Publications
Filter Total Items: 2346
Glacier and permafrost hazards Glacier and permafrost hazards
No abstract available.
Authors
G.J. Wolken, A.K. Liljedahl, M. Brubaker, Jeffrey A. Coe, G. Fiske, H.H. Christiansen, M. Jacquemart, B.M. Jones, A. Kaab, F. Løvholt, S. Natali, A.C.A. Rudy, D. Streletskiy
The impact of 3D finite‐fault information on ground‐motion forecasting for earthquake early warning The impact of 3D finite‐fault information on ground‐motion forecasting for earthquake early warning
We identify aspects of finite‐source parameterization that strongly affect the accuracy of estimated ground motion for earthquake early warning (EEW). EEW systems aim to alert users to impending shaking before it reaches them. The U.S. West Coast EEW system, ShakeAlert, currently uses two algorithms based on seismic data to characterize the earthquake’s location, magnitude, and origin...
Authors
Jessica R. Murray, Eric M. Thompson, Annemarie S. Baltay Sundstrom, Sarah E. Minson
Crustal seismic attenuation of the central United States and Intermountain West Crustal seismic attenuation of the central United States and Intermountain West
Seismic attenuation is generally greater in the western United States (WUS) than the central and eastern United States (CEUS), but the nature of this transition or location of this boundary is poorly constrained. We conduct crustal seismic (Lg) attenuation tomography across a region that stretches from the CEUS across the Rocky Mountains to the Basin and Range using a total of 115,870...
Authors
Will Levandowski, Oliver S. Boyd, Danya AbdelHameid, Daniel McNamara
Multi-model comparison of computed debris flow runout for the 9 January 2018 Montecito, California post-wildfire event Multi-model comparison of computed debris flow runout for the 9 January 2018 Montecito, California post-wildfire event
Hazard assessment for post-wildfire debris flows, which are common in the steep terrain of the western United States, has focused on the susceptibility of upstream basins to generate debris flows. However, reducing public exposure to this hazard also requires an assessment of hazards in downstream areas that might be inundated during debris flow runout. Debris flow runout models are...
Authors
Katherine R. Barnhart, Ryan P. Jones, David L. George, Brian W. McArdell, Francis K. Rengers, Dennis M. Staley, Jason W. Kean
Hazard-consistent seismic losses and collapse capacities for light-frame wood buildings in California and Cascadia Hazard-consistent seismic losses and collapse capacities for light-frame wood buildings in California and Cascadia
We evaluate the seismic performance of modern seismically designed wood light-frame (WLF) buildings, considering regional seismic hazard characteristics that influence ground motion duration and frequency content and, thus, seismic risk. Results show that WLF building response correlates strongly with ground motion spectral shape but weakly with duration. Due to the flatter spectral...
Authors
Robert Edward Chase, Abbie B. Liel, Nico Luco, Zach Bullock
Local variations in broadband sensor installations: Orientations, sensitivities, and noise levels 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)...
Authors
Adam T. Ringler, Robert E. Anthony
An evaluation of the timing accuracy of global and regional seismic stations and networks An evaluation of the timing accuracy of global and regional seismic stations and networks
Clock accuracy is a basic parameter of any seismic station and has become increasingly important for seismology as the community seeks to refine structures and dynamic processes of the Earth. In this study, we measure the arrival time differences of moderate repeating earthquakes with magnitude 5.0–5.9 in the time range of 1991–2017 at the same seismic stations by cross‐correlating their...
Authors
Ying Yang, Xiaodong Song, Adam T. Ringler
Hydrogeomorphic recovery and temporal changes in rainfall thresholds for debris flows following wildfire Hydrogeomorphic recovery and temporal changes in rainfall thresholds for debris flows following wildfire
Wildfire-induced changes to soil and vegetation promote runoff-generated debris flows in steep watersheds. Postfire debris flows are most commonly observed in steep watersheds during the first wet season following a wildfire, but it is unclear how long the elevated threat of debris flow persists and why debris-flow potential changes in recovering burned areas. This work quantifies how...
Authors
Olivia J. Hoch, Luke A. McGuire, Ann M. Youberg, Francis K. Rengers
Comment on “Which earthquake accounts matter” by Susan E. Hough and Stacey S. Martin Comment on “Which earthquake accounts matter” by Susan E. Hough and Stacey S. Martin
In their analysis of the U.S. Geological Survey’s (USGS) “Did You Feel It?” (DYFI) data Hough and Martin (2021) claim, among other assertions, that the following: Socioeconomic and geopolitical factors can introduce biases in the USGS’ characterization of earthquakes and their effects, especially if online data collection systems are not designed to be broadly accessible; These biases...
Authors
David J. Wald
Evaluation of intensity prediction equations (IPEs) for small-magnitude earthquakes Evaluation of intensity prediction equations (IPEs) for small-magnitude earthquakes
This study assesses existing intensity prediction equations (IPEs) for small unspecified magnitude (M ≤3.5) earthquakes at short hypocentral distances (Dh) and explores such earthquakes’ contribution to the felt shaking hazard. In particular, we consider IPEs by Atkinson and Wald (2007) and Atkinson et al. (2014), and evaluate their performance based on “Did You Feel It” (DYFI) reports...
Authors
Ganyu Teng, Jack W. Baker, David J. Wald
Modeling seismic network detection thresholds using production picking algorithms Modeling seismic network detection thresholds using production picking algorithms
Estimating the detection threshold of a seismic network (the minimum magnitude earthquake that can be reliably located) is a critical part of network design and can drive network maintenance efforts. The ability of a station to detect an earthquake is often estimated by assuming the spectral amplitude for an earthquake of a given size, assuming an attenuation relationship, and comparing...
Authors
David C. Wilson, Emily Wolin, William L. Yeck, Robert E. Anthony, Adam T. Ringler
Hazard characterization for alternative intensity measures using the total probability theorem Hazard characterization for alternative intensity measures using the total probability theorem
Since their inception in the 1980s, simplified procedures for the analysis of liquefaction hazards have typically characterized seismic loading using a combination of peak ground acceleration and earthquake magnitude. However, more recent studies suggest that certain evolutionary intensity measures (IMs) such as Arias intensity or cumulative absolute velocity may be more efficient and...
Authors
Michael W. Greenfield, Andrew James Makdisi