Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data

Accurate mapping of fast ice deformation can effectively characterize the rheological behavior of fast ice and subsequently improve sea ice model. This study used the Sentinel-1A descending and ascending orbits data to detect the deformations of fast ice in the Baltic Sea. A method for automatically...

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Published in:E3S Web of Conferences
Main Authors: Jian LIU, Jinning WANG, Zhiyong WANG
Format: Article in Journal/Newspaper
Language:English
French
Published: EDP Sciences 2020
Subjects:
Online Access:https://doi.org/10.1051/e3sconf/202020603028
https://doaj.org/article/ae03d83a51f8485c9edd079f25cdae45
id ftdoajarticles:oai:doaj.org/article:ae03d83a51f8485c9edd079f25cdae45
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:ae03d83a51f8485c9edd079f25cdae45 2023-05-15T18:18:27+02:00 Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data Jian LIU Jinning WANG Zhiyong WANG 2020-01-01T00:00:00Z https://doi.org/10.1051/e3sconf/202020603028 https://doaj.org/article/ae03d83a51f8485c9edd079f25cdae45 EN FR eng fre EDP Sciences https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/66/e3sconf_icgec2020_03028.pdf https://doaj.org/toc/2267-1242 2267-1242 doi:10.1051/e3sconf/202020603028 https://doaj.org/article/ae03d83a51f8485c9edd079f25cdae45 E3S Web of Conferences, Vol 206, p 03028 (2020) Environmental sciences GE1-350 article 2020 ftdoajarticles https://doi.org/10.1051/e3sconf/202020603028 2022-12-31T15:56:50Z Accurate mapping of fast ice deformation can effectively characterize the rheological behavior of fast ice and subsequently improve sea ice model. This study used the Sentinel-1A descending and ascending orbits data to detect the deformations of fast ice in the Baltic Sea. A method for automatically obtaining fast ice edge line by combining interferometric coherence image and SAR amplitude image was proposed. Then, the deformations of fast ice were detected from different incidence angles with the descending and ascending orbits data. The results showed that the deformations in radar line of sight obtained from the descending and ascending orbits data were 38cm and 37cm respectively within the fast ice region of 960km2 in the study area. The continuous strong southwest wind was the principal reason for the deformation, and the deformation direction was dominated by east to west. Moreover, the inner fast ice kept stable and its deformation was smaller due to the protection of outer consolidated ice. The experimental results in this paper showed that the deformation trend and characteristics of fast ice can be better understood by InSAR technology with multi-orbits SAR data. Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles The Sentinel ENVELOPE(73.317,73.317,-52.983,-52.983) E3S Web of Conferences 206 03028
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
French
topic Environmental sciences
GE1-350
spellingShingle Environmental sciences
GE1-350
Jian LIU
Jinning WANG
Zhiyong WANG
Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data
topic_facet Environmental sciences
GE1-350
description Accurate mapping of fast ice deformation can effectively characterize the rheological behavior of fast ice and subsequently improve sea ice model. This study used the Sentinel-1A descending and ascending orbits data to detect the deformations of fast ice in the Baltic Sea. A method for automatically obtaining fast ice edge line by combining interferometric coherence image and SAR amplitude image was proposed. Then, the deformations of fast ice were detected from different incidence angles with the descending and ascending orbits data. The results showed that the deformations in radar line of sight obtained from the descending and ascending orbits data were 38cm and 37cm respectively within the fast ice region of 960km2 in the study area. The continuous strong southwest wind was the principal reason for the deformation, and the deformation direction was dominated by east to west. Moreover, the inner fast ice kept stable and its deformation was smaller due to the protection of outer consolidated ice. The experimental results in this paper showed that the deformation trend and characteristics of fast ice can be better understood by InSAR technology with multi-orbits SAR data.
format Article in Journal/Newspaper
author Jian LIU
Jinning WANG
Zhiyong WANG
author_facet Jian LIU
Jinning WANG
Zhiyong WANG
author_sort Jian LIU
title Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data
title_short Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data
title_full Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data
title_fullStr Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data
title_full_unstemmed Detecting the deformation of fast ice by InSAR technology with Sentinel-1A descending and ascending orbits data
title_sort detecting the deformation of fast ice by insar technology with sentinel-1a descending and ascending orbits data
publisher EDP Sciences
publishDate 2020
url https://doi.org/10.1051/e3sconf/202020603028
https://doaj.org/article/ae03d83a51f8485c9edd079f25cdae45
long_lat ENVELOPE(73.317,73.317,-52.983,-52.983)
geographic The Sentinel
geographic_facet The Sentinel
genre Sea ice
genre_facet Sea ice
op_source E3S Web of Conferences, Vol 206, p 03028 (2020)
op_relation https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/66/e3sconf_icgec2020_03028.pdf
https://doaj.org/toc/2267-1242
2267-1242
doi:10.1051/e3sconf/202020603028
https://doaj.org/article/ae03d83a51f8485c9edd079f25cdae45
op_doi https://doi.org/10.1051/e3sconf/202020603028
container_title E3S Web of Conferences
container_volume 206
container_start_page 03028
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