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Validation of radiometric models  and simulated KaRIn/SWOT  data based on ground and  airborne acquisitions ,[object Object],[object Object],[object Object],[object Object],IGARSS 2011, Vancouver, Canada, 25-29 July 2011
Outline ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Introduction ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Specificities of KaRIn interferometric SAR w.r.t. existing spaceborne earth observation SAR systems ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Simulation of SLC images (L1) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],SAR images  Coherence  Interferogram DEM Land cover classes EM models Orbit  file Layover/ shadow mask e.g. detection of water surfaces, height estimation, … a r
Δ T  = t 0  – t -1  = t +1  – t o  = 1 / PRF -> V t -1 t o t +1 RCS t-1 RCS to RCS t+1 Stacking of all raw images indexed by time Focusing Final RAW data level 1 data Simulation of raw images (L0) e.g. study impact of moving water
BUSARD/DRIVE airborne acquisitions (1/2) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
BUSARD/DRIVE airborne acquisitions (2/2) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Espiguette  (buoy) Acquisition sites in the Camargue area (2011) Piemanson Vaccarès Rhône
voie a Amplitude ~700 m 0° 13° ~2,6 km ~1°  0° ~4°  ~10°  Trihedrals  Artifacts due to wide  antenna lobe (right/ left contamination) DRIVE/BUSARD acquisition 24/02/2011 (Rhône)
DRIVE/BUSARD acquisition 24/02/2011 (Rhône) Phase
DRIVE/BUSARD acquisition 24/02/2011 (Rhône) Coherence >0.9 ~0.7 ~0.3
DRIVE/BUSARD acquisition 14/04/2011 (Vaccarès) Amplitude
DRIVE/BUSARD acquisition 14/04/2011 (Vaccarès) Amplitude 1 Amplitude 2 Coherence Phase
DRIVE/BUSARD acquisition 14/04/2011 (Espiguette) Amplitude
DRIVE/BUSARD acquisition 14/04/2011 (Espiguette) Amplitude 1 Amplitude 2 Coherence Phase
DRIVE/BUSARD acquisition 25/05/2011 (Rhône) Amplitude
Near-field measurements in Ka-band (1/2) ,[object Object],[object Object],[object Object]
Near-field measurements in Ka-band (2/2) ,[object Object],[object Object],[object Object],[object Object]
Water   0  as a function of wind speed Incidence (°/100)  0  (dB) Wind parallel to incidence direction Wind perpendicular to incidence direction  0  (dB) Incidence (°/100)
Conclusion ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
SWOT-related presentations in other sessions ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

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Notas del editor

  1. Page de titre, mentionner contributions Altamira et Cap
  2. Spécificités par rapport aux systèmes SAR spatiaux actuels : Bande Ka: impact prévisible de la courte longueur d’onde d’un point de qualitatif (comme listé ici), mais peu de rapport quantitatifs sur sigma_0 Proche nadir : layover, contraste terre/eau, variation fort/rapide de plusieur paramètres qui d’habitude sont quasiment constants ou varient lentement Faire référence à l’article EUSAR où ces aspects sont détaillés (me contacter pour avoir une copie de l’article, il y a eu un problème technique côté organisateur qui fait qu’il n’est pas sur le CD-ROM proc. EUSAR)