Glacier motion estimation using SAR offset-tracking procedures

By T. Strozzi, A. Luckman, T. Murray, U. Wegmüller, C. Werner. IEEE Transactions on Geoscience and Remote Sensing, 2002

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Persistent Scatterer Interferometry: A review (2016, background): “Its main limitation is the low sensitivity to deformation, which is a fraction of the SAR pixel footprint (e.g. 1/10th or 1/20th of the pixel, see Fialko et al. (2001) and Strozzi et al. (2002)) and depends on the local SAR amplitude contrast.”
Glacier-surge mechanisms promoted by a hydro-thermodynamic feedback to summer melt (2015, methodology): “Displacement fields were derived by using cross-correlation between two consecutive acquisitions (Strozzi et al., 2002) and geocoded using a DEM of Austfonna (Moholdt and Kääb, 2012).”
Ocean regulation hypothesis for glacier dynamics in southeast Greenland and implications for ice sheet mass changes (2010, methodology): “[10] We derived flow speeds of ninemajor tidewater outlets from the SE Greenland Ice Sheet (Figure 1) using cross‐ correlation feature tracking [Scambos et al., 1992; Strozzi et al., 2002] on pairs of ASTER, Landsat‐7, and ENVISAT‐ ASAR images, and repeated lidar swaths.”