Surface Displacement Measurement from Remote Sensing Images. Olivier Cavalie

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Surface Displacement Measurement from Remote Sensing Images - Olivier Cavalie


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Dcycle (days) Ntot Altitude (km) ERS-1, ERS-2 routine 22:30 14 11 35 501 785 ERS-1 phases A, B, D 22:30 14 1 3 43 775 Envisat 22:30 14 11 35 501 785 Envisat end of life 22:30 14 11 30 431 783 Radarsat-1,2 18:00 14 7 24 343 798 JERS-1 22:30 14 43 44 659 568 ALOS 22:30 14 27 46 671 692 TerraSAR-X, TanDEM-X, PAZ 18:00 15 2 11 167 515 CSK, CSG 6:00 14 13 16 237 620 Sentinel-1A/B 18:00 14 7 12 175 693 Radarsat CM 18:00 14 11 12 179 593 ALOS-2 18:00 14 3 14 199 628
Satellite Local hour Ascending/descending Period of orbit (min) Dcycle (days) Altitude (km)
Cartosat-2A/2B 9:32 D 97.4 5 635
Landsat 8 10:00 D 98.8 28 705
SPOT-7 10:30 D 98.8 26 694
Sentinel-2A/2B 10:30 D 100.6 10 786
Kompsat-3A 10:50 A 95.2 28 528
Co3D 11:00 - 94.6 - 502
WorldView-1 13:30 D 94.6 14 496
Eros B 14:00 D 94.8 4 520

      Common parameters for optical missions: For the optical missions, the same orbital parameters are key elements for the mission. The orbits are in general sun-synchronous. The local hour has a direct impact on the viewed scenes. There is a compromise between viewing a scene early in the morning in order to reduce atmospheric effects (water vapor) and near midday in order to reduce the length of shadows in the images. The local hour is in general chosen between 9:30 and 14:00.

      Non-sun-synchronous missions: The famous Shuttle Radar Topography Mission (SRTM) was phased, but not sun-synchronous. With an inclination of 57° at 233 km altitude, this mission produced a worldwide digital elevation model (DEM), but it was limited in latitude.

      This section addresses some parameters specific to SAR systems. Some important parameters, such as the range and azimuth ambiguity ratios, are not listed because they do not really affect phase or ground motion measurements.


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