The distribution and evolution of surface fractures on pan-Antarctic ice shelves
Surface fractures have a great impact on ice shelf stability in Antarctica and can be considered precursors of ice shelf calving. However, our understanding of the spatial distribution and temporal evolution of surface fractures on the Antarctic ice shelf is limited. In this study, a ResUNet model w...
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2023
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Online Access: | https://doi.org/10.1080/17538947.2023.2246436 https://doaj.org/article/e2e6cb61da7e459a9431427c4d1002b5 |
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ftdoajarticles:oai:doaj.org/article:e2e6cb61da7e459a9431427c4d1002b5 2023-10-09T21:46:55+02:00 The distribution and evolution of surface fractures on pan-Antarctic ice shelves Ao Pang Qi Liang Weijia Li Lei Zheng Teng Li Xiao Cheng 2023-12-01T00:00:00Z https://doi.org/10.1080/17538947.2023.2246436 https://doaj.org/article/e2e6cb61da7e459a9431427c4d1002b5 EN eng Taylor & Francis Group http://dx.doi.org/10.1080/17538947.2023.2246436 https://doaj.org/toc/1753-8947 https://doaj.org/toc/1753-8955 1753-8947 1753-8955 doi:10.1080/17538947.2023.2246436 https://doaj.org/article/e2e6cb61da7e459a9431427c4d1002b5 International Journal of Digital Earth, Vol 16, Iss 1, Pp 3295-3320 (2023) surface fractures antarctic ice shelf resunet moa Mathematical geography. Cartography GA1-1776 article 2023 ftdoajarticles https://doi.org/10.1080/17538947.2023.2246436 2023-09-24T00:35:54Z Surface fractures have a great impact on ice shelf stability in Antarctica and can be considered precursors of ice shelf calving. However, our understanding of the spatial distribution and temporal evolution of surface fractures on the Antarctic ice shelf is limited. In this study, a ResUNet model was implemented on the Moderate Resolution Imaging Spectroradiometer (MODIS)-based Mosaic of Antarctica (MOA) to identify the spatial distribution of Antarctic ice shelf surface fractures in 2004, 2009, and 2014. The accuracy of identification had an F1 value of 0.771. Our model identified 44744.59$\; \pm \;$2619.61 km² of surface fractures in 2004, 43737.15$\; \pm \;$2644.60 km² in 2009, and 42978.67 $\pm \;$2639.33 km² in 2014. The reduction is primarily attributed to the variation in surface fractures within 20 km of the ice front, paratactically in the Amundsen and Wilkes sectors. Ice shelves in the Amundsen sector typically have a widespread distribution of surface fractures, with particularly high concentrations found in the Thwaites Ice Shelf, Crosson Ice Shelf and Getz Ice Shelf. The Brunt Ice Shelf also exhibits numerous surface fractures. This study provides comprehensive and detailed information about surface fractures on Antarctic ice shelves, carrying implications for evaluating ice shelf vulnerability. Article in Journal/Newspaper Antarc* Antarctic Antarctica Brunt Ice Shelf Crosson Ice Shelf Getz Ice Shelf Ice Shelf Ice Shelves Thwaites Ice Shelf Directory of Open Access Journals: DOAJ Articles Antarctic Brunt Ice Shelf ENVELOPE(-22.500,-22.500,-74.750,-74.750) Crosson Ice Shelf ENVELOPE(-109.500,-109.500,-74.950,-74.950) Getz ENVELOPE(-145.217,-145.217,-76.550,-76.550) Getz Ice Shelf ENVELOPE(-126.500,-126.500,-74.250,-74.250) Moa ENVELOPE(157.950,157.950,-80.767,-80.767) The Antarctic International Journal of Digital Earth 16 1 3295 3320 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
surface fractures antarctic ice shelf resunet moa Mathematical geography. Cartography GA1-1776 |
spellingShingle |
surface fractures antarctic ice shelf resunet moa Mathematical geography. Cartography GA1-1776 Ao Pang Qi Liang Weijia Li Lei Zheng Teng Li Xiao Cheng The distribution and evolution of surface fractures on pan-Antarctic ice shelves |
topic_facet |
surface fractures antarctic ice shelf resunet moa Mathematical geography. Cartography GA1-1776 |
description |
Surface fractures have a great impact on ice shelf stability in Antarctica and can be considered precursors of ice shelf calving. However, our understanding of the spatial distribution and temporal evolution of surface fractures on the Antarctic ice shelf is limited. In this study, a ResUNet model was implemented on the Moderate Resolution Imaging Spectroradiometer (MODIS)-based Mosaic of Antarctica (MOA) to identify the spatial distribution of Antarctic ice shelf surface fractures in 2004, 2009, and 2014. The accuracy of identification had an F1 value of 0.771. Our model identified 44744.59$\; \pm \;$2619.61 km² of surface fractures in 2004, 43737.15$\; \pm \;$2644.60 km² in 2009, and 42978.67 $\pm \;$2639.33 km² in 2014. The reduction is primarily attributed to the variation in surface fractures within 20 km of the ice front, paratactically in the Amundsen and Wilkes sectors. Ice shelves in the Amundsen sector typically have a widespread distribution of surface fractures, with particularly high concentrations found in the Thwaites Ice Shelf, Crosson Ice Shelf and Getz Ice Shelf. The Brunt Ice Shelf also exhibits numerous surface fractures. This study provides comprehensive and detailed information about surface fractures on Antarctic ice shelves, carrying implications for evaluating ice shelf vulnerability. |
format |
Article in Journal/Newspaper |
author |
Ao Pang Qi Liang Weijia Li Lei Zheng Teng Li Xiao Cheng |
author_facet |
Ao Pang Qi Liang Weijia Li Lei Zheng Teng Li Xiao Cheng |
author_sort |
Ao Pang |
title |
The distribution and evolution of surface fractures on pan-Antarctic ice shelves |
title_short |
The distribution and evolution of surface fractures on pan-Antarctic ice shelves |
title_full |
The distribution and evolution of surface fractures on pan-Antarctic ice shelves |
title_fullStr |
The distribution and evolution of surface fractures on pan-Antarctic ice shelves |
title_full_unstemmed |
The distribution and evolution of surface fractures on pan-Antarctic ice shelves |
title_sort |
distribution and evolution of surface fractures on pan-antarctic ice shelves |
publisher |
Taylor & Francis Group |
publishDate |
2023 |
url |
https://doi.org/10.1080/17538947.2023.2246436 https://doaj.org/article/e2e6cb61da7e459a9431427c4d1002b5 |
long_lat |
ENVELOPE(-22.500,-22.500,-74.750,-74.750) ENVELOPE(-109.500,-109.500,-74.950,-74.950) ENVELOPE(-145.217,-145.217,-76.550,-76.550) ENVELOPE(-126.500,-126.500,-74.250,-74.250) ENVELOPE(157.950,157.950,-80.767,-80.767) |
geographic |
Antarctic Brunt Ice Shelf Crosson Ice Shelf Getz Getz Ice Shelf Moa The Antarctic |
geographic_facet |
Antarctic Brunt Ice Shelf Crosson Ice Shelf Getz Getz Ice Shelf Moa The Antarctic |
genre |
Antarc* Antarctic Antarctica Brunt Ice Shelf Crosson Ice Shelf Getz Ice Shelf Ice Shelf Ice Shelves Thwaites Ice Shelf |
genre_facet |
Antarc* Antarctic Antarctica Brunt Ice Shelf Crosson Ice Shelf Getz Ice Shelf Ice Shelf Ice Shelves Thwaites Ice Shelf |
op_source |
International Journal of Digital Earth, Vol 16, Iss 1, Pp 3295-3320 (2023) |
op_relation |
http://dx.doi.org/10.1080/17538947.2023.2246436 https://doaj.org/toc/1753-8947 https://doaj.org/toc/1753-8955 1753-8947 1753-8955 doi:10.1080/17538947.2023.2246436 https://doaj.org/article/e2e6cb61da7e459a9431427c4d1002b5 |
op_doi |
https://doi.org/10.1080/17538947.2023.2246436 |
container_title |
International Journal of Digital Earth |
container_volume |
16 |
container_issue |
1 |
container_start_page |
3295 |
op_container_end_page |
3320 |
_version_ |
1779309536275857408 |