4.7 Review

Debris-flow monitoring and warning: Review and examples

期刊

EARTH-SCIENCE REVIEWS
卷 199, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.earscirev.2019.102981

关键词

Debris flow; Monitoring; Sensor; Hazard; Warning

资金

  1. JSPS program for fostering globally talented researchers [G2901]
  2. Civil Protection Agency of the Autonomous Province of Bozen-Bolzano
  3. EFRE-FESR project SEDIPLAN-r
  4. SMuCPhy project of the Spain Government [BIA 2015-67500-R]
  5. AEI/FEDER
  6. SedAlp Project (INTERREG Alpine Space Program) [1-4-3-AT]

向作者/读者索取更多资源

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.

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