Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry
<p>The recent rapid growth of rifts in the Brunt Ice Shelf appears to signal the onset of its largest calving event since records began in 1915. The aim of this study is to determine whether this calving event will lead to a new steady state in which the Brunt Ice Shelf remains in contact with...
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doaj-a6bdde021b6a4896ae7ae8c881b457ff2020-11-24T23:54:41ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242019-02-011354555610.5194/tc-13-545-2019Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometryD. A. Hodgson0D. A. Hodgson1T. A. Jordan2J. De Rydt3P. T. Fretwell4S. A. Seddon5S. A. Seddon6D. Becker7K. A. Hogan8A. M. Smith9D. G. Vaughan10British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UKDepartment of Geography, Durham University, Durham, DH1 3LE, UKBritish Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UKDepartment of Geography and Environmental Sciences, Faculty of Engineering and Environment, Northumbria University, Newcastle upon Tyne, UKBritish Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UKBritish Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UKSeddon Geophysical Limited, Ipswich, UKPhysical and Satellite Geodesy, Technische Universitaet Darmstadt, Franziska-Braun-Str. 7, 64287 Darmstadt, GermanyBritish Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UKBritish Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UKBritish Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK<p>The recent rapid growth of rifts in the Brunt Ice Shelf appears to signal the onset of its largest calving event since records began in 1915. The aim of this study is to determine whether this calving event will lead to a new steady state in which the Brunt Ice Shelf remains in contact with the bed, or an unpinning from the bed, which could predispose it to accelerated flow or possible break-up. We use a range of geophysical data to reconstruct the sea-floor bathymetry and ice shelf geometry, to examine past ice sheet configurations in the Brunt Basin, and to define the present-day geometry of the contact between the Brunt Ice Shelf and the bed. Results show that during past ice advances grounded ice streams likely converged in the Brunt Basin from the south and east. As the ice retreated, it was likely pinned on at least three former grounding lines marked by topographic highs, and transverse ridges on the flanks of the basin. These may have subsequently formed pinning points for developing ice shelves. The ice shelf geometry and bathymetry measurements show that the base of the Brunt Ice Shelf now only makes contact with one of these topographic highs. This contact is limited to an area of less than 1.3 to 3 km<span class="inline-formula"><sup>2</sup></span> and results in a compressive regime that helps to maintain the ice shelf's integrity. The maximum overlap between ice shelf draft and the bathymetric high is 2–25 m and is contingent on the presence of incorporated iceberg keels, which protrude beneath the base of the ice shelf. The future of the ice shelf depends on whether the expected calving event causes full or partial loss of contact with the bed and whether the subsequent response causes re-grounding within a predictable period or a loss of structural integrity resulting from properties inherited at the grounding line.</p>https://www.the-cryosphere.net/13/545/2019/tc-13-545-2019.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
D. A. Hodgson D. A. Hodgson T. A. Jordan J. De Rydt P. T. Fretwell S. A. Seddon S. A. Seddon D. Becker K. A. Hogan A. M. Smith D. G. Vaughan |
spellingShingle |
D. A. Hodgson D. A. Hodgson T. A. Jordan J. De Rydt P. T. Fretwell S. A. Seddon S. A. Seddon D. Becker K. A. Hogan A. M. Smith D. G. Vaughan Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry The Cryosphere |
author_facet |
D. A. Hodgson D. A. Hodgson T. A. Jordan J. De Rydt P. T. Fretwell S. A. Seddon S. A. Seddon D. Becker K. A. Hogan A. M. Smith D. G. Vaughan |
author_sort |
D. A. Hodgson |
title |
Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry |
title_short |
Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry |
title_full |
Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry |
title_fullStr |
Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry |
title_full_unstemmed |
Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry |
title_sort |
past and future dynamics of the brunt ice shelf from seabed bathymetry and ice shelf geometry |
publisher |
Copernicus Publications |
series |
The Cryosphere |
issn |
1994-0416 1994-0424 |
publishDate |
2019-02-01 |
description |
<p>The recent rapid growth of rifts in the Brunt Ice Shelf appears to
signal the onset of its largest calving event since records began in 1915.
The aim of this study is to determine whether this calving event will lead to
a new steady state in which the Brunt Ice Shelf remains in contact with the bed,
or an unpinning from the bed, which could predispose it to accelerated flow
or possible break-up. We use a range of geophysical data to reconstruct the
sea-floor bathymetry and ice shelf geometry, to examine past ice sheet
configurations in the Brunt Basin, and to define the present-day geometry of
the contact between the Brunt Ice Shelf and the bed. Results show that during
past ice advances grounded ice streams likely converged in the Brunt Basin
from the south and east. As the ice retreated, it was likely pinned on at
least three former grounding lines marked by topographic highs, and
transverse ridges on the flanks of the basin. These may have subsequently
formed pinning points for developing ice shelves. The ice shelf geometry and
bathymetry measurements show that the base of the Brunt Ice Shelf now only
makes contact with one of these topographic highs. This contact is limited to
an area of less than 1.3 to 3 km<span class="inline-formula"><sup>2</sup></span> and results in a compressive regime
that helps to maintain the ice shelf's integrity. The maximum overlap between ice shelf
draft and the bathymetric high is 2–25 m and is contingent on the presence
of incorporated iceberg keels, which protrude beneath the base of the ice
shelf. The future of the ice shelf depends on whether the expected calving
event causes full or partial loss of contact with the bed and whether the
subsequent response causes re-grounding within a predictable period or a
loss of structural integrity resulting from properties inherited at the
grounding line.</p> |
url |
https://www.the-cryosphere.net/13/545/2019/tc-13-545-2019.pdf |
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