Landslide depth inversion method using InSAR elevating track deformation data
A lifting rail and deformation technology, applied in the direction of re-radiation, radio wave reflection/re-radiation, and measuring devices, can solve problems such as inability to accurately reflect the depth distribution of landslides, improve reliability and applicability, and improve The effect of accuracy
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[0050] Example 1:
[0051] like figure 1 As shown in a slide rail InSAR depth deformation data inversion method using the lift, comprising the steps of:
[0052] Sl, using the timing technique InSAR landslide lifting rail radar image area is processed to obtain time series data of deformation of the slide region;
[0053] S2, timing deformation data, the spatial region geometric relationship landslides and DEM data, solving a two-dimensional deformation data and the landslide slope along the surface normal direction;
[0054] S3, constructed in the mass conservation criteria based on two-dimensional depth of the landslide model inversion deformation, and calculates the depth of the landslide deformation data models of the 2D inversion, to obtain the depth of the landslide inversion calculation.
[0055] The present embodiment considers the small Baseline Interferometry (SBAS-InSAR) technology can be better overcome the conventional temporal decorrelation DInSAR faced problems and ...
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[0090] Example 2:
[0091] In this embodiment landslide depth inversion by the above method as in Example 1 to ancient landslide area Tsubosato peach, peach Xiang Li County, Sichuan ancient landslide located Tsubosato peach, north western Sichuan genus mountains and high mountain region, located mountain monsoon climate zone, the area elevation height difference between, complex terrain. Affected by climate in the region each year 7 - October more rainfall in winter is relatively little precipitation, annual rainfall of between 650mm ~ 1000mm. Peach Tsubosato overall presentation slide chair shape ancient, low-lying southwest NE high, narrow width on the slope, the average slope of about 27 ° ~ 53 °, landslide bound to slow steep slope is approximately the leading edge height of 1480m, the edge elevation of about 2710m, relative height of ~ 1230m, 2700m longitudinal length, lateral width ~ 2000m, is a large landslide.
[0092] In this embodiment the collection region Sentinel-1 sa...
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