Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic

Sea ice elevation plays a crucial role in sea ice dynamic processes driven by winds and waves, for which satellite radar remote sensing becomes indispensable to monitor snow-covered sea ice across the vast polar regions regardless of darkness and clouds. To measure sea ice elevation, a theory of pol...

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Main Authors: Nghiem, Son V., Huang, Lanqing, id_orcid:0 000-0002-5180-7491, Hajnsek, Irena, id_orcid:0 000-0002-0926-3283
Format: Article in Journal/Newspaper
Language:English
Published: California Institute of Technology, Jet Propulsion Laboratory 2022
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/585819
https://doi.org/10.3929/ethz-b-000546697
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author Nghiem, Son V.
Huang, Lanqing
id_orcid:0 000-0002-5180-7491
Hajnsek, Irena
id_orcid:0 000-0002-0926-3283
author_facet Nghiem, Son V.
Huang, Lanqing
id_orcid:0 000-0002-5180-7491
Hajnsek, Irena
id_orcid:0 000-0002-0926-3283
author_sort Nghiem, Son V.
collection ETH Zürich Research Collection
description Sea ice elevation plays a crucial role in sea ice dynamic processes driven by winds and waves, for which satellite radar remote sensing becomes indispensable to monitor snow-covered sea ice across the vast polar regions regardless of darkness and clouds. To measure sea ice elevation, a theory of polarimetric interferometry for both monostatic and bistatic radars is developed based on analytic solutions of Maxwell's equations, accounting for realistic and complicated properties of snow, sea ice, and seawater. This analytic method inherently preserves phase information that is imperative for radar polarimetry and interferometry. Among a multitude of complex radar coefficients in the general polarimetric interferometric covariance matrix, the symmetry group theory is utilized to identify and select appropriate terms pertaining to the retrieval of sea ice elevation while avoiding radar parameters that may inadvertently introduce non-uniqueness and excessive uncertainty. Theoretical calculations compare well with field observations for rough and old sea ice encountered in the Operation-IceBridge and TanDEM-X Antarctic Science Campaign over the Western Weddell Sea. The results show that the magnitude of the coefficient of normalized correlation between co-polarized horizontal and co-polarized vertical radar returns is inversely related to sea ice elevation, while the associate phase term is nonlinear and noisy and should be excluded. From these analyses, a protocol is set up to measure Antarctic sea ice elevation to be presented in the next companion paper. ISSN:2333-5084
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Sea ice
Weddell Sea
genre_facet Antarc*
Antarctic
Sea ice
Weddell Sea
geographic Antarctic
Weddell Sea
Weddell
geographic_facet Antarctic
Weddell Sea
Weddell
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/585819
institution Open Polar
language English
op_collection_id ftethz
op_doi https://doi.org/20.500.11850/58581910.3929/ethz-b-000546697
op_relation info:eu-repo/semantics/altIdentifier/wos/000789930500001
http://hdl.handle.net/20.500.11850/585819
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc/4.0/
Creative Commons Attribution-NonCommercial 4.0 International
op_source Earth and Space Science, 9 (5)
publishDate 2022
publisher California Institute of Technology, Jet Propulsion Laboratory
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/585819 2025-03-30T14:56:17+00:00 Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic Nghiem, Son V. Huang, Lanqing id_orcid:0 000-0002-5180-7491 Hajnsek, Irena id_orcid:0 000-0002-0926-3283 2022-05 application/application/pdf https://hdl.handle.net/20.500.11850/585819 https://doi.org/10.3929/ethz-b-000546697 en eng California Institute of Technology, Jet Propulsion Laboratory info:eu-repo/semantics/altIdentifier/wos/000789930500001 http://hdl.handle.net/20.500.11850/585819 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc/4.0/ Creative Commons Attribution-NonCommercial 4.0 International Earth and Space Science, 9 (5) Sea ice elevation radar polarimetric interferometry Maxwell's equations analytic method Weddell Sea Antarctic info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftethz https://doi.org/20.500.11850/58581910.3929/ethz-b-000546697 2025-03-05T22:09:16Z Sea ice elevation plays a crucial role in sea ice dynamic processes driven by winds and waves, for which satellite radar remote sensing becomes indispensable to monitor snow-covered sea ice across the vast polar regions regardless of darkness and clouds. To measure sea ice elevation, a theory of polarimetric interferometry for both monostatic and bistatic radars is developed based on analytic solutions of Maxwell's equations, accounting for realistic and complicated properties of snow, sea ice, and seawater. This analytic method inherently preserves phase information that is imperative for radar polarimetry and interferometry. Among a multitude of complex radar coefficients in the general polarimetric interferometric covariance matrix, the symmetry group theory is utilized to identify and select appropriate terms pertaining to the retrieval of sea ice elevation while avoiding radar parameters that may inadvertently introduce non-uniqueness and excessive uncertainty. Theoretical calculations compare well with field observations for rough and old sea ice encountered in the Operation-IceBridge and TanDEM-X Antarctic Science Campaign over the Western Weddell Sea. The results show that the magnitude of the coefficient of normalized correlation between co-polarized horizontal and co-polarized vertical radar returns is inversely related to sea ice elevation, while the associate phase term is nonlinear and noisy and should be excluded. From these analyses, a protocol is set up to measure Antarctic sea ice elevation to be presented in the next companion paper. ISSN:2333-5084 Article in Journal/Newspaper Antarc* Antarctic Sea ice Weddell Sea ETH Zürich Research Collection Antarctic Weddell Sea Weddell
spellingShingle Sea ice elevation
radar polarimetric interferometry
Maxwell's equations
analytic method
Weddell Sea
Antarctic
Nghiem, Son V.
Huang, Lanqing
id_orcid:0 000-0002-5180-7491
Hajnsek, Irena
id_orcid:0 000-0002-0926-3283
Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic
title Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic
title_full Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic
title_fullStr Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic
title_full_unstemmed Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic
title_short Theory of Radar Polarimetric Interferometry and Its Application to the Retrieval of Sea Ice Elevation in the Western Weddell Sea, Antarctic
title_sort theory of radar polarimetric interferometry and its application to the retrieval of sea ice elevation in the western weddell sea, antarctic
topic Sea ice elevation
radar polarimetric interferometry
Maxwell's equations
analytic method
Weddell Sea
Antarctic
topic_facet Sea ice elevation
radar polarimetric interferometry
Maxwell's equations
analytic method
Weddell Sea
Antarctic
url https://hdl.handle.net/20.500.11850/585819
https://doi.org/10.3929/ethz-b-000546697