
  fullname: Hürlimann, Marcel
  email: marcel.hurlimann@upc.edu
  organization: Department Division of Geotechnical Engineering and Geosciences, Department of Civil and Environmental Engineering UPC BarcelonaTECH, Barcelona, Spain
– sequence: 2
  givenname: Velio
  surname: Coviello
  fullname: Coviello, Velio
  organization: Faculty of Science and Technology, Free University of Bozen-Bolzano, Italy
– sequence: 3
  givenname: Coraline
  surname: Bel
  fullname: Bel, Coraline
  organization: Université Grenoble Alpes, Irstea, UR ETNA, St-Martin-d’Hères, France
– sequence: 4
  givenname: Xiaojun
  surname: Guo
  fullname: Guo, Xiaojun
  organization: Key Laboratory of Mountain Surface Process and Hazards/Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, China
– sequence: 5
  givenname: Matteo
  surname: Berti
  fullname: Berti, Matteo
  organization: Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Università di Bologna, Bologna, Italy
– sequence: 6
  givenname: Christoph
  surname: Graf
  fullname: Graf, Christoph
  organization: Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf, Switzerland
– sequence: 7
  givenname: Johannes
  surname: Hübl
  fullname: Hübl, Johannes
  organization: Institute of Mountain Risk Engineering, Department of Natural Hazards and Civil Engineering, University of Natural Resources and Life Sciences (BOKU), Vienna, Austria
– sequence: 8
  givenname: Shusuke
  surname: Miyata
  fullname: Miyata, Shusuke
  organization: Disaster Prevention Research Institute, Kyoto University, Takayama, Japan
– sequence: 9
  givenname: Joel B.
  surname: Smith
  fullname: Smith, Joel B.
  organization: U.S. Geological Survey, Landslide Hazards Program, Geologic Hazards Science Center, Golden, USA
– sequence: 10
  givenname: Hsiao-Yuan
  surname: Yin
  fullname: Yin, Hsiao-Yuan
  organization: Soil and Water Conservation Bureau, Council of Agriculture, Nantou, Taiwan
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Snippet Debris flows represent one of the most dangerous types of mass movements, because of their high velocities, large impact forces and long runout distances. This...
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SubjectTerms alarm systems
algorithms
Asia
Debris flow
Environmental Sciences
Europe
Hazard
hazard characterization
hydrodynamics
mass movement
Monitoring
rain
rain gauges
rain intensity
Sensor
soil water
United States
vibration
video cameras
Warning
watersheds
Title Debris-flow monitoring and warning: Review and examples
URI https://dx.doi.org/10.1016/j.earscirev.2019.102981
https://www.proquest.com/docview/2352427197
https://hal.inrae.fr/hal-02610274
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