GNGTS 2017 - 36° Convegno Nazionale

96 GNGTS 2017 S essione 1.1 The geometrical combination of sets of images from both ascending and descending SAR orbits has allowed constraining the ground motion orientations, and identifying a change in the orientation of vertical-component ground motion. In particular, orientation of vertical- component ground deformation in the 2005/05/01 to 2008/09/01 time span (hereinafter Fig. 2 - NW-SE oriented topographic profile and relative vertical ground displacement, from IDW raster interpolation, in the 2005/05 - 2009/05 time span. Fig. 3 - NW-SE oriented opographic profile and relative vertical ground displacement, from IDW raster interpolation, in the 2005/05 - 2009/05 time span.