Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets

Conventional processing of ice-sounder data produces 2-D images of the ice sheet and bed, where the two dimensions are along-track and depth, while the across-track direction is fixed to nadir. The 2-D images contain information about the topography and radar reflectivity of the ice sheet’s surface,...

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Main Authors: Heister, Anton, Scheiber, Rolf
Format: Conference Object
Language:English
Published: 2017
Subjects:
Online Access:https://elib.dlr.de/111950/
https://elib.dlr.de/111950/1/EGU2017-18952.pdf
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spelling ftdlr:oai:elib.dlr.de:111950 2023-05-15T15:53:44+02:00 Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets Heister, Anton Scheiber, Rolf 2017-01-30 application/pdf https://elib.dlr.de/111950/ https://elib.dlr.de/111950/1/EGU2017-18952.pdf en eng https://elib.dlr.de/111950/1/EGU2017-18952.pdf Heister, Anton und Scheiber, Rolf (2017) Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets. European Geosciences Union (EGU), 2017-04-24 - 2017-04-26, Vienna, Austria. SAR-Technologie Konferenzbeitrag NonPeerReviewed 2017 ftdlr 2019-08-04T22:59:29Z Conventional processing of ice-sounder data produces 2-D images of the ice sheet and bed, where the two dimensions are along-track and depth, while the across-track direction is fixed to nadir. The 2-D images contain information about the topography and radar reflectivity of the ice sheet’s surface, bed, and internal layers in the along-track direction. Having multiple antenna phase centers in the across-track direction enables the production of 3-D images of the ice sheet and bed. Compared to conventional 2-D images, these contain additional information about the surface and bed topography, and orientation of the internal layers over a swath in the across-track direction. We apply a 3-D SAR tomographic ice-sounding method based on sparse signal reconstruction to the data collected by Center for Remote Sensing of Ice Sheets (CReSIS) in 2008 in Greenland using their multichannel coherent radar depth sounder (MCoRDS). The MCoRDS data have 16 effective phase centers which allows us to better understand the performance of the method. Lastly we offer sparsity improvement by including wavelet dictionaries into the reconstruction.The results show improved scene feature resolvability in across-track direction compared to MVDR beamformer. Conference Object Center for Remote Sensing of Ice Sheets (CReSIS) Greenland Ice Sheet German Aerospace Center: elib - DLR electronic library Greenland
institution Open Polar
collection German Aerospace Center: elib - DLR electronic library
op_collection_id ftdlr
language English
topic SAR-Technologie
spellingShingle SAR-Technologie
Heister, Anton
Scheiber, Rolf
Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets
topic_facet SAR-Technologie
description Conventional processing of ice-sounder data produces 2-D images of the ice sheet and bed, where the two dimensions are along-track and depth, while the across-track direction is fixed to nadir. The 2-D images contain information about the topography and radar reflectivity of the ice sheet’s surface, bed, and internal layers in the along-track direction. Having multiple antenna phase centers in the across-track direction enables the production of 3-D images of the ice sheet and bed. Compared to conventional 2-D images, these contain additional information about the surface and bed topography, and orientation of the internal layers over a swath in the across-track direction. We apply a 3-D SAR tomographic ice-sounding method based on sparse signal reconstruction to the data collected by Center for Remote Sensing of Ice Sheets (CReSIS) in 2008 in Greenland using their multichannel coherent radar depth sounder (MCoRDS). The MCoRDS data have 16 effective phase centers which allows us to better understand the performance of the method. Lastly we offer sparsity improvement by including wavelet dictionaries into the reconstruction.The results show improved scene feature resolvability in across-track direction compared to MVDR beamformer.
format Conference Object
author Heister, Anton
Scheiber, Rolf
author_facet Heister, Anton
Scheiber, Rolf
author_sort Heister, Anton
title Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets
title_short Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets
title_full Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets
title_fullStr Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets
title_full_unstemmed Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets
title_sort demonstration of sparse signal reconstruction for radar imaging of ice sheets
publishDate 2017
url https://elib.dlr.de/111950/
https://elib.dlr.de/111950/1/EGU2017-18952.pdf
geographic Greenland
geographic_facet Greenland
genre Center for Remote Sensing of Ice Sheets (CReSIS)
Greenland
Ice Sheet
genre_facet Center for Remote Sensing of Ice Sheets (CReSIS)
Greenland
Ice Sheet
op_relation https://elib.dlr.de/111950/1/EGU2017-18952.pdf
Heister, Anton und Scheiber, Rolf (2017) Demonstration of Sparse Signal Reconstruction for Radar Imaging of Ice Sheets. European Geosciences Union (EGU), 2017-04-24 - 2017-04-26, Vienna, Austria.
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