Subduction ground motions in northern South America are about a factor of 2 smaller than the ground motions for similar events in other regions. Nevertheless, historical and recent large-interface and intermediate-depth slab earthquakes of moment magnitudes Mw = 7.8 (Ecuador, 2016) and 7.2 (Colombia, 2012) evidenced the vast potential damage that vulnerable populations close to earthquake epicenters could experience. This article proposes a new empirical ground-motion prediction model for subduction events in northern South America, a regionalization of the global AG2020 ground-motion prediction equations. An updated ground-motion database curated by the Colombian Geological Survey is employed. It comprises recordings from earthquakes associated with the subduction of the Nazca plate gathered by the National Strong Motion Network in Colombia and by the Institute of Geophysics at Escuela Politécnica Nacional in Ecuador. The regional terms of our model are estimated with 539 records from 60 subduction events in Colombia and Ecuador with epicenters in the range of −0.6° to 7.6°N and 75.5° to 79.6°W, with Mw≥4.5, hypocentral depth range of 4 ≤ Zhypo ≤ 210 km, for distances up to 350 km. The model includes forearc and backarc terms to account for larger attenuation at backarc sites for slab events and site categorization based on natural period. The proposed model corrects the median AG2020 global model to better account for the larger attenuation of local ground motions and includes a partially non-ergodic variance model.
Ground-motion model for subduction earthquakes in northern South America Available to Purchase
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
Carlos A Arteta, Department of Civil and Environmental Engineering, Universidad del Norte, Km 5 Vía Puerto Colombia, Área Metropolitana de Barranquilla, 081007, Colombia. Email: [email protected]
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
1Department of Civil and Environmental Engineering, Universidad del Norte, Barranquilla, Colombia
2Colombian Geological Survey (SGC), Bogota, Colombia
3Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, CA, USA
Carlos A Arteta, Department of Civil and Environmental Engineering, Universidad del Norte, Km 5 Vía Puerto Colombia, Área Metropolitana de Barranquilla, 081007, Colombia. Email: [email protected]
- Funder(s):asociación porkcolombia
- Award Id(s): SCOA#03-2020-SGC-UNINORTE
- Award Id(s):
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CitationCarlos A Arteta, Cesar A Pajaro, Vicente Mercado, Julián Montejo, Mónica Arcila, Norman A Abrahamson; Ground-motion model for subduction earthquakes in northern South America. Earthquake Spectra 2021;; 37 (4): 2419–2452. doi: https://doi.org/10.1177/87552930211027585
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- acceleration
- accelerograms
- attenuation
- back-arc basins
- basins
- body waves
- Colombia
- data bases
- data processing
- deep-focus earthquakes
- depth
- earthquakes
- Ecuador
- elastic waves
- epicenters
- faults
- focus
- fore-arc basins
- geologic hazards
- ground motion
- intermediate-focus earthquakes
- intraplate processes
- magnitude
- models
- natural hazards
- Nazca Plate
- networks
- normal faults
- peak ground acceleration
- plate tectonics
- prediction
- regression analysis
- rupture
- S-waves
- seismic waves
- seismograms
- slabs
- soils
- South America
- South American Plate
- spectra
- spectral analysis
- statistical analysis
- strike-slip faults
- subduction
- velocity
- Ecuador earthquake 2016
- Muisne earthquake 2016
- Guaitarilla earthquake 2013
- Calima earthquake 1995
- La Vega earthquake 2012
- Genova earthquake 1997