Physical and morphological properties of first-year Antarctic sea ice in the spring marginal ice zone of the Atlantic-Indian sector

This study presents the first dataset of physical and textural properties of sea ice collected in the South Atlantic and Indian Ocean sector of the Antarctic marginal ice zone (MIZ). Observations of sea ice from this region in the austral spring 2019, including sea-ice core temperature, salinity, cr...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Siobhan Johnson, Riesna R. Audh, Wayne de Jager, Boitumelo Matlakala, Marcello Vichi, Ashleigh Womack, Tokoloho Rampai
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Crystal growth
frazil ice
ice/atmosphere interactions
sea ice
sea-ice growth and decay
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Antarctic
Austral
Indian
The Antarctic
Antarc*
ice core
ice pack
Journal of Glaciology
Sea ice
Online Access:https://doi.org/10.1017/jog.2023.21
https://doaj.org/article/d99c9a0e8fa346429852ec4b11ce045a
Description
Summary:This study presents the first dataset of physical and textural properties of sea ice collected in the South Atlantic and Indian Ocean sector of the Antarctic marginal ice zone (MIZ). Observations of sea ice from this region in the austral spring 2019, including sea-ice core temperature, salinity, crystal size, texture, oxygen isotopes and stratigraphy, were used in conjunction with a Lagrangian back-tracking algorithm and atmospheric reanalyses. This method relates the reconstructed synoptic conditions to sea-ice growth along the transect. A significant difference was found between the stratigraphy of consolidated pack ice samples collected at the same latitude and spanning over 550 km eastwards. The eastward group was found to have more disturbances in their stratigraphy which is attributed to the highly variable atmospheric and sea-ice conditions together with varying wave penetration through the sea-ice pack, notably during the passage of an intense polar cyclone, while the westward group showed no signs of disturbance or deformation. These results indicate that consolidated Antarctic sea-ice floes of similar thickness and from the same latitude in the MIZ have distinct stratigraphic properties, which will influence their physical and biogeochemical features.

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