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Monitoring ground deformation of eruption center by ground based interferometric synthetic aperture radar (GB InSAR): a case study during the 2015 phreatic eruption of Hakone volcano

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Academic year: 2020

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Figure

Fig. 1 Location and monitoring direction of the GB-InSAR. a Locations of new craters, new fumaroles, and steam wells that blew out in Owakudani area, b the GB-InSAR equipment installed in Owakudani, and c photograph showing the area scanned by the GB-InSAR
Fig. 2 Plane and cross-sectional views of radar coordinates and resolutions of the GB-InSAR with respect to a slope
Fig. 3 Cumulative relative displacement for the period from 10:20 a.m. of June 25 to 9:26 a.m
Fig. 5 Close view of the time variations of the relative displacements of two areas (area 2 and area 3) and estimated onset of rapid deformation

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