Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland

Different approaches have been proposed in recent years to map glacier zones using Synthetic Aperture Radar (SAR). Most of them rely on empirical or statistical approaches for the interpretation of backscatter intensity measurements and their seasonal variations related to the melting regime of the...

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Main Authors: Parrella, Giuseppe, Hajnsek, Irena, Papathanassiou, Konstantinos
Format: Article in Journal/Newspaper
Language:English
Published: IEEE 2021
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/518625
https://doi.org/10.3929/ethz-b-000518625
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author Parrella, Giuseppe
Hajnsek, Irena
Papathanassiou, Konstantinos
author_facet Parrella, Giuseppe
Hajnsek, Irena
Papathanassiou, Konstantinos
author_sort Parrella, Giuseppe
collection ETH Zürich Research Collection
description Different approaches have been proposed in recent years to map glacier zones using Synthetic Aperture Radar (SAR). Most of them rely on empirical or statistical approaches for the interpretation of backscatter intensity measurements and their seasonal variations related to the melting regime of the different glacier zones. This article focuses on the potential of polarimetric SAR measurements to characterize the scattering in the different glacier zones in order to distinguish between them. For this, a general two-component scattering model is proposed, accounting for surface and subsurface contributions in the different glacier zones. The (anisotropic) propagation through snow, firn, and ice layers is also accounted for as it plays an important role in the interpretation of the polarimetric signatures. A set of five polarimetric descriptors is proposed to describe the projection of the model on the SAR measurements. The ability of the model to characterize the scattering in the different glacier zones is validated and discussed at different frequencies (X-, C-, and L-band). For this, a multifrequency airborne SAR dataset acquired by the DLR's F-SAR sensor in West Greenland during the ARCTIC 2015 campaign is used. The achieved results indicate that L-band polarimetric measurements allow to differentiate the different glacier zones based on the subsurface (e.g., volume) scattering characteristics. In contrast, the increased (back-) scattering complexity and the reduced penetration capability limit the potential of X- and C-band polarimetric measurements. ISSN:1939-1404 ISSN:2151-1535
format Article in Journal/Newspaper
genre Arctic
glacier
Greenland
genre_facet Arctic
glacier
Greenland
geographic Arctic
Greenland
Line Glacier
geographic_facet Arctic
Greenland
Line Glacier
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/518625
institution Open Polar
language English
long_lat ENVELOPE(167.833,167.833,-72.983,-72.983)
op_collection_id ftethz
op_doi https://doi.org/20.500.11850/51862510.3929/ethz-b-00051862510.1109/JSTARS.2021.3126069
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1109/JSTARS.2021.3126069
info:eu-repo/semantics/altIdentifier/wos/000722001900007
http://hdl.handle.net/20.500.11850/518625
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_source IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 14
publishDate 2021
publisher IEEE
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/518625 2025-03-30T15:05:06+00:00 Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland Parrella, Giuseppe Hajnsek, Irena Papathanassiou, Konstantinos 2021 application/application/pdf https://hdl.handle.net/20.500.11850/518625 https://doi.org/10.3929/ethz-b-000518625 en eng IEEE info:eu-repo/semantics/altIdentifier/doi/10.1109/JSTARS.2021.3126069 info:eu-repo/semantics/altIdentifier/wos/000722001900007 http://hdl.handle.net/20.500.11850/518625 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 14 Firn line glacier zones Greenland polarimetric synthetic aperture radar (SAR) polarization phase difference info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftethz https://doi.org/20.500.11850/51862510.3929/ethz-b-00051862510.1109/JSTARS.2021.3126069 2025-03-05T22:09:16Z Different approaches have been proposed in recent years to map glacier zones using Synthetic Aperture Radar (SAR). Most of them rely on empirical or statistical approaches for the interpretation of backscatter intensity measurements and their seasonal variations related to the melting regime of the different glacier zones. This article focuses on the potential of polarimetric SAR measurements to characterize the scattering in the different glacier zones in order to distinguish between them. For this, a general two-component scattering model is proposed, accounting for surface and subsurface contributions in the different glacier zones. The (anisotropic) propagation through snow, firn, and ice layers is also accounted for as it plays an important role in the interpretation of the polarimetric signatures. A set of five polarimetric descriptors is proposed to describe the projection of the model on the SAR measurements. The ability of the model to characterize the scattering in the different glacier zones is validated and discussed at different frequencies (X-, C-, and L-band). For this, a multifrequency airborne SAR dataset acquired by the DLR's F-SAR sensor in West Greenland during the ARCTIC 2015 campaign is used. The achieved results indicate that L-band polarimetric measurements allow to differentiate the different glacier zones based on the subsurface (e.g., volume) scattering characteristics. In contrast, the increased (back-) scattering complexity and the reduced penetration capability limit the potential of X- and C-band polarimetric measurements. ISSN:1939-1404 ISSN:2151-1535 Article in Journal/Newspaper Arctic glacier Greenland ETH Zürich Research Collection Arctic Greenland Line Glacier ENVELOPE(167.833,167.833,-72.983,-72.983)
spellingShingle Firn line
glacier zones
Greenland
polarimetric synthetic aperture radar (SAR)
polarization phase difference
Parrella, Giuseppe
Hajnsek, Irena
Papathanassiou, Konstantinos
Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland
title Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland
title_full Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland
title_fullStr Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland
title_full_unstemmed Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland
title_short Model-Based Interpretation of PolSAR Data for the Characterization of Glacier Zones in Greenland
title_sort model-based interpretation of polsar data for the characterization of glacier zones in greenland
topic Firn line
glacier zones
Greenland
polarimetric synthetic aperture radar (SAR)
polarization phase difference
topic_facet Firn line
glacier zones
Greenland
polarimetric synthetic aperture radar (SAR)
polarization phase difference
url https://hdl.handle.net/20.500.11850/518625
https://doi.org/10.3929/ethz-b-000518625