The use of differential synthetic aperture radar interferometry (DIFSAR) to analyze the long term effects in volcanic areas was discussed. DIFSAR evaluated the surface deformations by removing from the interferogram, the topographic contribution, computed from an available Digital Elevation Map of the scene under investigation. The ground surface displacements were measured along the line of sight of the radar source. The DIFSAR experiments show that the existence of a long term deformation effect was an actively growing anticline.

Long term effects in volcanic areas observed by differential SAR interferometry

Berardino P;Fornaro G;Lanari R;Sansosti E;
2000

Abstract

The use of differential synthetic aperture radar interferometry (DIFSAR) to analyze the long term effects in volcanic areas was discussed. DIFSAR evaluated the surface deformations by removing from the interferogram, the topographic contribution, computed from an available Digital Elevation Map of the scene under investigation. The ground surface displacements were measured along the line of sight of the radar source. The DIFSAR experiments show that the existence of a long term deformation effect was an actively growing anticline.
2000
Data recording
Data reduction
Deformation
Error analysis
Global positioning system
Hazards
Interferometry
Landslides
Radar antennas
Remote sensing
Satellites
Seismology
Sensors
Surface topography
Synthetic aperture radar
Vectors
Atmospheric effects
Radar sources
Volcanic peripheries
Volcanoes
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/214729
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