C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars
Snow cover on sea ice poses a challenge for radar measurements as microwave penetration into snow is not yet fully understood. In this study, the aim is to investigate microwave penetration into snow on Arctic sea ice using commercial C (6 GHz) and K (26 GHz) band tank radars. Nadir-looking radar me...
Published in: | Annals of Glaciology |
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Online Access: | https://doi.org/10.1017/aog.2023.47 https://doaj.org/article/94f0590f42894c2ca7f3ca0bef9478cf |
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ftdoajarticles:oai:doaj.org/article:94f0590f42894c2ca7f3ca0bef9478cf 2023-07-30T03:56:17+02:00 C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars Arttu Jutila Christian Haas https://doi.org/10.1017/aog.2023.47 https://doaj.org/article/94f0590f42894c2ca7f3ca0bef9478cf EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305523000472/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2023.47 0260-3055 1727-5644 https://doaj.org/article/94f0590f42894c2ca7f3ca0bef9478cf Annals of Glaciology, Pp 1-11 sea ice snow remote sensing Meteorology. Climatology QC851-999 article ftdoajarticles https://doi.org/10.1017/aog.2023.47 2023-07-09T00:34:30Z Snow cover on sea ice poses a challenge for radar measurements as microwave penetration into snow is not yet fully understood. In this study, the aim is to investigate microwave penetration into snow on Arctic sea ice using commercial C (6 GHz) and K (26 GHz) band tank radars. Nadir-looking radar measurements collected at nine study locations over first-year and multiyear landfast sea ice in the Lincoln Sea in May 2018 are analysed together with detailed measurements of the physical properties of the snow cover to determine the dominant scattering horizons at both frequencies. They are evaluated for the feasibility to determine snow depth. The results show that in 39% of the measurements and only on first-year ice a major fraction of the C band radar backscatter originated closer to the snow–ice interface potentially enabling snow depth retrieval. At K band, 81% of the radar returns originated from the snow surface. Partly confirming the findings of previous studies, however, the analysis was potentially hampered by relatively warm air temperatures (up to $-0.9^\circ$C) during the study period as well as stratigraphic features and inconclusive microwave interaction with the saline basal layers found in the snow cover on first-year ice. Article in Journal/Newspaper Annals of Glaciology Arctic Lincoln Sea Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Annals of Glaciology 1 11 |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
sea ice snow remote sensing Meteorology. Climatology QC851-999 |
spellingShingle |
sea ice snow remote sensing Meteorology. Climatology QC851-999 Arttu Jutila Christian Haas C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars |
topic_facet |
sea ice snow remote sensing Meteorology. Climatology QC851-999 |
description |
Snow cover on sea ice poses a challenge for radar measurements as microwave penetration into snow is not yet fully understood. In this study, the aim is to investigate microwave penetration into snow on Arctic sea ice using commercial C (6 GHz) and K (26 GHz) band tank radars. Nadir-looking radar measurements collected at nine study locations over first-year and multiyear landfast sea ice in the Lincoln Sea in May 2018 are analysed together with detailed measurements of the physical properties of the snow cover to determine the dominant scattering horizons at both frequencies. They are evaluated for the feasibility to determine snow depth. The results show that in 39% of the measurements and only on first-year ice a major fraction of the C band radar backscatter originated closer to the snow–ice interface potentially enabling snow depth retrieval. At K band, 81% of the radar returns originated from the snow surface. Partly confirming the findings of previous studies, however, the analysis was potentially hampered by relatively warm air temperatures (up to $-0.9^\circ$C) during the study period as well as stratigraphic features and inconclusive microwave interaction with the saline basal layers found in the snow cover on first-year ice. |
format |
Article in Journal/Newspaper |
author |
Arttu Jutila Christian Haas |
author_facet |
Arttu Jutila Christian Haas |
author_sort |
Arttu Jutila |
title |
C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars |
title_short |
C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars |
title_full |
C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars |
title_fullStr |
C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars |
title_full_unstemmed |
C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars |
title_sort |
c and k band microwave penetration into snow on sea ice studied with off-the-shelf tank radars |
publisher |
Cambridge University Press |
url |
https://doi.org/10.1017/aog.2023.47 https://doaj.org/article/94f0590f42894c2ca7f3ca0bef9478cf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Annals of Glaciology Arctic Lincoln Sea Sea ice |
genre_facet |
Annals of Glaciology Arctic Lincoln Sea Sea ice |
op_source |
Annals of Glaciology, Pp 1-11 |
op_relation |
https://www.cambridge.org/core/product/identifier/S0260305523000472/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2023.47 0260-3055 1727-5644 https://doaj.org/article/94f0590f42894c2ca7f3ca0bef9478cf |
op_doi |
https://doi.org/10.1017/aog.2023.47 |
container_title |
Annals of Glaciology |
container_start_page |
1 |
op_container_end_page |
11 |
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1772812711724318720 |