Closson, Abou Karaki, al-Fugha SPACE BORNE RADAR INTERFEROMETRIC MAPPING OF PRECURSORY DEFORMATIONS OF A DYKE COLLAPSE, DEAD SEA, JORDAN Closson, Abou Karaki, al-Fugha dclosson@mail.com naj@paris.com
1650m The case study : the collapse of the salt evaporation pond 19 Ikonos : 19-10-2000 The case study : the collapse of the salt evaporation pond 19 of the Arab poatsh Company 1650m
The SEP costed 32 M Jordan Dinar It collapsed on March 22, 2000 55 M m3 brine to the Dead Sea in less than one our
After the mid sixties The Dead Sea Decrease from -392m To -418m
June, 30 1993 ERS Radar Images May, 29 1999 Lisan Coastline 1961-1962 1993 1999
SAR-based remote sensing technique
Remote sensing SAR SAR = Synthetic Aperture RADAR (RAdio Detection And Ranging) SAR is a sensor able to generate high resolution images imaging sensor: Allows the observation of the Earth surface in 2D exemple of another sensor : Radar altimetre: provide data in one dimension. Allow generation of topographic maps
SAR remote sensing - properties main characteristics of SAR images: 1. It is an active system (illuminate the area of interest with microwaves) independant of solar illumination allows measurement in day and night conditions 2. use micro-waves to penetrate through cloud cover allows observations in cloud cover areas remark: it alters the accuracy of measurements 3. Its a coherent system by opposition to visible remote sensing wich use the incoherent light of the sun allows the use of interferometry technic Main characteristics of a SAR system 1. Is an active system (it provides its own illumination) Is not dependent on the sunlight Permits continuous day/night operation 2. Uses microwaves, which have reduced impact of cloud, fog and rain Permits all-weather imaging Nota: hay un impacto en la fase del SAR 3. It is a coherent system, which provides both the amplitude and the phase of the radar signal Interferometric techniques can be employed to exploit the information contained in the phase (tema principal del curso)
SAR remote sensing - properties 4. SAR allows the observation of Earth surface properties that are not accessible to visible sensors - rugosity, dielectric properties (through coherence images) - possibilities to penetrate - the vegetation (L band) - ultra dry soil - snow cap 5. The Sar resolution is independant of the distance between the sensor and the objective 6. – Allows the utilisation of different polarization in transmission as well as in reception : HH, HV, VV, VH - Allows the utilization of different frequencies
SAR applications 1. Geometric applications, based on the interferometric phase: - Generation of digital terrain model (DTM) Technic: SAR interferometry (InSAR) - Control the deformations fields over the Earth surface Technic: differential SAR interferometry (DInSAR) 2. Thematic application - Change detection from coherence variation through time (soil erosion, flood)
Deformation fields : principle
DInSAR Topo topographic phase Mov movement Atm atmosphere Noise noise of instruments The differential interferometric phase is a sum of several components
Subidence from 1995-1997