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Fig. 5 | Earth, Planets and Space

Fig. 5

From: Impact of crustal deformation detection by the DSI (difference of split-band interferograms) method with PALSAR-2 data: a case study on the 2016 Kumamoto Earthquake

Fig. 5

a, b Slant-range change maps of the post-seismic pair of Path 126 obtained using the difference of split-band interferograms (DSI) analysis and conventional Interferometric Synthetic Aperture Radar (InSAR), respectively. c, d Differential interferogram and coherence obtained from conventional InSAR. e Scatter plot showing the differences in slant-range changes obtained using DSI (y-axis) versus coherences (x-axis). f Relationship between the coherence and standard deviation of the differences in the slant-range changes

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