Issues

Special Section: Seismoacoustics and Seismoacoustic Data Fusion
Introduction to the Special Section on Seismoacoustics and Seismoacoustic Data Fusion
A New Decade in Seismoacoustics (2010–2022)
Evaluating Spatiotemporal Trends in Infrasound Propagation Using Seismoacoustic Arrivals from Repeating Explosions
Using Local Infrasound to Estimate Seismic Velocity and Earthquake Magnitudes
Seismoacoustic Explosion Yield and Depth Estimation: Insights from the Large Surface Explosion Coupling Experiment
Remote Characterization of the 12 January 2020 Eruption of Taal Volcano, Philippines, Using Seismo‐Acoustic, Volcanic Lightning, and Satellite Observations
Seismoacoustic Signatures Observed During a Long‐Term Deployment of Infrasound Sensors at the Nevada National Security Site
Seismoacoustic Coupled Signals from the 11 July 2020 5.1 Tangshan, China, Earthquake
Hydroacoustic Study of a Seismic Swarm in 2016–2017 near the Melville Transform Fault on the Southwest Indian Ridge
Short‐Range Recordings of Shallow Underwater Explosions with Short‐Period and Broadband Seismometers in the Bay of Hyères, France
Fundamental Investigations of Propagation through the Land–Air–Water Interface in a Controlled Littoral Environment
Characterizing Infrasound Station Frequency Response Using Large Earthquakes and Colocated Seismometers
Numerical Simulations of Seismoacoustic Nuisance Patterns from an Induced M 1.8 Earthquake in the Helsinki, Southern Finland, Metropolitan Area
Infrasound Observations at Bahía de Banderas, Western Mexico
Numerical Modeling of Air‐Blast Suppression as a Function of Explosive‐Charge Burial Depth
Seismoacoustic Analysis of the 7 July 2011 Abadan, Turkmenistan, Explosions
Seismoacoustic Monitoring of a Longwall Face Using Distributed Acoustic Sensing
The Redmond Salt Mine Monitoring Experiment: Observations of Infrasound Resonance
A Multimodal Event Catalog and Waveform Data Set That Supports Explosion Monitoring from Nevada, U.S.A.
Seismoacoustic Analysis of the Large Surface Explosion Coupling Experiment Using a Large‐N Seismic Array
Articles
Geomechanical Modeling of Ground Surface Deformation Associated with Thrust and Reverse‐Fault Earthquakes: A Distinct Element Approach
Fault Damage Zone Effects on Ground Motions during the 2019 7.1 Ridgecrest, California, Earthquake
Source‐Parameter Estimation after Attenuation Correction through the Use of Q Tomography
Noise Reduction from Vertical‐Component Seismograms Recorded by Broadband Ocean‐Bottom Seismometers Deployed at the Western Pacific
Characteristics of Background Noise in the Oldest‐1 Array Deployed on the Oldest Part of the Pacific Plate
Evaluation of Station Timing Errors from Demeaned Arrival Time Delays
Quality Control Metrics for Cepstral Analysis with Homomorphic Deconvolution
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Cover Image
Cover Image
On 12 January 2020, an eruption started on Taal Volcano, one of the most active volcanoes in the Philippines. The activity increased during the day, producing a sustained 16–17 km high plume, intense volcanic lightning, and widespread ashfall. The lightning streaks over the city of Batangas, located at the shores of Main Crater Lake, dramatically illuminating the ashcloud of the eruption. The range of data collected during the eruption allows investigating how the combination of different remote sensing methods may complement local observations and monitoring. The paper by Perttu et al., “Remote Characterization of the 12 January 2020 Eruption of Taal Volcano, Philippines, Using Seismo-Acoustic, Volcanic Lightning, and Satellite Observations,” which is part of the featured Special Section “Seismoacoustics and Seismoacoustic Data Fusion,” presents a post-event analysis of the 12 January activity. The authors combine data from long-range lightning, infrasound, and seismic arrays located up to thousands of kilometers away to identify five phases of activity, including a major shift in eruption behavior around 12:00 (UTC) on 12 January.
Image credit: Domcar C. Lagto/Pacific Press/Shutterstock
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