Assessing ScanSAR Interferometry for Deformation Studies

There is a trend in civil satellite SAR mission design to implement an imaging strategy that incorporates both stripmap mode and ScanSAR imaging. This represents a compromise between high resolution data collection and a desire for greater spatial coverage and more frequent revisit times. However, mixed mode imaging can greatly reduce the number of stripmap images available for measuring subtle ground deformation. Although ScanSAR-ScanSAR and ScanSAR-stripmap repeat-pass interferometry have been demonstrated, these approaches are infrequently used for single interferogram formation and nonexistent for InSAR time series analysis. For future mission design, e.g., a dedicated US InSAR mission, the effect of various ScanSAR system parameter choices on InSAR time series analysis also remains unexplored. Our objective is to determine the utility of ScanSAR differential interferometry. We will demonstrate the use of ScanSAR interferograms for several previous deformation studies: localized and broad-scale urban land subsidence, tunneling, volcanic surface movements and several examples associated with the seismic cycle. We also investigate the effect of various ScanSAR burst synchronization levels on our ability to detect and make quality measurements of deformation. To avoid the issues associated with Envisat ScanSAR burst alignment and to exploit a decade of InSAR measurements, we simulate ScanSAR data by bursting (throwing away range lines of) ERS-1/2 data. All the burst mode datasets are processed using a Modified SPECAN algorithm. To investigate the effects of burst misalignment, a number of cases with varying degrees of burst overlap are considered. In particular, we look at phase decorrelation as a function of percentage of burst overlap. Coherence clearly reduces as the percentage of overlap decreases and we find a useful threshold of 40-70% burst overlap depending on the study site. In order to get a more generalized understanding for different surface conditions, we consider several vastly different study sites. Phoenix, Arizona is an urban area which is located in an arid region with very little vegetation. C-band data over Phoenix is generally coherent over 5+ years. ERS data collected through the 1990s is used to monitor land subsidence in and around the Phoenix metropolitan area. We contrast these measurements with both broad and narrow deformation features in the vegetated Houston, Texas and London, U.K. areas. We find that low resolution ScanSAR data can be used to detect narrow features with small spatial extent. Several additional interferograms demonstrate the general applicability of C-band ScanSAR interferometry to WInSAR community interests, e.g., the Hector Mine earthquake, aseismic fault motion and Long Valley and Yellowstone deformation over time. With the September 2006 implementation of a new burst synchronization strategy for Envisat, 90% of all ScanSAR acquisitions exhibit at least 50% burst overlap. Our results demonstrate that these new data can be successfully used for a number of InSAR applications.