Journal
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
Volume 108, Issue B11, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2002JB001848
Keywords
radar interferometry; subsidence; synthetic aperture radar; extensometer; Houston; SAR
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We present results from a radar interferometry study over the Houston-Galveston, Texas Gulf Coast region. From the nearly 60 potential interferograms considered, an atmospheric artifact assessment is performed and a tractable set of interferograms selected for detailed processing and error analysis. The subsequent interferogram time series spanning 1996 - 1998 is constrained by coincident extensometer data with root-mean-square error less than 2.5 mm. The interferogram time series confirms that historic subsidence in east Houston has stopped. Consistent with current groundwater use patterns, broad-scale subsidence bowls are observed in west and northwest Houston, where maximum subsidence rates are in excess of 2 and 4 cm yr(-1), respectively. Linear interferogram phase signatures associated with approximately 1 cm of differential subsidence across faults, including the Long Point fault in northwest Houston, are observed. Near the Seabrook extensometer, a hereto-unidentified subsidence bowl with a maximum subsidence rate in excess of 3 cm yr(-1) is revealed. This study demonstrates that when used in conjunction with a set of traditional geodetic measurements, radar interferometry can measure the spatial and temporal evolution of urban land subsidence within even the most challenging of environments.
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