Details

Autor(en) / Beteiligte

• Bowden, Daniel C.
• Tsai, Victor C.

Titel

Earthquake ground motion amplification for surface waves

Ist Teil von

• Geophysical research letters, 2017-01, Vol.44 (1), p.121-127

Ort / Verlag

Washington: John Wiley & Sons, Inc

Erscheinungsjahr

2017

Quelle

Wiley-Blackwell Journals

Beschreibungen/Notizen

• Surface waves from earthquakes are known to cause strong damage, especially for larger structures such as skyscrapers and bridges. However, common practice in characterizing seismic hazard at a specific site considers the effect of near‐surface geology on only vertically propagating body waves. Here we show that surface waves have a unique and different frequency‐dependent response to known geologic structure and that this amplification can be analytically calculated in a manner similar to current hazard practices. Applying this framework to amplification in the Los Angeles Basin, we find that peak ground accelerations for certain large regional earthquakes are underpredicted if surface waves are not properly accounted for and that the frequency of strongest ground motion amplification can be significantly different. Including surface‐wave amplification in hazards calculations is therefore essential for accurate predictions of strong ground motion for future San Andreas Fault ruptures. Key Points Site amplification term is different between surface waves and vertically‐incident shear waves Amplification maps for Southern California, based on 1‐D profiles, can be very different Waveforms from the El Mayor Cucapah earthquake support a different site term definition between wave types