Group A, Poster #081, Tectonic Geodesy
Surface displacements and megathrust slip of the M8.8 2025 Kamchatka earthquake from Sentinel-1 and ALOS-2 InSAR
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Poster Presentation
2025 SCEC Annual Meeting, Poster #081, SCEC Contribution #14921 VIEW PDF
nd descending tracks of Sentinel-1 Interferometric Wideswath (IW) and ALOS-2 Interferometric Widemode (WD1) data. We process all available data using the JPL/Caltech ISCE2 software, using the Copernicus DEM to correct for elevation. Despite the vegetated terrain, which can be challenging for C-band InSAR, we obtain usable coherence in our Sentinel-1 data, and identify line-of-sight displacement of up to ~1 m towards the satellite; our ALOS-2 data have good coherence, but are strongly affected by ionospheric noise. Our plan is to invert the InSAR displacements using the same fault geometry that we use for our studies of interseismic locking. This will allow us to gauge the level of agreement between our locking models and the pattern of coseismic slip on the megathrust implied by the InSAR data, and how well the InSAR data can be fitted by the accumulated slip deficit between the 1952 and 2025 earthquakes predicted by our locking model.
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