Fig. 11From: Surface deformation of Asama volcano, Japan, detected by time series InSAR combining persistent and distributed scatterers, 2014‒2018Comparisons of displacement time series between InSAR measurements (red squares) and GNSS measurements (gray circles) at the KAHG GNSS site. The GNSS 3D displacement components are, respectively, projected into the LOS directions of a ascending Sentinel-1 (path 39), and b the descending ALOS-2 (path 19) for comparisons. Error bars indicate the estimated uncertainties of InSAR measurements similar to these in Fig. 9Back to article page