作者: George E Hilley , Roland Burgmann , Alessandro Ferretti , Fabrizio Novali , Fabio Rocca
关键词: Precipitation 、 Geomorphology 、 Displacement (fluid) 、 Meteorology 、 Lead (sea ice) 、 Interferometric synthetic aperture radar 、 Pore water pressure 、 Creep 、 Active fault 、 Geology 、 Landslide 、 Multidisciplinary
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