Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning
Sea level rise contribution from the Antarctic ice sheet is influenced by changes in glacier and ice shelf front position. Still, little is known about seasonal glacier and ice shelf front fluctuations as the manual delineation of calving fronts from remote sensing imagery is very time-consuming. Th...
Published in: | Remote Sensing |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute (MDPI)
2019
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Subjects: | |
Online Access: | https://elib.dlr.de/129964/ |
_version_ | 1835015656439808000 |
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author | Baumhoer, Celia Dietz, Andreas Kneisel, Christoph Kuenzer, Claudia |
author_facet | Baumhoer, Celia Dietz, Andreas Kneisel, Christoph Kuenzer, Claudia |
author_sort | Baumhoer, Celia |
collection | Unknown |
container_issue | 21 |
container_start_page | 2529 |
container_title | Remote Sensing |
container_volume | 11 |
description | Sea level rise contribution from the Antarctic ice sheet is influenced by changes in glacier and ice shelf front position. Still, little is known about seasonal glacier and ice shelf front fluctuations as the manual delineation of calving fronts from remote sensing imagery is very time-consuming. The major challenge of automatic calving front extraction is the low contrast between floating glacier and ice shelf fronts and the surrounding sea ice. Additionally, in previous decades, remote sensing imagery over the often cloud-covered Antarctic coastline was limited. Nowadays, an abundance of Sentinel-1 imagery over the Antarctic coastline exists and could be used for tracking glacier and ice shelf front movement. To exploit the available Sentinel-1 data, we developed a processing chain allowing automatic extraction of the Antarctic coastline from Seninel-1 imagery and the creation of dense time series to assess calving front change. The core of the proposed workflow is a modified version of the deep learning architecture U-Net. This convolutional neural network (CNN) performs a semantic segmentation on dual-pol Sentinel-1 data and the Antarctic TanDEM-X digital elevation model (DEM). The proposed method is tested for four training and test areas along the Antarctic coastline. The automatically extracted fronts deviate on average 78 m in training and 108 m test areas. Spatial and temporal transferability is demonstrated on an automatically extracted 15-month time series along the Getz Ice Shelf. Between May 2017 and July 2018, the fronts along the Getz Ice Shelf show mostly an advancing tendency with the fastest moving front of DeVicq Glacier with 726 ± 20 m/yr. |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic DeVicq Glacier Getz Ice Shelf Ice Sheet Ice Shelf Sea ice |
genre_facet | Antarc* Antarctic DeVicq Glacier Getz Ice Shelf Ice Sheet Ice Shelf Sea ice |
geographic | Antarctic DeVicq Glacier Getz Getz Ice Shelf The Antarctic |
geographic_facet | Antarctic DeVicq Glacier Getz Getz Ice Shelf The Antarctic |
id | ftdlr:oai:elib.dlr.de:129964 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-131.000,-131.000,-75.000,-75.000) ENVELOPE(-145.217,-145.217,-76.550,-76.550) ENVELOPE(-126.500,-126.500,-74.250,-74.250) |
op_collection_id | ftdlr |
op_doi | https://doi.org/10.3390/rs11212529 |
op_relation | https://elib.dlr.de/129964/1/remotesensing-11-02529.pdf Baumhoer, Celia und Dietz, Andreas und Kneisel, Christoph und Kuenzer, Claudia (2019) Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning. Remote Sensing, 11 (21), Seiten 1-22. Multidisciplinary Digital Publishing Institute (MDPI). doi:10.3390/rs11212529 <https://doi.org/10.3390/rs11212529>. ISSN 2072-4292. |
op_rights | cc_by |
publishDate | 2019 |
publisher | Multidisciplinary Digital Publishing Institute (MDPI) |
record_format | openpolar |
spelling | ftdlr:oai:elib.dlr.de:129964 2025-06-15T14:08:49+00:00 Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning Baumhoer, Celia Dietz, Andreas Kneisel, Christoph Kuenzer, Claudia 2019-10-29 application/pdf https://elib.dlr.de/129964/ en eng Multidisciplinary Digital Publishing Institute (MDPI) https://elib.dlr.de/129964/1/remotesensing-11-02529.pdf Baumhoer, Celia und Dietz, Andreas und Kneisel, Christoph und Kuenzer, Claudia (2019) Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning. Remote Sensing, 11 (21), Seiten 1-22. Multidisciplinary Digital Publishing Institute (MDPI). doi:10.3390/rs11212529 <https://doi.org/10.3390/rs11212529>. ISSN 2072-4292. cc_by Dynamik der Landoberfläche Zeitschriftenbeitrag PeerReviewed 2019 ftdlr https://doi.org/10.3390/rs11212529 2025-06-04T04:58:07Z Sea level rise contribution from the Antarctic ice sheet is influenced by changes in glacier and ice shelf front position. Still, little is known about seasonal glacier and ice shelf front fluctuations as the manual delineation of calving fronts from remote sensing imagery is very time-consuming. The major challenge of automatic calving front extraction is the low contrast between floating glacier and ice shelf fronts and the surrounding sea ice. Additionally, in previous decades, remote sensing imagery over the often cloud-covered Antarctic coastline was limited. Nowadays, an abundance of Sentinel-1 imagery over the Antarctic coastline exists and could be used for tracking glacier and ice shelf front movement. To exploit the available Sentinel-1 data, we developed a processing chain allowing automatic extraction of the Antarctic coastline from Seninel-1 imagery and the creation of dense time series to assess calving front change. The core of the proposed workflow is a modified version of the deep learning architecture U-Net. This convolutional neural network (CNN) performs a semantic segmentation on dual-pol Sentinel-1 data and the Antarctic TanDEM-X digital elevation model (DEM). The proposed method is tested for four training and test areas along the Antarctic coastline. The automatically extracted fronts deviate on average 78 m in training and 108 m test areas. Spatial and temporal transferability is demonstrated on an automatically extracted 15-month time series along the Getz Ice Shelf. Between May 2017 and July 2018, the fronts along the Getz Ice Shelf show mostly an advancing tendency with the fastest moving front of DeVicq Glacier with 726 ± 20 m/yr. Article in Journal/Newspaper Antarc* Antarctic DeVicq Glacier Getz Ice Shelf Ice Sheet Ice Shelf Sea ice Unknown Antarctic DeVicq Glacier ENVELOPE(-131.000,-131.000,-75.000,-75.000) Getz ENVELOPE(-145.217,-145.217,-76.550,-76.550) Getz Ice Shelf ENVELOPE(-126.500,-126.500,-74.250,-74.250) The Antarctic Remote Sensing 11 21 2529 |
spellingShingle | Dynamik der Landoberfläche Baumhoer, Celia Dietz, Andreas Kneisel, Christoph Kuenzer, Claudia Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning |
title | Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning |
title_full | Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning |
title_fullStr | Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning |
title_full_unstemmed | Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning |
title_short | Automated Extraction of Antarctic Glacier and Ice Shelf Fronts from Sentinel-1 Imagery Using Deep Learning |
title_sort | automated extraction of antarctic glacier and ice shelf fronts from sentinel-1 imagery using deep learning |
topic | Dynamik der Landoberfläche |
topic_facet | Dynamik der Landoberfläche |
url | https://elib.dlr.de/129964/ |