Monitoring volcanic eruptions with a wireless sensor network

This paper describes our experiences using a wireless sensor network to monitor volcanic eruptions with low-frequency acoustic sensors. We developed a wireless sensor array and deployed it in July 2004 at Volcan Tingurahua, an active volcano in central Ecuador. The network collected infrasonic (low-frequency acoustic) signals at 102 Hz, transmitting data over a 9 km wireless link to a remote base station. During the deployment, we collected over 54 hours of continuous data which included at least 9 large explosions. Nodes were time-synchronized using a separate GPS receiver, and our data was later correlated with that acquired at a nearby wired sensor array. In addition to continuous sampling, we have developed a distributed event detector that automatically triggers data transmission when a well-correlated signal is received by multiple nodes. We evaluate this approach in terms of reduced energy and bandwidth usage, as well as accuracy of infrasonic signal detection.

[1]  Jonathan M. Lees,et al.  Interpretation and utility of infrasonic records from erupting volcanoes , 2003 .

[2]  Jurgen Neuberg,et al.  Highlights from a seismic broadband array on Stromboli Volcano , 1994 .

[3]  Hitoshi Yamasato,et al.  Quantitative Analysis of Pyroclastic Flows Using Infrasonic and Seismic Data at Unzen Volcano, Japan , 1997 .

[4]  Gyula Simon,et al.  The flooding time synchronization protocol , 2004, SenSys '04.

[5]  Richard C. Aster,et al.  Volcanic eruptions observed with infrasound , 2004 .

[6]  Richard C. Aster,et al.  Real-time data received from Mount Erebus Volcano, Antarctica , 2004 .

[7]  Jonathan M. Lees,et al.  P wave crustal velocity structure in the greater Mount Rainier area from local earthquake tomography , 1999 .

[8]  John C. Lahr,et al.  Three‐dimensional P and S wave velocity structure of Redoubt Volcano, Alaska , 1996 .

[9]  David E. Culler,et al.  Lessons from a Sensor Network Expedition , 2004, EWSN.

[10]  Stephen R. McNutt,et al.  Seismic Monitoring and Eruption Forecasting of Volcanoes: A Review of the State-of-the-Art and Case Histories , 1996 .

[11]  Stephen R. McNutt Seismic Monitoring of Volcanoes: A Review of the State-of-the-Art and Recent Trends , 1996 .

[12]  Michael Fehler,et al.  Traveltime tomography: A comparison of popular methods , 1991 .

[13]  Ryan Newton,et al.  Region streams: functional macroprogramming for sensor networks , 2004, DMSN '04.

[14]  John Anderson,et al.  Wireless sensor networks for habitat monitoring , 2002, WSNA '02.

[15]  P. Mothes,et al.  Tungurahua Volcano, Ecuador: structure, eruptive history and hazards , 1999 .

[16]  Maurizio Ripepe,et al.  Array tracking of infrasonic sources at Stromboli volcano , 2002 .

[17]  Milton Garces,et al.  Traveltimes for infrasonic waves propagating in a stratified atmosphere , 1998 .

[18]  F. Giudicepietro,et al.  Source mechanisms of explosions at Stromboli Volcano, Italy, determined from moment‐tensor inversions of very‐long‐period data , 2003 .

[19]  J. Elson,et al.  Fine-grained network time synchronization using reference broadcasts , 2002, OSDI '02.

[20]  Keiiti Aki,et al.  Data summary for dense GEOS array observations of seismic activity associated with magma transport at Kilauea Volcano, Hawaii , 1989 .

[21]  Jonathan M. Lees,et al.  Tomographic inversion for three‐dimensional velocity structure at Mount St. Helens using earthquake data , 1989 .

[22]  R. Scarpa,et al.  Correction to “Source mechanisms of explosions at Stromboli Volcano, Italy, determined from moment-tensor inversions of very-long-period data” , 2003 .

[23]  Roberto Scarpa,et al.  Monitoring and Mitigation of Volcano Hazards , 1996 .

[24]  David E. Culler,et al.  System architecture directions for networked sensors , 2000, SIGP.