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...

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Bibliographic Details
Main Authors: Jutila, Arttu, Haas, Christian
Other Authors: orcid:0000-0001-6115-1687, Ilmatieteen laitos, Finnish Meteorological Institute
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society. 2023
Subjects:
ice
Online Access:http://hdl.handle.net/10138/566072
id ftunivhelsihelda:oai:helda.helsinki.fi:10138/566072
record_format openpolar
spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/566072 2023-11-12T04:01:18+01:00 C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars Jutila, Arttu Haas, Christian orcid:0000-0001-6115-1687 Ilmatieteen laitos Finnish Meteorological Institute 2023-10-10T12:34:36Z 1-11 application/pdf http://hdl.handle.net/10138/566072 en eng International Glaciological Society. 10.1017/aog.2023.47 Annals of glaciology 0260-3055 1727-5644 88071 http://hdl.handle.net/10138/566072 URN:NBN:fi-fe20231010139546 CC BY 4.0 snow sea ice remote sensing radars ice ice cover snow cover microwaves measurement glaciology lumi jää jääpeite lumipeite tutkat mikroaallot mittaus glasiologia merijää A1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä A1 Journal article (refereed), original research 2023 ftunivhelsihelda 2023-10-18T23:01:29Z 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◦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 HELDA – University of Helsinki Open Repository Arctic
institution Open Polar
collection HELDA – University of Helsinki Open Repository
op_collection_id ftunivhelsihelda
language English
topic snow
sea ice
remote sensing
radars
ice
ice cover
snow cover
microwaves
measurement
glaciology
lumi
jää
jääpeite
lumipeite
tutkat
mikroaallot
mittaus
glasiologia
merijää
spellingShingle snow
sea ice
remote sensing
radars
ice
ice cover
snow cover
microwaves
measurement
glaciology
lumi
jää
jääpeite
lumipeite
tutkat
mikroaallot
mittaus
glasiologia
merijää
Jutila, Arttu
Haas, Christian
C and K band microwave penetration into snow on sea ice studied with off-the-shelf tank radars
topic_facet snow
sea ice
remote sensing
radars
ice
ice cover
snow cover
microwaves
measurement
glaciology
lumi
jää
jääpeite
lumipeite
tutkat
mikroaallot
mittaus
glasiologia
merijää
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◦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.
author2 orcid:0000-0001-6115-1687
Ilmatieteen laitos
Finnish Meteorological Institute
format Article in Journal/Newspaper
author Jutila, Arttu
Haas, Christian
author_facet Jutila, Arttu
Haas, Christian
author_sort Jutila, Arttu
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 International Glaciological Society.
publishDate 2023
url http://hdl.handle.net/10138/566072
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_relation 10.1017/aog.2023.47
Annals of glaciology
0260-3055
1727-5644
88071
http://hdl.handle.net/10138/566072
URN:NBN:fi-fe20231010139546
op_rights CC BY 4.0
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