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...
Published in: | IEEE Transactions on Geoscience and Remote Sensing |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
IEEE - Institute of Electrical and Electronics Engineers
2021
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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 |
record_format | openpolar |
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/ |