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New approach to detect seismic surface waves in 1Hz-sampled GPS time series
N Houlié1, G Occhipinti, T Blanchard
1UC Berkeley, Seismological Laboratory, Berkeley, California, USA. houlie@seismo.berkeley.edu
We present a new method using Global Positioning System (GPS) double-difference (DD) computations to detect 3D co-seismic ground shaking. This technique improves accuracy by minimizing GPS measurement errors, even with varying satellite visibility.
Area of Science:
- Geodesy
- Seismology
- Earthquake Engineering
Background:
- Co-seismic seismic source characterization using Global Positioning System (GPS) measurements has yielded significant results.
- Accuracy in ground displacement measurement from GPS phase residuals is limited by satellite distribution.
- Existing methods struggle with intrinsic GPS measurement errors.
Purpose of the Study:
- To introduce and test a novel method for detecting 3D co-seismic ground shaking.
- To enhance the accuracy of ground displacement measurements during seismic events.
- To overcome limitations posed by satellite geometry in GPS measurements.
Main Methods:
- Utilizing double-difference (DD) computations of Line of Sight (LOS) measurements.
- Employing a quasi-analytical approach to minimize intrinsic GPS errors.
- Benchmarking the method with data from the Hokkaido Earthquake (2003) using GEONET GPS stations.
Main Results:
- The DD method successfully detects 3D co-seismic ground shaking.
- DD amplitudes generated by seismic waves were 4 and 7 times stronger than background noise.
- The method demonstrated robustness despite potential satellite distribution issues.
Conclusions:
- The developed DD method offers a more accurate way to characterize co-seismic ground motion.
- This technique is effective in identifying 3D seismic shaking, improving upon existing GPS-based methods.
- The study validates the DD method's performance using real-world earthquake data.
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