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Seasonality of warm water intrusions onto the continental shelf near the Totten glacier

Seasonality of warm water intrusions onto the continental shelf near the Totten glacier
Seasonality of warm water intrusions onto the continental shelf near the Totten glacier
Warm Modified Circumpolar Deep Water (MCDW) from the Southern Ocean drives rapid basal melt of the Totten Ice Shelf on the Sabrina Coast (East Antarctica), affecting the mass balance of the grounded Totten Glacier. Recent observations show that MCDW intrudes onto the continental shelf through a depression at the shelf break. Here we investigate such intrusions by combining (1) new oceanographic and bathymetric observations collected for two consecutive years by profiling floats in the depression south of the shelf break, (2) oceanographic measurements collected by conductivity-temperature-depth-instrumented seals on continental slope, and (3) an ocean model. The depression provides a pathway for persistent inflow of warm (0-1°C) MCDW to the inner shelf. In austral autumn and early winter MCDW intrusions were up to 0.5°C warmer and were ~75 m thicker than in spring and summer. The seasonality of the flow on the continental slope explains the seasonality of the intrusions. The MCDW layer on the continental slope is warmer and thicker to the east of the depression than to the west. In autumn and early winter a strong, top-to-bottom westward current (Antarctic Slope Current) transports the warmer and thicker MCDW layer along the slope and is diverted poleward at the eastern entrance of the depression. A bottom-intensified eastward current (Antarctic Slope Undercurrent) develops in other months, allowing cooler and thinner intrusions to enter the depression from the west. Our study illustrates how circulation on the Antarctic slope regulates the ocean heat delivery to the continental shelf and ultimately to the ice shelves.
2169-9275
4272-4289
Silvano, Alessandro
54a4322b-c52d-4179-a414-dc108c416ec9
Rintoul, Stephen R.
ff078a21-d6cd-45bf-8c8f-f81f2e8ae410
Kusahara, Kazuya
dc47d937-3647-4dca-9088-14d094a41f9b
Peña‐Molino, Beatriz
6c1c2b33-8b10-42bc-b9ff-aab760ace79d
Wijk, Esmee
a22d3dc2-b17a-4cad-8073-d78b37eef00d
Gwyther, David E.
ede5ab85-e944-4e09-97a0-40bb08f2e1ae
Williams, Guy D.
0a237221-85c5-48b9-b4ca-a06a3b5074e5
Silvano, Alessandro
54a4322b-c52d-4179-a414-dc108c416ec9
Rintoul, Stephen R.
ff078a21-d6cd-45bf-8c8f-f81f2e8ae410
Kusahara, Kazuya
dc47d937-3647-4dca-9088-14d094a41f9b
Peña‐Molino, Beatriz
6c1c2b33-8b10-42bc-b9ff-aab760ace79d
Wijk, Esmee
a22d3dc2-b17a-4cad-8073-d78b37eef00d
Gwyther, David E.
ede5ab85-e944-4e09-97a0-40bb08f2e1ae
Williams, Guy D.
0a237221-85c5-48b9-b4ca-a06a3b5074e5

Silvano, Alessandro, Rintoul, Stephen R., Kusahara, Kazuya, Peña‐Molino, Beatriz, Wijk, Esmee, Gwyther, David E. and Williams, Guy D. (2019) Seasonality of warm water intrusions onto the continental shelf near the Totten glacier. Journal of Geophysical Research: Oceans, 124 (6), 4272-4289. (doi:10.1029/2018JC014634).

Record type: Article

Abstract

Warm Modified Circumpolar Deep Water (MCDW) from the Southern Ocean drives rapid basal melt of the Totten Ice Shelf on the Sabrina Coast (East Antarctica), affecting the mass balance of the grounded Totten Glacier. Recent observations show that MCDW intrudes onto the continental shelf through a depression at the shelf break. Here we investigate such intrusions by combining (1) new oceanographic and bathymetric observations collected for two consecutive years by profiling floats in the depression south of the shelf break, (2) oceanographic measurements collected by conductivity-temperature-depth-instrumented seals on continental slope, and (3) an ocean model. The depression provides a pathway for persistent inflow of warm (0-1°C) MCDW to the inner shelf. In austral autumn and early winter MCDW intrusions were up to 0.5°C warmer and were ~75 m thicker than in spring and summer. The seasonality of the flow on the continental slope explains the seasonality of the intrusions. The MCDW layer on the continental slope is warmer and thicker to the east of the depression than to the west. In autumn and early winter a strong, top-to-bottom westward current (Antarctic Slope Current) transports the warmer and thicker MCDW layer along the slope and is diverted poleward at the eastern entrance of the depression. A bottom-intensified eastward current (Antarctic Slope Undercurrent) develops in other months, allowing cooler and thinner intrusions to enter the depression from the west. Our study illustrates how circulation on the Antarctic slope regulates the ocean heat delivery to the continental shelf and ultimately to the ice shelves.

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More information

Accepted/In Press date: 29 April 2019
Published date: 3 June 2019
Additional Information: ©2019. American Geophysical Union. All Rights Reserved.

Identifiers

Local EPrints ID: 469725
URI: http://eprints.soton.ac.uk/id/eprint/469725
ISSN: 2169-9275
PURE UUID: 9f40fe06-b0e6-4582-9d59-e7a09286fef8
ORCID for Alessandro Silvano: ORCID iD orcid.org/0000-0002-6441-1496

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Date deposited: 23 Sep 2022 16:32
Last modified: 17 Mar 2024 03:59

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Contributors

Author: Stephen R. Rintoul
Author: Kazuya Kusahara
Author: Beatriz Peña‐Molino
Author: Esmee Wijk
Author: David E. Gwyther
Author: Guy D. Williams

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