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Adam Ringler, Ph.D.

I am a scientist at the Albuquerque Seismological Laboratory.  I like to work on problems related to instrumentation and data quality.  If you have any queries please don't hesitate to contact me.

Publications

Ringler, A. T., R. E. Anthony, R. C. Aster, C. J. Ammon, S. Arrowsmith, H. Benz, C. Ebeling, W. -Y. Kim, H. C. P. Lau, V. Lekić, P. G. Richards, D. P. Schaff, M. Vallée, and W. Yeck (2021).  Achievements and prospects of global broadband seismic networks after 30 years of continuous geophysical observations, in review.

Ringler, A. T., R. E. Anthony, P. Davis, K. Hafner, R. Mellors, S. Schneider, and D. C. Wilson (2021).  Improved resolution across the Global Seismographic Network: A new era in low-frequency seismology, in review.

Anthony, R. E., A. T. Ringler, and D. C. Wilson (2021).  Seismic background noise levels across the Continental United States from USArray Transportable Array: The influence of geology and geopgraphy, in review.

Yang, Y., X. Song, and A. T. Ringler (2021).  An evaluation of the timing accuracy of global and regional seismic stations and networks, Seis. Res. Lett., in press.

Wilson, D. C., E. Wolin, W. Yeck, R. E. Anthony, and A. T. Ringler (2021).  Modeling seismic network detection thresholds using production picking algorithms, Seis. Res. Lett., in press.

Ringler, A. T. and R. E. Anthony (2021).  Local variations in broadband sensor installations: Orientations, sensitivities, and noise levels, Pure Appl. Geophys., in press.

Zürn, W., T. Forbriger, R. Widmer-Schnidrig, P. Duffner, and A. T. Ringler (2021).  Modeling tilt noise caused by atmospheric processes at long periods for several horizontal seismometers at BFO - A reprise, Geophys. J. Int., DOI: 10.1093/gji/ggab336 [Link]

Ringler, A. T., D. B. Mason, G. Laske, T. Storm, and M. Templeton (2021).  Why do my squiggles look funny? A gallery of compromised seismic signals, Seis. Res. Lett., DOI: 10.1785/0220210094 [Link]

Ringler, A. T., R. E. Anthony, C. A. Dalton, and D. C. Wilson (2021).  Rayleigh-wave amplitude uncertainty across the Global Seismographic Network and potential implications for global tomography, Bull. Seis. Soc. Amer., 111 (3), 1273-1292. [Link]

Ringler, A. T., R. E. Anthony, D. C. Wilson, D. Auerbach, S. Bargabus, P. Davis, M. Gunnels, K. Hafner, J. F. Holland, A. Kearns, and E. Klimczak (2021).  A review of timing accuracy across the Global Seismographic Network, Seis. Res. Lett., 92 (4), 2270-2281 [Link]

Anthony, R. E., A. T. Ringler, M. DuVernois, K. R. Anderson, and D. C. Wilson (2021).  Six decades of seismology at South Pole, Antarctica: Current limitiations and future opportunities to facilitate new geophysical observations, Seis. Res. Lett., 92 (5), 2718-2735. [Link]

Tape, C., A. T. Ringler, and D. L. Hampton (2020).  Recording the Aurora at seismometers across Alaska, Seis. Res. Lett., 91 (6), 3039-3053. [Link]

Alejandro, A. C. B., A. T. Ringler, D. C. Wilson, R. E. Anthony, and S. V. Moore (2020).  Towards understanding relationships between atmo

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Auroras and Earthquakes: Strange Companions

Release Date: JULY 6, 2020 In 1722 and 1723 a London clockmaker, George Graham, observed daily and consistent variations on one of his instruments, a “Needle upon the Pin” (a compass), for which he had no explanation. Swedish scientists obtained some of Graham’s instruments to record what is now known to be the variations in Earth’s magnetic field. In 1741, they noticed a significant deflection of...
By
Natural Hazards Mission Area, Earthquake Hazards Program, Geomagnetism Program
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Auroras and Earthquakes: Strange Companions

Release Date: JULY 6, 2020 In 1722 and 1723 a London clockmaker, George Graham, observed daily and consistent variations on one of his instruments, a “Needle upon the Pin” (a compass), for which he had no explanation. Swedish scientists obtained some of Graham’s instruments to record what is now known to be the variations in Earth’s magnetic field. In 1741, they noticed a significant deflection of...
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Filter Total Items: 65

Comment on “A new decade in seismoacoustics (2010–2022)” by Fransiska Dannemann Dugick, Clinton Koch, Elizabeth Berg, Stephen Arrowsmith, and Sarah Albert

An increase in seismic stations also having microbarographs has led to increased interest in the field of seismoacoustics. A review of the recent advances in this field can be found in Dannemann Dugick et al. (2023). The goal of this note is to draw the attention of the readers of Dannemann Dugick et al. (2023) to several additional interactions between the solid Earth and atmosphere that have not
Authors
Adam T. Ringler, Robert E. Anthony, Brian Shiro, Toshiro Tanimoto, David C. Wilson
By
Volcano Hazards Program, Volcano Science Center

Comparison of co-recorded analog and digital systems for characterization of responses and uncertainties

One of the most prominent challenges related to legacy seismic data is determining how these data can be appropriately used in modern research applications. The wide variety of instrumentation used in the analog era, the format of recording on paper wrapped around a helicorder drum, and limited metadata information introduces ambiguities that are not typical of modern digital data. Therefore, tech
Authors
Thomas A. Lee, Adam T. Ringler, Robert E. Anthony, Miaki Ishii
By
Natural Hazards Mission Area, Geologic Hazards Science Center

Introduction to the digitization of seismic data: A user’s guide

Modern seismic data are collected, distributed, and analyzed using digital formats, and this has become a standard for the field. Although most modern seismometers still make use of analog electronic circuits, their data are converted from an analog voltage output to time‐tagged counts by way of digitization. Although much of the digitization process is not complicated to conceptualize, there is a
Authors
Adam T. Ringler, Robert E. Anthony, Patrick Bastien, Adam Pascale, Bion J. Merchant
By
Natural Hazards Mission Area, Earthquake Hazards Program, Geologic Hazards Science Center

Earth’s upper crust seismically excited by infrasound from the 2022 Hunga Tonga–Hunga Ha’apai eruption, Tonga

Records of pressure variations on seismographs were historically considered unwanted noise; however, increased deployments of collocated seismic and acoustic instrumentation have driven recent efforts to use this effect induced by both wind and anthropogenic explosions to invert for near‐surface Earth structure. These studies have been limited to shallow structure because the pressure signals have
Authors
Robert E. Anthony, Adam T. Ringler, Toshiro Tanimoto, Robin Matoza, Silvio De Angelis, David C. Wilson
By
Natural Hazards Mission Area, Geologic Hazards Science Center

The global seismographic network reveals atmospherically coupled normal modes excited by the 2022 Hunga Tonga eruption

The eruption of the submarine Hunga Tonga-Hunga Haʻapai (Hunga Tonga) volcano on 15 January 2022, was one of the largest volcanic explosions recorded by modern geophysical instrumentation. The eruption was notable for the broad range of atmospheric wave phenomena it generated and for their unusual coupling with the oceans and solid Earth. The event was recorded worldwide across the Global Seismogr
Authors
Adam T. Ringler, Robert E. Anthony, Rick Aster, T. Taira, Brian Shiro, David C. Wilson, S. H. De Angelis, C. Ebeling, Matthew M. Haney, R. Matoza, H. Ortiz
By
Natural Hazards Mission Area, Volcano Hazards Program, Geologic Hazards Science Center, Volcano Science Center

Achievements and prospects of global broadband seismographic networks after 30 years of continuous geophysical observations

Global seismographic networks (GSNs) emerged during the late nineteenth and early twentieth centuries, facilitated by seminal international developments in theory, technology, instrumentation, and data exchange. The mid- to late-twentieth century saw the creation of the World-Wide Standardized Seismographic Network (1961) and International Deployment of Accelerometers (1976), which advanced global
Authors
Adam T. Ringler, Robert E. Anthony, R. C. Aster, C. J. Ammon, S. Arrowsmith, Harley M. Benz, C. Ebeling, A. Frassetto, W. Y. Kim, Paula Koelemeijer, H. C. P. Lau, V. Lekic, J. P. Montagner, P. G. Richards, D. P. Schaff, M. Vallee, William L. Yeck
By
Natural Hazards Mission Area, Geologic Hazards Science Center

Characteristics, relationships and precision of direct acoustic-to-seismic coupling measurements from local explosions

Acoustic energy originating from explosions, sonic booms, bolides and thunderclaps have been recorded on seismometers since the 1950s. Direct pressure loading from the passing acoustic wave has been modelled and consistently observed to produce ground deformations of the near surface that have retrograde elliptical particle motions. In the past decade, increased deployments of colocated seismomete
Authors
Robert E. Anthony, Josh Watzak, Adam T. Ringler, David C. Wilson
By
Natural Hazards Mission Area, Geologic Hazards Science Center

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

The 15 January 2022 climactic eruption of Hunga volcano, Tonga, produced an explosion in the atmosphere of a size that has not been documented in the modern geophysical record. The event generated a broad range of atmospheric waves observed globally by various ground-based and spaceborne instrumentation networks. Most prominent was the surface-guided Lamb wave (≲0.01 hertz), which we observed prop
Authors
Robin S. Matoza, David Fee, Jelle D. Assink, Alexandra M. Iezzi, David N. Green, Keehoon Kim, Liam Toney, Thomas Lecocq, Siddharth Krishnamoorthy, Jean-Marie Lalande, Kiwamu Nishida, Kent L. Gee, Matthew M. Haney, Hugo D. Ortiz, Quentin Brissaud, Léo Martire, Lucie Rolland, Panagiotis Vergados, Alexandra Nippress, Junghyun Park, Shahar Shani-Kadmiel, Alex Witsil, Stephen Arrowsmith, Corentin Caudron, Shingo Watada, Anna Perttu, Benoit Taisne, Pierrick Mialle, Alexis Le Pichon, Julien Vergoz, Patrick Hupe, Philip S. Blom, Roger M. Waxler, Silvio De Angelis, Jonathan Snively, Adam T. Ringler, Robert E. Anthony, Arthur Din Jolly, Geoff Kilgour, Gil Averbuch, Maurizio Ripepe, Mie Ichihara, Alejandra Arciniega-Ceballos, Elvira Astafyeva, Lars Ceranna, Sandrine Cevuard, Il-Young Che, Rodrigo de Negri Leiva, Carl W. Ebeling, Läslo G. Evers, Luis E. Franco-Marin, Tom Gabrielson, Katrin Hafner, R. Giles Harrison, Attila Komjathy, Giorgio Lacanna, John J. Lyons, Kenneth A. Macpherson, Emanuele Marchetti, Kathleen McKee, Rob Mellors, Gerardo Mendo-Pérez, T. Dylan Mikesell, Edhah Munaibari, Mayra Oyola-Merced, Iseul Park, Christoph Pilger, Cristina Ramos, Mario Ruiz, Roberto Sabatini, Hans Schwaiger, Dorianne Tailpied, Carrick Talmadge, Jérôme Vidot, Jeremy Webster, David C. Wilson
By
Natural Hazards Mission Area, Volcano Hazards Program, Geologic Hazards Science Center, Volcano Science Center

Classifying Worldwide Standardized Seismograph Network records using a simple convolution neural network

The U.S. Geological Survey (USGS) maintains an archive of 189,180 digitized scans of analog seismic records from the World‐Wide Standardized Seismograph Network (WWSSN). Although these scans have been made public, the archive is too large to manually review, and few researchers have utilized large numbers of these records. To facilitate further research using this historical dataset, we develop a
Authors
Nagle Nagle-McNaughton, Adam T. Ringler, Robert E. Anthony, Alexis Casondra Bianca Alejandro, David C. Wilson, Justin Thomas Wilgus
By
Natural Hazards Mission Area, Geologic Hazards Science Center

Improved resolution across the Global Seismographic Network: A new era in low-frequency seismology

The Global Seismographic Network (GSN)—a global network of ≈150 very broadband stations—is used by researchers to study the free oscillations of the Earth (≈0.3–10 mHz) following large earthquakes. Normal‐mode observations can provide information about the radial density and anisotropic velocity structure of the Earth (including near the core–mantle boundary), but only when signal‐to‐noise ratios
Authors
Adam T. Ringler, Robert E. Anthony, P. Thompson Davis, Carl Ebeling, K. Hafner, R. Mellors, S. Schneider, David C. Wilson
By
Natural Hazards Mission Area, Earthquake Hazards Program, Geologic Hazards Science Center

Seismic background noise levels across the continental United States from USArray Transportable Array: The influence of geology and geography

Since 2004, the most complete estimate of background noise levels across the continental U.S. was attained using 61 broadband seismic stations to calculate power spectral density (PSD) probability density functions. To improve seismic noise estimates across the U.S., we examine vertical component seismic data from the EarthScope USArray Transportable Array seismic network that rolled across the U.
Authors
Robert E. Anthony, Adam T. Ringler, David C. Wilson
By
Natural Hazards Mission Area, Geologic Hazards Science Center

Local variations in broadband sensor installations: Orientations, sensitivities, and noise levels

As seismologists continue to place more stringent demands on data quality, accurately described metadata are becoming increasingly important. In order to better constrain the orientation and sensitivities of seismometers deployed in U.S. Geological Survey networks, the Albuquerque Seismological Laboratory (ASL) has recently begun identifying true north with a fiber optic gyroscope (FOG) and has de
Authors
Adam T. Ringler, Robert E. Anthony
By
Natural Hazards Mission Area, Earthquake Hazards Program, Geologic Hazards Science Center

ASL Sensor Test Suite

This program is used to analyze various aspects of seismic sensor data in order to determine information about their configuration, such as gain and orientation.

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