Change in Antarctic Ice Shelf Area from 2009 to 2019

Antarctic ice shelves provide buttressing support to the ice sheet, stabilising the flow of grounded ice and its contribution to global sea levels. Over the past 50 years, satellite observations have shown ice shelves collapse, thin, and retreat; however, there are few measurements of the Antarctic-...

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Main Authors: Andreasen, Julia R., Hogg, Anna E., Selley, Heather L.
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-1087
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1087/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere107053 2023-07-16T03:54:26+02:00 Change in Antarctic Ice Shelf Area from 2009 to 2019 Andreasen, Julia R. Hogg, Anna E. Selley, Heather L. 2023-06-21 application/pdf https://doi.org/10.5194/egusphere-2022-1087 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1087/ eng eng doi:10.5194/egusphere-2022-1087 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1087/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2022-1087 2023-06-26T16:24:20Z Antarctic ice shelves provide buttressing support to the ice sheet, stabilising the flow of grounded ice and its contribution to global sea levels. Over the past 50 years, satellite observations have shown ice shelves collapse, thin, and retreat; however, there are few measurements of the Antarctic-wide change in ice shelf area. Here, we use MODIS (Moderate Resolution Imaging Spectroradiometer) satellite data to measure the change in ice shelf calving front position and area on 34 ice shelves in Antarctica from 2009 to 2019. Over the last decade, a reduction in the area on the Antarctic Peninsula (6693 km 2 ) and West Antarctica (5563 km 2 ) has been outweighed by area growth in East Antarctica (3532 km 2 ) and the large Ross and Ronne–Filchner ice shelves (14 028 km 2 ). The largest retreat was observed on the Larsen C Ice Shelf, where 5917 km 2 of ice was lost during an individual calving event in 2017, and the largest area increase was observed on Ronne Ice Shelf in East Antarctica, where a gradual advance over the past decade (535 km 2 yr −1 ) led to a 5889 km 2 area gain from 2009 to 2019. Overall, the Antarctic ice shelf area has grown by 5305 km 2 since 2009, with 18 ice shelves retreating and 16 larger shelves growing in area. Our observations show that Antarctic ice shelves gained 661 Gt of ice mass over the past decade, whereas the steady-state approach would estimate substantial ice loss over the same period, demonstrating the importance of using time-variable calving flux observations to measure change. Text Antarc* Antarctic Antarctic Peninsula Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves Ronne Ice Shelf West Antarctica Copernicus Publications: E-Journals Antarctic The Antarctic Antarctic Peninsula East Antarctica West Antarctica Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Antarctic ice shelves provide buttressing support to the ice sheet, stabilising the flow of grounded ice and its contribution to global sea levels. Over the past 50 years, satellite observations have shown ice shelves collapse, thin, and retreat; however, there are few measurements of the Antarctic-wide change in ice shelf area. Here, we use MODIS (Moderate Resolution Imaging Spectroradiometer) satellite data to measure the change in ice shelf calving front position and area on 34 ice shelves in Antarctica from 2009 to 2019. Over the last decade, a reduction in the area on the Antarctic Peninsula (6693 km 2 ) and West Antarctica (5563 km 2 ) has been outweighed by area growth in East Antarctica (3532 km 2 ) and the large Ross and Ronne–Filchner ice shelves (14 028 km 2 ). The largest retreat was observed on the Larsen C Ice Shelf, where 5917 km 2 of ice was lost during an individual calving event in 2017, and the largest area increase was observed on Ronne Ice Shelf in East Antarctica, where a gradual advance over the past decade (535 km 2 yr −1 ) led to a 5889 km 2 area gain from 2009 to 2019. Overall, the Antarctic ice shelf area has grown by 5305 km 2 since 2009, with 18 ice shelves retreating and 16 larger shelves growing in area. Our observations show that Antarctic ice shelves gained 661 Gt of ice mass over the past decade, whereas the steady-state approach would estimate substantial ice loss over the same period, demonstrating the importance of using time-variable calving flux observations to measure change.
format Text
author Andreasen, Julia R.
Hogg, Anna E.
Selley, Heather L.
spellingShingle Andreasen, Julia R.
Hogg, Anna E.
Selley, Heather L.
Change in Antarctic Ice Shelf Area from 2009 to 2019
author_facet Andreasen, Julia R.
Hogg, Anna E.
Selley, Heather L.
author_sort Andreasen, Julia R.
title Change in Antarctic Ice Shelf Area from 2009 to 2019
title_short Change in Antarctic Ice Shelf Area from 2009 to 2019
title_full Change in Antarctic Ice Shelf Area from 2009 to 2019
title_fullStr Change in Antarctic Ice Shelf Area from 2009 to 2019
title_full_unstemmed Change in Antarctic Ice Shelf Area from 2009 to 2019
title_sort change in antarctic ice shelf area from 2009 to 2019
publishDate 2023
url https://doi.org/10.5194/egusphere-2022-1087
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1087/
long_lat ENVELOPE(-61.000,-61.000,-78.500,-78.500)
geographic Antarctic
The Antarctic
Antarctic Peninsula
East Antarctica
West Antarctica
Ronne Ice Shelf
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
East Antarctica
West Antarctica
Ronne Ice Shelf
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Ronne Ice Shelf
West Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Ronne Ice Shelf
West Antarctica
op_source eISSN:
op_relation doi:10.5194/egusphere-2022-1087
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1087/
op_doi https://doi.org/10.5194/egusphere-2022-1087
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