Dynamics of Slow-Moving Landslides from Permanent Scatterer Analysis

作者: George E Hilley , Roland Burgmann , Alessandro Ferretti , Fabrizio Novali , Fabio Rocca

DOI: 10.1126/SCIENCE.1098821

关键词: PrecipitationGeomorphologyDisplacement (fluid)MeteorologyLead (sea ice)Interferometric synthetic aperture radarPore water pressureCreepActive faultGeologyLandslideMultidisciplinary

摘要: High-resolution interferometric synthetic aperture radar (InSAR) permanent scatterer data allow us to resolve the rates and variations in of slow-moving landslides. Satellite-to-ground distances (range changes) on landslides increase at 5 7 millimeters per year, indicating average downslope sliding velocities from 27 38 year. Time-series analysis shows that displacement occurs mainly during high-precipitation season; 1997-1998 El Nino event, range change increased as much 11 The observed nonlinear relationship creep precipitation suggests pore fluid pressures within shallow subsurface may initiate accelerate these features. Changes slope a hill resulting increases pressure lithostatic stress gradients then lead

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