Estimating Strain and Rotation From Wrapped SAR Interferograms
This letter aims to discuss a general framework that allows the direct interpretation of the wrapped differential synthetic aperture radar interferometry phase in terms of surface strain <inline-formula> <tex-math notation="LaTeX">S </tex-math></inline-formula> and...
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Published in: | IEEE geoscience and remote sensing letters Vol. 15; no. 9; pp. 1367 - 1371 |
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Format: | Journal Article |
Language: | English |
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01-09-2018
The Institute of Electrical and Electronics Engineers, Inc. (IEEE) |
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Abstract | This letter aims to discuss a general framework that allows the direct interpretation of the wrapped differential synthetic aperture radar interferometry phase in terms of surface strain <inline-formula> <tex-math notation="LaTeX">S </tex-math></inline-formula> and rotation <inline-formula> <tex-math notation="LaTeX">R </tex-math></inline-formula> components. The methodology is demonstrated showing the estimation of strain and rotation components of a glacier flow using three TerraSAR-X interferometric geometries (ascending right-looking, descending right-looking, and descending left-looking). Finally, since the left-looking geometry can be difficult to obtain on a regular basis, the surface parallel flow assumption is extended to the phase gradients inversion in order to reduce the amount of necessary geometries from three to two. |
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AbstractList | This letter aims to discuss a general framework that allows the direct interpretation of the wrapped differential synthetic aperture radar interferometry phase in terms of surface strain S and rotation R components. The methodology is demonstrated showing the estimation of strain and rotation components of a glacier flow using three TerraSAR-X interferometric geometries (ascending right-looking, descending right-looking, and descending left-looking). Finally, since the left-looking geometry can be difficult to obtain on a regular basis, the surface parallel flow assumption is extended to the phase gradients inversion in order to reduce the amount of necessary geometries from three to two. This letter aims to discuss a general framework that allows the direct interpretation of the wrapped differential synthetic aperture radar interferometry phase in terms of surface strain <inline-formula> <tex-math notation="LaTeX">S </tex-math></inline-formula> and rotation <inline-formula> <tex-math notation="LaTeX">R </tex-math></inline-formula> components. The methodology is demonstrated showing the estimation of strain and rotation components of a glacier flow using three TerraSAR-X interferometric geometries (ascending right-looking, descending right-looking, and descending left-looking). Finally, since the left-looking geometry can be difficult to obtain on a regular basis, the surface parallel flow assumption is extended to the phase gradients inversion in order to reduce the amount of necessary geometries from three to two. |
Author | Abdel Jaber, Wael Parizzi, Alessandro |
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References | ref13 ref12 ref15 ref14 parizzi (ref5) 0 ref20 ref11 ref10 ref21 ref2 ref1 ref17 ref16 sharov (ref3) 2003 ref19 ref18 van der veen (ref9) 2013 ref8 ref7 ref4 ref6 |
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SubjectTerms | Components Differential synthetic aperture radar interferometry (DInSAR) Estimation Frameworks Frequency estimation Geometry Glacier flow Glaciers glaciers flow gradient tensor Interferometry Parallel flow Radar Rotation SAR (radar) Strain Synthetic aperture radar Synthetic aperture radar interferometry Tensile stress |
Title | Estimating Strain and Rotation From Wrapped SAR Interferograms |
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