Gaining a three-dimensional picture of recent Antarctic sea ice variability

Southern Ocean sea ice has undergone dramatic losses in extent in recent years, this year reaching a record (40-year) low of 1.91 million square kilometres in early February, weeks before its minimum annual extent. These drastic losses have garnered much attention from the scientific community and t...

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Main Authors: Lawrence, I., Shepherd, A., Wilkinson, J., Holland, P.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021493
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021493 2023-07-30T03:58:16+02:00 Gaining a three-dimensional picture of recent Antarctic sea ice variability Lawrence, I. Shepherd, A. Wilkinson, J. Holland, P. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021493 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4053 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021493 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4053 2023-07-09T23:40:20Z Southern Ocean sea ice has undergone dramatic losses in extent in recent years, this year reaching a record (40-year) low of 1.91 million square kilometres in early February, weeks before its minimum annual extent. These drastic losses have garnered much attention from the scientific community and the media, but for the moment our understanding of these events remains two-dimensional because observations of sea ice thickness and volume are limited. Were changes in extent caused by increased convergence of the sea ice pack with a little overall change in volume? or did thermodynamic forcing during low-extent years promote thinner ice more prone to summer melt?Here we utilise data from the ESA CryoSat-2 and Copernicus Sentinel-3 radar altimetry missions, combining radar freeboard with a newly developed snow-on-Antarctic-sea-ice model to derive circumpolar sea ice thickness and volume from 2011 to 2023. We assess the variability in sea ice thickness in the run-up to the February minimum, focussing on the difference between below-average and above-average extent years to ascertain if low summer extent was facilitated by a thinner winter-spring ice pack.Using sea ice concentration and motion data, we then decompose sea ice thickness changes into dynamic and thermodynamic components to understand the principal driving mechanisms behind sea ice thickness variability between 2011-2023, and the dramatic extent losses of 2017, 2022 and 2023.This work forms part of the NERC DEFIANT project, which combines new in-situ and satellite data sets with advanced modelling techniques to better understand the drivers and effects of Antarctic sea ice variability. Conference Object Antarc* Antarctic ice pack Sea ice Southern Ocean GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Antarctic Southern Ocean
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Southern Ocean sea ice has undergone dramatic losses in extent in recent years, this year reaching a record (40-year) low of 1.91 million square kilometres in early February, weeks before its minimum annual extent. These drastic losses have garnered much attention from the scientific community and the media, but for the moment our understanding of these events remains two-dimensional because observations of sea ice thickness and volume are limited. Were changes in extent caused by increased convergence of the sea ice pack with a little overall change in volume? or did thermodynamic forcing during low-extent years promote thinner ice more prone to summer melt?Here we utilise data from the ESA CryoSat-2 and Copernicus Sentinel-3 radar altimetry missions, combining radar freeboard with a newly developed snow-on-Antarctic-sea-ice model to derive circumpolar sea ice thickness and volume from 2011 to 2023. We assess the variability in sea ice thickness in the run-up to the February minimum, focussing on the difference between below-average and above-average extent years to ascertain if low summer extent was facilitated by a thinner winter-spring ice pack.Using sea ice concentration and motion data, we then decompose sea ice thickness changes into dynamic and thermodynamic components to understand the principal driving mechanisms behind sea ice thickness variability between 2011-2023, and the dramatic extent losses of 2017, 2022 and 2023.This work forms part of the NERC DEFIANT project, which combines new in-situ and satellite data sets with advanced modelling techniques to better understand the drivers and effects of Antarctic sea ice variability.
format Conference Object
author Lawrence, I.
Shepherd, A.
Wilkinson, J.
Holland, P.
spellingShingle Lawrence, I.
Shepherd, A.
Wilkinson, J.
Holland, P.
Gaining a three-dimensional picture of recent Antarctic sea ice variability
author_facet Lawrence, I.
Shepherd, A.
Wilkinson, J.
Holland, P.
author_sort Lawrence, I.
title Gaining a three-dimensional picture of recent Antarctic sea ice variability
title_short Gaining a three-dimensional picture of recent Antarctic sea ice variability
title_full Gaining a three-dimensional picture of recent Antarctic sea ice variability
title_fullStr Gaining a three-dimensional picture of recent Antarctic sea ice variability
title_full_unstemmed Gaining a three-dimensional picture of recent Antarctic sea ice variability
title_sort gaining a three-dimensional picture of recent antarctic sea ice variability
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021493
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
ice pack
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
ice pack
Sea ice
Southern Ocean
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4053
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021493
op_doi https://doi.org/10.57757/IUGG23-4053
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