Abstract
Physical and deployment factors that influence infrasound signal detection and assess automatic detection performance for a regional infrasound network of arrays in the Western U.S. are explored using signatures of ground truth (GT) explosions (yields). Despite these repeated known sources, published infrasound event bulletins contain few GT events. Arrays are primarily distributed toward the south-southeast and south-southwest at distances between 84 and 458 km of the source with one array offering azimuthal resolution toward the northeast. Events occurred throughout the spring, summer, and fall of 2012 with the majority occurring during the summer months. Depending upon the array, automatic detection, which utilizes the adaptive F-detector successfully, identifies between 14% and 80% of the GT events, whereas a subsequent analyst review increases successful detection to 24%-90%. Combined background noise quantification, atmospheric propagation analyses, and comparison of spectral amplitudes determine the mechanisms that contribute to missed detections across the network. This analysis provides an estimate of detector performance across the network, as well as a qualitative assessment of conditions that impact infrasound monitoring capabilities. The mechanisms that lead to missed detections at individual arrays contribute to network-level estimates of detection capabilities and provide a basis for deployment decisions for regional infrasound arrays in areas of interest.
Original language | English |
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Pages (from-to) | 3509-3526 |
Number of pages | 18 |
Journal | Journal of the Acoustical Society of America |
Volume | 148 |
Issue number | 6 |
DOIs | |
State | Published - Dec 1 2020 |
Funding
The authors acknowledge the support of the National Nuclear Security Administration Office of Defense Nuclear Nonproliferation Research and Development (R & D) for funding this work. Los Alamos National Laboratory completed this work under the auspices of the U.S. Department of Energy. Instrumentation support came from the Incorporated Research Institutions for Seismology (IRIS) Program for Array Seismic Studies of the Continental Lithosphere (PASSCAL) program, as well as from SMU. The University of Utah in cooperation with SMU installed and operated the arrays, as well as provided information and data. Data were distributed and archived at the IRIS Data Management Center.2 Junghyun Park completed the seismic analysis of the UTTR arrivals at BGU, which enhanced the completeness of the GT event dataset. The authors would like to thank the editor and reviewers of this manuscript, whose detailed comments significantly improved the structure and focus of the paper.
Funders | Funder number |
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National Nuclear Security Administration Office of Defense Nuclear Nonproliferation Research and Development |