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InSAR monitoring of Coastal Landslides.   V. Singhroy, F. Charbonneau, J. Li, G. Pavlic, R. Couture*    Canada Centre for Remote  Sensing   * Geological Survey of Canada   [email_address]
Debris  flows Landslides in Cretaceous Shale Retrogressive earthflows Rockfalls Rotational slumps Landslides in Canada  Coastal Landslides
Objectives ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
InSAR Monitoring Sites in Canada Earthquake sites Landslide sites
Gaspé   Study area – slope failure in 1998 Active zone
Landslide: Field Instruments ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],InSAR Contribution Passive In Situ No In Situ
Deployment of corner reflectors Descending  &  Ascending
PTA-InSAR Aquisition ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Gascons, Qc Péninsule gaspésienne 4mm/y 12mm/y
PTA-InSAR: Results  2D ,[object Object],[object Object],Look Azimuth 0 0 -9 -2 CR8 2 2 CR7 3 14 CR6 9 14 CR5 4 15 CR4 -14 36 * CR3 0 0 CR2 (ref) CR1 (ref) Vertical Azimuth-Horizontal
 
Daniels Harbour, NF- InSAR monitoring of Coastal Landslides 15mm/year
Daniels Harbour, NF: Monitoring Landslide from Radarsat-2 InSAR April 2007 RADARSAT-2 Ultra Fine :  Master: 20090610 Slave: 20090914 Baseline: 67 m x Site A Site B June 2010 -50  0  50 Vertical displacement [mm]
Landslides in Newfoundland- Corner Brook and Daniels Harbour Triggers:  Coastal erosion from high frequency and intensity of storms combined with favourable geological conditions  Corner Brook
Site A Site B Site C 80mm/y RADARSAT 2 INSAR monitoring of Corner Brook Landslides
1) RADARSAT 2 – Ultra Fine  Inc. Angle = 36.81° Ascending Orbit 2) Lidar DEM 1 m  Deformations are only shown where scene coherence exceeds 0.5 x Corner Brook, NF: Monitoring Landslide from Radarsat-2 InSAR -60  0  60 Vertical displacement [mm]
RADARSAT Missions   Committed to provide RADARSAT Data Continuity 1995: RADARSAT-1 2007: RADARSAT-2 2016: 2017:  2017: RCM Repeat Cycle: 24 days 24 days 4 days 3 to 100 metres 0.7 to 100 metres 10 to 100 metres Spatial Resolution
Conclusions ,[object Object],[object Object],[object Object],[object Object]
Thanks

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igarss11-singhroy.ppt

  • 1. InSAR monitoring of Coastal Landslides. V. Singhroy, F. Charbonneau, J. Li, G. Pavlic, R. Couture* Canada Centre for Remote Sensing * Geological Survey of Canada [email_address]
  • 2. Debris flows Landslides in Cretaceous Shale Retrogressive earthflows Rockfalls Rotational slumps Landslides in Canada Coastal Landslides
  • 3.
  • 4. InSAR Monitoring Sites in Canada Earthquake sites Landslide sites
  • 5. Gaspé Study area – slope failure in 1998 Active zone
  • 6.
  • 7. Deployment of corner reflectors Descending & Ascending
  • 8.
  • 9. Gascons, Qc Péninsule gaspésienne 4mm/y 12mm/y
  • 10.
  • 11.  
  • 12. Daniels Harbour, NF- InSAR monitoring of Coastal Landslides 15mm/year
  • 13. Daniels Harbour, NF: Monitoring Landslide from Radarsat-2 InSAR April 2007 RADARSAT-2 Ultra Fine : Master: 20090610 Slave: 20090914 Baseline: 67 m x Site A Site B June 2010 -50 0 50 Vertical displacement [mm]
  • 14. Landslides in Newfoundland- Corner Brook and Daniels Harbour Triggers: Coastal erosion from high frequency and intensity of storms combined with favourable geological conditions Corner Brook
  • 15. Site A Site B Site C 80mm/y RADARSAT 2 INSAR monitoring of Corner Brook Landslides
  • 16. 1) RADARSAT 2 – Ultra Fine Inc. Angle = 36.81° Ascending Orbit 2) Lidar DEM 1 m Deformations are only shown where scene coherence exceeds 0.5 x Corner Brook, NF: Monitoring Landslide from Radarsat-2 InSAR -60 0 60 Vertical displacement [mm]
  • 17. RADARSAT Missions Committed to provide RADARSAT Data Continuity 1995: RADARSAT-1 2007: RADARSAT-2 2016: 2017: 2017: RCM Repeat Cycle: 24 days 24 days 4 days 3 to 100 metres 0.7 to 100 metres 10 to 100 metres Spatial Resolution
  • 18.

Notas do Editor

  1. This is the ASAR title, as submitted for conference abstract