scholarly journals Displacement field and fault model for the September 7, 1999 Athens Earthquake inferred from ERS2 Satellite radar interferometry

2000 ◽  
Vol 27 (24) ◽  
pp. 3989-3992 ◽  
Author(s):  
C. Kontoes ◽  
P. Elias ◽  
O. Sykioti ◽  
P. Briole ◽  
D. Remy ◽  
...  
Keyword(s):  
Displacement Field ◽  
Fault Model ◽  
Radar Interferometry ◽  
Athens Earthquake ◽  
Satellite Radar

scholarly journals A Methodology to Validate the InSAR Derived Displacement Field of the September 7th, 1999 Athens Earthquake Using Terrestrial Surveying. Improvement of the Assessed Deformation Field by Interferometric Stacking

Sensors ◽  
2008 ◽  
Vol 8 (7) ◽  
pp. 4119-4134 ◽  
Author(s):  
Ioannis Kotsis ◽  
Charalabos Kontoes ◽  
Dimitrios Paradissis ◽  
Spyros Karamitsos ◽  
Panagiotis Elias ◽  
...  
Keyword(s):  
Displacement Field ◽  
Deformation Field ◽  
Athens Earthquake

Pre-eruptive ground deformation of Azerbaijan mud volcanoes detected through satellite radar interferometry (DInSAR)

2014 ◽  
Vol 637 ◽  
pp. 163-177 ◽  
Author(s):  
Benedetta Antonielli ◽  
Oriol Monserrat ◽  
Marco Bonini ◽  
Gaia Righini ◽  
Federico Sani ◽  
...  
Keyword(s):  
Ground Deformation ◽  
Radar Interferometry ◽  
Mud Volcanoes ◽  
Satellite Radar

scholarly journals Measurement of ice-sheet topography using satellite-radar interferometry

1996 ◽  
Vol 42 (140) ◽  
pp. 10-22 ◽  
Author(s):  
Ian Joughin ◽  
Dale Winebrenner ◽  
Mark Fahnestock ◽  
Ron Kwok ◽  
William Krabill
Keyword(s):  
Ice Sheets ◽  
Ice Sheet ◽  
Surface Displacement ◽  
Horizontal Resolution ◽  
Radar Interferometry ◽  
Altimeter Data ◽  
Laser Altimeter ◽  
Digital Elevation ◽  
Satellite Radar ◽  
Ice Sheet Topography

AbstractDetailed digital elevation models (DEMs) do not exist for much of the Greenland and Antartic ice sheets. Radar altimetry is at present the primary, in many cases the only, source of topographic data over the ice sheets, but the horizontal resolution of such data is coarse. Satellite-radar interferometry uses the phase difference between pairs of synthetic aperture radar (SAR) images to measure both ice-sheet topography and surface displacement. We have applied this technique using ERS-1 SAR data to make detailed (i.e. 80 m horizontal resolution) maps of surface topography in a 100 km by 300 km strip in West Greenland, extending northward from just above Jakobshavns Isbræ. Comparison with а 76 km long line of airborne laser-altimeter data shows that We have achieved a relative accuracy of 2.5 m along the profile. These observations provide a detailed view of dynamically Supported topography near the margin of an ice sheet. In the final section We compare our estimate of topography with phase contours due to motion, and confirm our earlier analysis concerning vertical ice-sheet motion and complexity in ERS-1 SAR interferograms.

Satellite Radar Interferometry for Monitoring Ice Sheet Motion: Application to an Antarctic Ice Stream

Science ◽  
1993 ◽  
Vol 262 (5139) ◽  
pp. 1525-1530 ◽  
Author(s):  
R. M. Goldstein ◽  
H. Engelhardt ◽  
B. Kamb ◽  
R. M. Frolich
Keyword(s):  
Ice Sheet ◽  
Radar Interferometry ◽  
Ice Stream ◽  
Satellite Radar

Drought-driven transient aquifer compaction imaged using multitemporal satellite radar interferometry

Geology ◽  
2011 ◽  
Vol 39 (6) ◽  
pp. 551-554 ◽  
Author(s):  
Pablo J. González ◽  
José Fernández
Keyword(s):  
Radar Interferometry ◽  
Satellite Radar

The solution of the dynamic field of the Haskell fault model reconsidered

1982 ◽  
Vol 72 (4) ◽  
pp. 1069-1083
Author(s):  
R. D. List
Keyword(s):  
Half Space ◽  
Displacement Field ◽  
Body Force ◽  
Fault Model ◽  
Earthquake Source ◽  
Infinite Space ◽  
Force Method ◽  
Body Force Method ◽  
Rupture Speed ◽  
Seismic Dislocations

abstract A method of obtaining the displacement field of the Haskell model of an earthquake source, based on the well-known equivalence of seismic dislocations and body force, is described. It is shown that the solution of Madariaga (1978) can be generalized and that the two methods are equivalent for the problem of a rectangular dislocation expanding on a plane in an infinite space with a variable rupture speed and variable slip in the direction of rupture. One of the advantages of the equivalent body force method is that it can be used to readily obtain the transformed solution to the Haskell model in a half-space for a rectangular dislocation, expanding with variable rupture speed and variable slip.

The use of satellite radar interferometry to monitor landslides in Slovakia

2020 ◽  
pp. 129-137
Author(s):  
M. Lesko ◽  
J. Papco ◽  
M. Bakon ◽  
R. Czikhardt ◽  
M. Plakinger ◽  
...  
Keyword(s):  
Radar Interferometry ◽  
Satellite Radar

scholarly journals Intertidal DEM Generation Using Satellite Radar Interferometry

2012 ◽  
Vol 28 (1) ◽  
pp. 121-128 ◽  
Author(s):  
Jeong-Won Park ◽  
Jung-Hyun Choi ◽  
Yoon-Kyung Lee ◽  
Joong-Sun Won
Keyword(s):  
Radar Interferometry ◽  
Satellite Radar
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