Constraints on surface deformation in the Seattle, WA, urban corridor from satellite radar interferometry time-series analysis

Details Constraints on surface deformation in the Seattle, WA, urban corridor from satellite radar interferometry time-series analysis Constraints on surface deformation in the Seattle, WA, urban corridor from satellite radar interferometry time-series analysis

Jul 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008geoji.174...29f&link_type=abstract

Geophysical Journal International, Volume 174, Issue 1, pp. 29-41.

Astronomy and Astrophysics

Astronomy

2

Time Series Analysis, Radar Interferometry, Hydrology, Intra-Plate Processes, Continental Tectonics: Compressional, North America

Scientific paper

We apply differential InSAR (DInSAR) time-series techniques to the urban corridor between Tacoma, Seattle and Everett, WA, using 93 interferograms from three satellites (ERS 1, ERS 2 and RADARSAT-1) between 1992 and 2007. Our goal is to study local tectonic, geomorphic and groundwater processes. Consequently, we remove long-wavelength (>50-100 km) deformation signals from unwrapped interferograms. By comparing surface velocities generated via the time-series technique at more than two million points within the overlapping region between two independent ERS tracks, we estimate the uncertainty of relative surface velocity measurements to be ~0.5 mm yr-1 in the vertical. We estimate the uncertainty of relative displacement measurements to be ~5.4 mm, given our comparisons of DInSAR-derived time-series to GPS data, a result that is consistent both with previous DInSAR time-series analysis and with the uncertainty expected from GPS displacements projected onto the radar line-of-sight. Active tectonic deformation at shallow depths on the region's numerous east-west structures is absent over the ~11.5 yr of SAR data examined. Assuming that the south-dipping thrust beneath Seattle and Tacoma takes up 3 mm yr-1 of north-south shortening, our data indicate that the fault must be currently locked to a depth of greater than 10 km. We also document extensive groundwater-related deformation throughout much of the study region. Most notably, we identify sharp, linear deformation gradients near Federal Way, WA, and running between Sumner, WA, and Steilacoom, WA. These features may mark the locations of previously unmapped fault splays that locally control groundwater movement. We find no slow landslide deformation on any of the numerous mapped slide complexes within Seattle, although regions of known active landsliding, such as along Perkins Lane in Seattle, exhibit radar phase de-correlation. These observations are consistent with relatively infrequent and rapid landslide deformation within Seattle.

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