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Figure 1: Map of Alaska showing stations with colocated broadband seismometers and pressure sensors that recorded signal from the HTHH eruption with high (>= 0.8) coherence between the vertical seismic and infrasound in a  0.015 to 0.035 Hz passband.

Alaska Upper Crustal Velocities Revealed by Air-to-Ground Coupled Waves From the 2022 Hunga Tonga-Hunga Ha’apai Eruption
07/08/2025


Figure 3

Unsupervised Machine Learning Clustering of Seismic and Infrasound Data Quality Metrics
12/19/2023


Figure 1

Back‐Azimuth Estimation of Air‐to‐Ground Coupled Infrasound from Transverse Coherence Minimization
10/02/2023


Fig.1

Using Local Infrasound to Estimate Seismic Velocity and Earthquake Magnitudes
04/27/2023


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Projects By Year

2025

Alaska Upper Crustal Velocities Revealed by Air-to-Ground Coupled Waves From the 2022 Hunga Tonga-Hunga Ha’apai Eruption
07/08/2025

2023

Back‐Azimuth Estimation of Air‐to‐Ground Coupled Infrasound from Transverse Coherence Minimization
10/02/2023

Characterizing Infrasound Station Frequency Response Using Large Earthquakes and Colocated Seismometers
02/22/2023

Unsupervised Machine Learning Clustering of Seismic and Infrasound Data Quality Metrics
12/19/2023

Using Local Infrasound to Estimate Seismic Velocity and Earthquake Magnitudes
04/27/2023

2022

Ambient Infrasound Noise, Station Performance, and Their Relation to Land Cover across Alaska
04/19/2022

Atmospheric waves and global seismoacoustic observations of the January 2022 Hunga eruption, Tonga
05/12/2022

Detecting Large Explosions with Machine Learning Models Trained on Synthetic Infrasound Data
05/24/2022

Waveform Features Strongly Control Subcrater Classification Performance for a Large, Labeled Volcano Infrasound Dataset
07/28/2022

2021

Infrasound Propagation Working Group Report
06/10/2021

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