NGA-Subduction research program

Bozorgnia, Yousef; Abrahamson, Norman A.; Ahdi, Sean K.; Ancheta, Timothy D.; Al Atik, Linda; Archuleta, Ralph J.; Atkinson, Gail M.; Boore, David M.; Campbell, Kenneth W.; Chiou, Brian S-J; Contreras, Victor; Darragh, Robert B.; Derakhshan, Sahar; Donahue, Jennifer L.; Gregor, Nick; et. al.

Abstract

This article summarizes the Next Generation Attenuation (NGA) Subduction (NGA-Sub) project, a major research program to develop a database and ground motion models (GMMs) for subduction regions. A comprehensive database of subduction earthquakes recorded worldwide was developed. The database includes a total of 214,020 individual records from 1,880 subduction events, which is by far the largest database of all the NGA programs. As part of the NGA-Sub program, four GMMs were developed. Three of them are global subduction GMMs with adjustment factors for up to seven worldwide regions: Alaska, Cascadia, Central America and Mexico, Japan, New Zealand, South America, and Taiwan. The fourth GMM is a new Japan-specific model. The GMMs provide median predictions, and the associated aleatory variability, of RotD50 horizontal components of peak ground acceleration, peak ground velocity, and 5%-damped pseudo-spectral acceleration (PSA) at oscillator periods ranging from 0.01 to 10 s. Three GMMs also quantified "within-model" epistemic uncertainty of the median prediction, which is important in regions with sparse ground motion data, such as Cascadia. In addition, a damping scaling model was developed to scale the predicted 5%-damped PSA of horizontal components to other damping ratios ranging from 0.5% to 30%. The NGA-Sub flatfile, which was used for the development of the NGA-Sub GMMs, and the NGA-Sub GMMs coded on various software platforms, have been posted for public use.

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Título según WOS: ID WOS:000796019300001 Not found in local WOS DB
Título de la Revista: EARTHQUAKE SPECTRA
Volumen: 38
Número: 2
Editorial: SAGE PUBLICATIONS INC
Fecha de publicación: 2022
Página de inicio: 783
Página final: 798
DOI:

10.1177/87552930211056081

Notas: ISI