Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition

Reflectometry measurements have been conducted aboard the German research icebreaker Polarstern during the MOSAiC expedition (Multidisciplinary drifting Observatory for the Study of Arctic Climate). Signals of Global Navigation Satellite Systems (GNSS) were recorded using a dedicated GNSS reflectome...

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Published in:IEEE Transactions on Geoscience and Remote Sensing
Main Authors: Semmling, Maximilian, Wickert, Jens, Kreß, Frederik, Hoque, Mohammed Mainul, Divine, Dmitry, Gerland, Sebastian, Spreen, Gunnar
Format: Article in Journal/Newspaper
Language:English
Published: IEEE - Institute of Electrical and Electronics Engineers 2021
Subjects:
Online Access:https://elib.dlr.de/145664/
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author Semmling, Maximilian
Wickert, Jens
Kreß, Frederik
Hoque, Mohammed Mainul
Divine, Dmitry
Gerland, Sebastian
Spreen, Gunnar
author_facet Semmling, Maximilian
Wickert, Jens
Kreß, Frederik
Hoque, Mohammed Mainul
Divine, Dmitry
Gerland, Sebastian
Spreen, Gunnar
author_sort Semmling, Maximilian
collection Unknown
container_start_page 1
container_title IEEE Transactions on Geoscience and Remote Sensing
description Reflectometry measurements have been conducted aboard the German research icebreaker Polarstern during the MOSAiC expedition (Multidisciplinary drifting Observatory for the Study of Arctic Climate). Signals of Global Navigation Satellite Systems (GNSS) were recorded using a dedicated GNSS reflectometry receiver for retrieval of sea-ice reflectivity. The primary goal is a reflectometry-based monitoring of sea ice as part of the Arctic climate study. The data set presented here covers the expedition's first leg (late Sep. to mid Dec. 2019) in the Siberian Sector of the central Arctic (at about 82°N to 87°N). Daily profiles of reflectivity are retrieved for satellite elevations < 45°. In agreement with model prediction the results show best reflectivity contrast (about 5 dB between compact pack-ice and lower ice concentrations) for observations at left-handed circular polarization and elevation angles of 10° to 20°. A daily resolved time series of sea-ice relative permittivity is inverted from the left-handed data. In general, the level of inversion results is at the lower limit of sea-ice values (rel. permittivity of 3 and below), potentially indicating an influence of incoherent volume scattering. Occasional increase of relative permittivity is attributed to the presence of water. Sea-ice profiles show anomalies that are confirmed by enhanced model prediction (slab reflection). A long-term comparison of prediction and retrieved profiles indicates anomalies' dependence on ice thickness and temperature.
format Article in Journal/Newspaper
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
geographic Arctic
geographic_facet Arctic
id ftdlr:oai:elib.dlr.de:145664
institution Open Polar
language English
op_collection_id ftdlr
op_container_end_page 1
op_doi https://doi.org/10.1109/TGRS.2021.3121993
op_relation https://elib.dlr.de/145664/1/Sea-ice_permittivity_derived_from_GNSS_reflection_profiles_Results_of_the_MOSAiC_expedition.pdf
Semmling, Maximilian und Wickert, Jens und Kreß, Frederik und Hoque, Mohammed Mainul und Divine, Dmitry und Gerland, Sebastian und Spreen, Gunnar (2021) Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition. IEEE Transactions on Geoscience and Remote Sensing. IEEE - Institute of Electrical and Electronics Engineers. doi:10.1109/TGRS.2021.3121993 <https://doi.org/10.1109/TGRS.2021.3121993>. ISSN 0196-2892.
publishDate 2021
publisher IEEE - Institute of Electrical and Electronics Engineers
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spelling ftdlr:oai:elib.dlr.de:145664 2025-06-15T14:20:22+00:00 Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition Semmling, Maximilian Wickert, Jens Kreß, Frederik Hoque, Mohammed Mainul Divine, Dmitry Gerland, Sebastian Spreen, Gunnar 2021-12-14 application/pdf https://elib.dlr.de/145664/ en eng IEEE - Institute of Electrical and Electronics Engineers https://elib.dlr.de/145664/1/Sea-ice_permittivity_derived_from_GNSS_reflection_profiles_Results_of_the_MOSAiC_expedition.pdf Semmling, Maximilian und Wickert, Jens und Kreß, Frederik und Hoque, Mohammed Mainul und Divine, Dmitry und Gerland, Sebastian und Spreen, Gunnar (2021) Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition. IEEE Transactions on Geoscience and Remote Sensing. IEEE - Institute of Electrical and Electronics Engineers. doi:10.1109/TGRS.2021.3121993 <https://doi.org/10.1109/TGRS.2021.3121993>. ISSN 0196-2892. Institut für Solar-Terrestrische Physik Zeitschriftenbeitrag PeerReviewed 2021 ftdlr https://doi.org/10.1109/TGRS.2021.3121993 2025-06-04T04:58:07Z Reflectometry measurements have been conducted aboard the German research icebreaker Polarstern during the MOSAiC expedition (Multidisciplinary drifting Observatory for the Study of Arctic Climate). Signals of Global Navigation Satellite Systems (GNSS) were recorded using a dedicated GNSS reflectometry receiver for retrieval of sea-ice reflectivity. The primary goal is a reflectometry-based monitoring of sea ice as part of the Arctic climate study. The data set presented here covers the expedition's first leg (late Sep. to mid Dec. 2019) in the Siberian Sector of the central Arctic (at about 82°N to 87°N). Daily profiles of reflectivity are retrieved for satellite elevations < 45°. In agreement with model prediction the results show best reflectivity contrast (about 5 dB between compact pack-ice and lower ice concentrations) for observations at left-handed circular polarization and elevation angles of 10° to 20°. A daily resolved time series of sea-ice relative permittivity is inverted from the left-handed data. In general, the level of inversion results is at the lower limit of sea-ice values (rel. permittivity of 3 and below), potentially indicating an influence of incoherent volume scattering. Occasional increase of relative permittivity is attributed to the presence of water. Sea-ice profiles show anomalies that are confirmed by enhanced model prediction (slab reflection). A long-term comparison of prediction and retrieved profiles indicates anomalies' dependence on ice thickness and temperature. Article in Journal/Newspaper Arctic Sea ice Unknown Arctic IEEE Transactions on Geoscience and Remote Sensing 1 1
spellingShingle Institut für Solar-Terrestrische Physik
Semmling, Maximilian
Wickert, Jens
Kreß, Frederik
Hoque, Mohammed Mainul
Divine, Dmitry
Gerland, Sebastian
Spreen, Gunnar
Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition
title Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition
title_full Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition
title_fullStr Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition
title_full_unstemmed Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition
title_short Sea-ice permittivity derived from GNSS reflection profiles: Results of the MOSAiC expedition
title_sort sea-ice permittivity derived from gnss reflection profiles: results of the mosaic expedition
topic Institut für Solar-Terrestrische Physik
topic_facet Institut für Solar-Terrestrische Physik
url https://elib.dlr.de/145664/