SAR Observation of Waves under Ice in the Marginal Ice Zone

The marginal ice zone (MIZ) connects the open ocean and the pack ice, playing significant roles in shaping the ice edge and wave–ice interaction. Spaceborne synthetic aperture radar (SAR) has been demonstrated to be one of the most advantageous sensors for MIZ exploration given its capability to col...

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Published in:Journal of Marine Science and Engineering
Main Authors: Ziyue Dai, Huimin Li, Dongbo Liu, Chen Wang, Lijian Shi, Yijun He
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/jmse10121836
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spelling ftmdpi:oai:mdpi.com:/2077-1312/10/12/1836/ 2023-08-20T04:02:25+02:00 SAR Observation of Waves under Ice in the Marginal Ice Zone Ziyue Dai Huimin Li Dongbo Liu Chen Wang Lijian Shi Yijun He agris 2022-11-29 application/pdf https://doi.org/10.3390/jmse10121836 EN eng Multidisciplinary Digital Publishing Institute Physical Oceanography https://dx.doi.org/10.3390/jmse10121836 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 10; Issue 12; Pages: 1836 Sentinel-1 wave mode marginal ice zone azimuth cutoff Text 2022 ftmdpi https://doi.org/10.3390/jmse10121836 2023-08-01T07:34:27Z The marginal ice zone (MIZ) connects the open ocean and the pack ice, playing significant roles in shaping the ice edge and wave–ice interaction. Spaceborne synthetic aperture radar (SAR) has been demonstrated to be one of the most advantageous sensors for MIZ exploration given its capability to collect images under all weather conditions during day and night. In this study, we take advantage of the Sentinel-1 wave mode vignettes acquired around the Antarctic to quantify the image properties over MIZ. A data set of SAR images covering the ice edge with both open water and sea ice present in the same scene was created by manual inspection. It is found that the radar return over sea ice decreases by an average of approximately 1.78 dB in comparison to its adjacent open water, which is roughly independent of the polarizations and incidence angles. The long ocean waves are barely attenuated right across the ice edge in terms of their comparable azimuth cutoff. Further inside the ice from the edge, the waves are gradually dampened out at distances associated with their wavelengths. The results obtained in this study shall help interpret the radar scattering model validation as well as the wave–ice interaction. Text Antarc* Antarctic Sea ice MDPI Open Access Publishing Antarctic The Antarctic The Sentinel ENVELOPE(73.317,73.317,-52.983,-52.983) Journal of Marine Science and Engineering 10 12 1836
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Sentinel-1 wave mode
marginal ice zone
azimuth cutoff
spellingShingle Sentinel-1 wave mode
marginal ice zone
azimuth cutoff
Ziyue Dai
Huimin Li
Dongbo Liu
Chen Wang
Lijian Shi
Yijun He
SAR Observation of Waves under Ice in the Marginal Ice Zone
topic_facet Sentinel-1 wave mode
marginal ice zone
azimuth cutoff
description The marginal ice zone (MIZ) connects the open ocean and the pack ice, playing significant roles in shaping the ice edge and wave–ice interaction. Spaceborne synthetic aperture radar (SAR) has been demonstrated to be one of the most advantageous sensors for MIZ exploration given its capability to collect images under all weather conditions during day and night. In this study, we take advantage of the Sentinel-1 wave mode vignettes acquired around the Antarctic to quantify the image properties over MIZ. A data set of SAR images covering the ice edge with both open water and sea ice present in the same scene was created by manual inspection. It is found that the radar return over sea ice decreases by an average of approximately 1.78 dB in comparison to its adjacent open water, which is roughly independent of the polarizations and incidence angles. The long ocean waves are barely attenuated right across the ice edge in terms of their comparable azimuth cutoff. Further inside the ice from the edge, the waves are gradually dampened out at distances associated with their wavelengths. The results obtained in this study shall help interpret the radar scattering model validation as well as the wave–ice interaction.
format Text
author Ziyue Dai
Huimin Li
Dongbo Liu
Chen Wang
Lijian Shi
Yijun He
author_facet Ziyue Dai
Huimin Li
Dongbo Liu
Chen Wang
Lijian Shi
Yijun He
author_sort Ziyue Dai
title SAR Observation of Waves under Ice in the Marginal Ice Zone
title_short SAR Observation of Waves under Ice in the Marginal Ice Zone
title_full SAR Observation of Waves under Ice in the Marginal Ice Zone
title_fullStr SAR Observation of Waves under Ice in the Marginal Ice Zone
title_full_unstemmed SAR Observation of Waves under Ice in the Marginal Ice Zone
title_sort sar observation of waves under ice in the marginal ice zone
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/jmse10121836
op_coverage agris
long_lat ENVELOPE(73.317,73.317,-52.983,-52.983)
geographic Antarctic
The Antarctic
The Sentinel
geographic_facet Antarctic
The Antarctic
The Sentinel
genre Antarc*
Antarctic
Sea ice
genre_facet Antarc*
Antarctic
Sea ice
op_source Journal of Marine Science and Engineering; Volume 10; Issue 12; Pages: 1836
op_relation Physical Oceanography
https://dx.doi.org/10.3390/jmse10121836
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse10121836
container_title Journal of Marine Science and Engineering
container_volume 10
container_issue 12
container_start_page 1836
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