Identification of Landslides in La Reunion Island with JERS-1 and RADARSAT-1 Radar Interferometry

Details Identification of Landslides in La Reunion Island with JERS-1 and RADARSAT-1 Radar Interferometry Identification of Landslides in La Reunion Island with JERS-1 and RADARSAT-1 Radar Interferometry

Jun 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004esasp.550e..66r&link_type=abstract

Proceedings of the FRINGE 2003 Workshop (ESA SP-550). 1-5 December 2003, ESA/ESRIN, Frascati, Italy. Editor: H. Lacoste. Publish

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La Réunion Island is affected by constant slope movement and huge landslides due to the rough topography, a wet climate and favourable geological context. Radar interferometry can provide a mean for identifying landslides on a large scale. Because of the vegetation cover, C-band interferograms are generally hampered. Using JERS-1 images, we show that the L-Band can be used to overcome the loss of coherence observed in the C-band. The technique has been applied to the cases of the Grand Ilet and Hellbourg landslides located in Salazie Circle.

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