Fig. 5From: Surface deformation and source modeling of Ayaz-Akhtarma mud volcano, Azerbaijan, as detected by ALOS/ALOS-2 InSARCumulative observed LOS changes derived from a ALOS/PALSAR data (P1-23), b ALOS-2/PALSAR-2 ascending data (P24–32), and c ALOS-2/PALSAR-2 descending data (P33–35). d Calculated ALOS-2/PALSAR-2 descending data, based on the slip distribution model in Fig. 12Back to article page