Proceedings of the 12th International Conference on Information Processing in Sensor Networks 2013
DOI: 10.1145/2461381.2461396
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Volcanic earthquake timing using wireless sensor networks

Abstract: Recent years have witnessed pilot deployments of inexpensive wireless sensor networks (WSNs) for active volcano monitoring. This paper studies the problem of picking arrival times of primary waves (i.e., P-phases) received by seismic sensors, one of the most critical tasks in volcano monitoring. Two fundamental challenges must be addressed. First, it is virtually impossible to download the real-time high-frequency seismic data to a central station for P-phase picking due to limited wireless network bandwidth. … Show more

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Cited by 53 publications
(43 citation statements)
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“…So to obtain high resolution and real time imaging we need large number of sensor stations which has the capability of performing in-network computing and also avoid costly data collection. The authors in Liu et al (2013) have discussed the use of low-cost sensor for P-phase detection of earthquake. The earthquake hypo-centre detection forms the basic step for seismic tomography and we extend this further to obtain innetwork imaging.…”
Section: Introductionmentioning
confidence: 99%
“…So to obtain high resolution and real time imaging we need large number of sensor stations which has the capability of performing in-network computing and also avoid costly data collection. The authors in Liu et al (2013) have discussed the use of low-cost sensor for P-phase detection of earthquake. The earthquake hypo-centre detection forms the basic step for seismic tomography and we extend this further to obtain innetwork imaging.…”
Section: Introductionmentioning
confidence: 99%
“…It provides aftermath of earthquakes on buildings very precisely. Sensor nodes deployed in different parts of a building which provides the effects of earthquake strength to the building [3].…”
Section: Introductionmentioning
confidence: 99%
“…For instance, in volcano monitoring system, a seismic vibration sensor (geophone) sample in a range of 16-24 bit at 50-200 Hz generating a high volume of raw data [28]. Preprocessing steps such as detecting an earthquake, finding its origin time and location can be performed in-situ [20]. Using these pre-processing steps, discretization of raw data leads us to the formation of a partial least squares problem at each node [26].…”
Section: Introductionmentioning
confidence: 99%