2012 IEEE International Geoscience and Remote Sensing Symposium 2012
DOI: 10.1109/igarss.2012.6350574
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Analyzing the topographic influence for the PS-INSAR processing in the Three Gorges region

Abstract: Persistent Scatterer Interferometry (PS-InSAR) is applied to derive displacement information with millimetric precision. Analyzing stable persistent scatterers from a large stack of SAR images,helps to overcome the geometrical and temporal decorrelation, which occur when using differential interferometry. The removal of the topographic phase with an external DEM seems to cause problems. In our experiment, we select three different DEMs: ASTER GDEM, a DEM derived from a digitized topographic map, and SRTM-3 in … Show more

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Cited by 3 publications
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“…The white squares in Figure 3 show the deformation area of this landslide that appears in interferograms of ALOS PALSAR and ENVISAT ASAR datasets with small normal baselines (156 m, 47 m and 97 m), respectively. However, D-InSAR in the Three Gorges region does not only suffer from the strong temporal decorrelation, but also from the lack of good external DEMs, which causes several fringes in the differential interferogram which could be misinterpreted as surface motions [22]. (Figure 4(c)) show two fast deformation zones (circled areas) located along the southern riverbank of the Yangtze River.…”
Section: Analysis Of Interferogramsmentioning
confidence: 99%
“…The white squares in Figure 3 show the deformation area of this landslide that appears in interferograms of ALOS PALSAR and ENVISAT ASAR datasets with small normal baselines (156 m, 47 m and 97 m), respectively. However, D-InSAR in the Three Gorges region does not only suffer from the strong temporal decorrelation, but also from the lack of good external DEMs, which causes several fringes in the differential interferogram which could be misinterpreted as surface motions [22]. (Figure 4(c)) show two fast deformation zones (circled areas) located along the southern riverbank of the Yangtze River.…”
Section: Analysis Of Interferogramsmentioning
confidence: 99%
“…The original (wrapped or unwrapped) phase is mostly derived from differential interferograms after removing topographic phase with external DEM. Therefore, the quality of differential interferometric phase (referred to as "original phase" hereafter) is directly affected by the external DEM, such as the phase unwrapping error caused by incorrect external DEM in mountainous areas [17,18], the aliasing of deformation signal, and topographic residues [19][20][21]. Meanwhile, it also affects the deformation …”
Section: Introductionmentioning
confidence: 99%