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TerraSAR-X
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Image
A TerraSAR‐X satellite‐based radar‐derived graphic showing range offsets (d...
Published: 22 August 2018
Figure 2. A TerraSAR‐X satellite‐based radar‐derived graphic showing range offsets (displacement) in meters, arising from the sixth test overlain on Google Earth. The satellite was on descending passes with a southwest‐oriented line of sight (LoS). The color scale is in meters, in which red
Image
A TerraSAR‐X satellite‐based radar‐derived graphic showing 3D displacement ...
Published: 22 August 2018
Figure 3. A TerraSAR‐X satellite‐based radar‐derived graphic showing 3D displacement from the sixth test, as overlain on Google Earth. It provides information on movements along three azimuths (west–east, south–north, and down‐up). The arrows indicate the direction and magnitude of the horizontal
Image
Mean amplitude of 34 TerraSAR-X images. The landslides investigated in prev...
Published: 13 May 2016
Fig. 2. Mean amplitude of 34 TerraSAR-X images. The landslides investigated in previous studies are indicated by the white rectangles.
Image
TerraSAR-X interferogram [master: 12 Feb. 2011; slave: 23 Feb. 2011, (a) ma...
Published: 01 August 2013
Fig. 4. TerraSAR-X interferogram [master: 12 Feb. 2011; slave: 23 Feb. 2011, (a) magnitude and (b) phase], (c) land use, (d) soil type, (e) and elevation of Noord-Holland, with polders Schermer (S), Beemster (B), Purmer (P) and Wieringermeer (W). The dashed line indicates the extent
Image
TerraSAR-X interferograms over Noord-Holland showing decorrelation effects ...
Published: 01 August 2013
Fig. 6. TerraSAR-X interferograms over Noord-Holland showing decorrelation effects to phase changes. (a) Phase images of an 11 d interferogram (master: 26 June 2010; slave: 7 July 2010). (b) Phase images of a 22 d interferogram (master: 19 Apr. 2011; slave: 11 May 2011). Interferograms show
Series: GSA Special Papers
Publisher: Geological Society of America
Published: 01 October 2015
DOI: 10.1130/2015.2518(12)
... The TanDEM-X digital elevation model (DEM), generated by the TanDEM-X mission, provides a unique opportunity for studying the topography and morphology of terrestrial impact structures. In the TanDEM-X mission, the two Earth-orbiting X-band radar satellites TerraSAR-X and TanDEM-X...
The TanDEM-X digital elevation model (DEM), generated by the TanDEM-X mission, provides a unique opportunity for studying the topography and morphology of terrestrial impact structures. In the TanDEM-X mission, the two Earth-orbiting X-band radar satellites TerraSAR-X and TanDEM-X are operated in close formation to act as a single-pass interferometer. Interferometric processing of the acquired data yields a global DEM with unprecedented accuracy of better than 4 m and a spatial resolution of 12 m. We investigate how the TanDEM-X DEM can be used for mapping terrestrial impact structures by applying it to the confirmed impact craters in the Earth Impact Database of the Planetary and Space Science Centre at the University of New Brunswick, Canada. The majority of these structures show distinct topographic signatures. Particularly prominent are medium-sized eroded craters. We provide representative elevation and X-band amplitude maps for a sample of the Earth Impact Database entries.
Journal Article
Photographic feature: Revealing millimetre-scale ground movements in London using SqueeSAR™
Publisher: Geological Society of London
Published: 16 May 2019
Quarterly Journal of Engineering Geology and Hydrogeology (2019) qjegh2018-075.
... area to demonstrate and validate measurements derived using InSAR; its continuous urban fabric and the regular acquisition of SAR images from high-resolution sensors, such as TerraSAR-X, allows detection and monitoring of over 1.7 million measurement points with millimetre-scale accuracy. The results...
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Journal Article
Evidence for Tear Faulting from New Constraints of the 23 October 2011 M w 7.1 Van, Turkey, Earthquake Based on InSAR, GPS, Coastal Uplift, and Field Observations
Publisher: Seismological Society of America
Published: 03 July 2018
Bulletin of the Seismological Society of America (2018) 108 (4): 1929-1946.
...‐thrust fault comprising one or two subparallel segments and the existence of a shallow slip deficit. Here, by introducing an additional coseismic pixel‐offset dataset from the TerraSAR‐X satellite, we conclude that a NNE–SSW‐trending left‐lateral tear fault that bounds the rupture to the east also...
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Includes: Supplemental Content
Journal Article
Landslide stability evaluation using high-resolution satellite SAR data in the Three Gorges area
Publisher: Geological Society of London
Published: 13 May 2016
Quarterly Journal of Engineering Geology and Hydrogeology (2016) 49 (3): 203-211.
...Fig. 2. Mean amplitude of 34 TerraSAR-X images. The landslides investigated in previous studies are indicated by the white rectangles. ...
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Journal Article
Satellite-Based Radar Interferometry to Estimate Large-Scale Soil Water Depletion from Clay Shrinkage: Possibilities and Limitations
Journal: Vadose Zone Journal
Publisher: Soil Science Society of America
Published: 01 August 2013
Vadose Zone Journal (2013) 12 (3): vzj2012.0098.
...Fig. 4. TerraSAR-X interferogram [master: 12 Feb. 2011; slave: 23 Feb. 2011, (a) magnitude and (b) phase], (c) land use, (d) soil type, (e) and elevation of Noord-Holland, with polders Schermer (S), Beemster (B), Purmer (P) and Wieringermeer (W). The dashed line indicates the extent...
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Image
A: Bathymetry of Nisihinoshima, Japan, before A.D. 2013 eruption. B–D: Terr...
Published: 01 April 2016
Figure 1. A: Bathymetry of Nisihinoshima, Japan, before A.D. 2013 eruption. B–D: TerraSAR-X satellite images of new island, taken on 22 November 2013, 25 December 2013, and 13 April 2014.JST—Japan Standard Time. TerraSAR-X images ©2014 DLR, Distribution Airbus DS/Infoterra GmbH, Sub-Distribution
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(a) Surface rupture at locality D, showing the zone of fracturing as descri...
Published: 01 March 2013
area of the Brawley swarm of August 2012 on TerraSAR‐X (09–31 August 2012) interferogram. Original TerraSAR‐X data copyright 2012 DLR. In the background, the map shows the agricultural fields, major roads, and the New River drainage. Fractures were observed at locations D and K. The green solid line
Image
(a,b) Range and (c,d) azimuth pixel offsets from X‐band, high‐resolution SA...
Published: 03 July 2018
Figure 9. (a,b) Range and (c,d) azimuth pixel offsets from X‐band, high‐resolution SAR scenery of CSK and TerraSAR‐X satellites, calculated on stable point‐like scatterers. The two offshore points to the north (in b,d) are on the Adır Island. White dashed lines represent the profiles shown
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InSAR time series for the maximum uplift rate at Lazufre (locations are col...
Published: 09 August 2017
Figure 3. InSAR time series for the maximum uplift rate at Lazufre (locations are colored points in Fig. 2 ). Note that each time-series inversion was performed separately for each data set (ERS and Envisat Image Swath 2, TerraSAR-X, and RADARSAT-2 satellites), however the similar orbits
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The profiles of the raw ALOS-2 DPM (red) and the Shuttle Radar Topography...
Published: 01 November 2015
and vegetated areas is different, the profile was selected only within urban area identified with the Global Urban Footprint derived from the German Aerospace Center’s (DLR’s) X-band TerraSAR-X SAR data.
Image
Comparison of the predicted LOS changes along profiles of the two‐segment m...
Published: 03 July 2018
Figure 7. Comparison of the predicted LOS changes along profiles of the two‐segment model (Fig. 11a ) with (a) the CSK range offsets and (b) TerraSAR‐X (TSX) range offsets, which were calculated at identified stable point‐like scatterers. Profiles A–A′ and B–B′ are shown in Figure 9 . Red
Image
A: Evolution of Nishinoshima, Japan, from May to October 2014, based on Ter...
Published: 01 April 2016
Figure 3. A: Evolution of Nishinoshima, Japan, from May to October 2014, based on TerraSAR-X satellite images. Lava lobes I, II, and III correspond to periods of peak lava discharge as shown in B. Black arrows indicate flow directions. Dashed lines indicate earlier lobe front. B: Temporal
Image
Surface displacements from optical image correlation and Line‐of‐Sight ( LO...
Published: 25 March 2014
range offset map for satellite TerraSAR‐X (beam 9). (c) LOS range offset map for satellite TerraSAR‐X (beam 11). (d) LOS range offset map for satellite RADARSAT‐2. Continuous black line is the fault surface trace mapped from surface displacements shown on (a). Dark arrows indicate the direction from
Image
Histograms of interferometric phase over Field A and Field B from cascade p...
Published: 01 August 2013
Fig. 7. Histograms of interferometric phase over Field A and Field B from cascade processed TerraSAR-X data from 2011. Acquisition dates were: 17 March, 28 March, 19 April, 11 May, 22 May, and 2 June. Fig. 7a is calculated from the oldest interferogram (master: 17 March; slave: 28 March) and Fig
Image
Limmo dewatering. ( a )–( e ) show the impact as measured by InSAR of the d...
Published: 16 May 2019
Fig. 6. Limmo dewatering. ( a )–( e ) show the impact as measured by InSAR of the dewatering necessary for Crossrail's construction in East London around the Limmo peninsula. The TerraSAR-X data were partitioned into five time periods, defined by the response to dewatering; the cut-off times
