Engineering Geology for Society and Territory - Volume 3 2014
DOI: 10.1007/978-3-319-09054-2_14
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One Year Use of High-Frequency RADAR Technology in Alpine Mass Movement Monitoring: Principles and Performance for Torrential Activities

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Cited by 12 publications
(10 citation statements)
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“…Mass movement-generated infrasound signals have specific amplitude and occupy a frequency band from 0.001 to 20 Hz (e.g. Kogelnig 2012). Infrasound can travel thousands of kilometres and remain detectable over such distances.…”
Section: Infrasound Signals Of Avalanchesmentioning
confidence: 99%
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“…Mass movement-generated infrasound signals have specific amplitude and occupy a frequency band from 0.001 to 20 Hz (e.g. Kogelnig 2012). Infrasound can travel thousands of kilometres and remain detectable over such distances.…”
Section: Infrasound Signals Of Avalanchesmentioning
confidence: 99%
“…The signal is recorded Fig. 3 Web application of the infrasound detection system (Kogelnig et al 2013; the table below is restricted due to image size)…”
Section: Single Infrasound Sensor Systemmentioning
confidence: 99%
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“…The event EWS for debris flows usually detects the passage of a debris flow at a certain cross section where the sensor is installed, but they may also be able to detect some tens of seconds in advance the arrival of the debris flow when ground vibration sensors are employed Koschuch et al, 2015;Schimmel and Hübl, 2015). The event EWS that rely on the use of algorithms to process the monitoring data and recognize the occurrence of a debris-flow event, usually require long development and systematic testing.…”
Section: Introductionmentioning
confidence: 99%