Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data
Ice shelves around Antarctica can provide back stress for outlet glaciers and control ice sheet mass loss. They often contain narrow bands of thin ice termed ice shelf channels. Ice shelf channel morphology can be interpreted through surface depressions and exhibits junctions and deflections from fl...
Published in: | Journal of Geophysical Research: Earth Surface |
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ftsubggeo:oai:e-docs.geo-leo.de:11858/8495 2024-06-09T07:39:40+00:00 Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data Drews, R. Schannwell, C. Ehlers, T. A. Gladstone, R. Pattyn, F. Matsuoka, K. 1 Department of Geoscience University of Tübingen Tübingen Germany 2 Arctic Centre University of Lapland Rovaniemi Finland 3 Laboratoire de Glaciologie Université Libre de Bruxelles Brussels Belgium 4 Norwegian Polar Institute Tromsø Norway 2020-07-09 https://doi.org/10.1029/2020JF005587 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8495 eng eng doi:10.1029/2020JF005587 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8495 This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. ddc:551 glaciology geophysics Antarctica ice shelves ice‐ocean interaction ice shelf channels doc-type:article 2020 ftsubggeo https://doi.org/10.1029/2020JF005587 2024-05-10T04:58:51Z Ice shelves around Antarctica can provide back stress for outlet glaciers and control ice sheet mass loss. They often contain narrow bands of thin ice termed ice shelf channels. Ice shelf channel morphology can be interpreted through surface depressions and exhibits junctions and deflections from flowlines. Using ice flow modeling and radar, we investigate ice shelf channels in the Roi Baudouin Ice Shelf. These are aligned obliquely to the prevailing easterly winds. In the shallow radar stratigraphy, syncline and anticline stacks occur beneath the upwind and downwind side, respectively. The structures are horizontally and vertically coherent, except near an ice shelf channel junction where patterns change structurally with depth. Deeper layers truncate near basal incisions. Using ice flow modeling, we show that the stratigraphy is ∼9 times more sensitive to atmospheric variability than to oceanic variability. This is due to the continual adjustment toward flotation. We propose that syncline‐anticline pairs in the shallow stratigraphy are caused by preferential snow deposition on the windward side and wind erosion at the downwind side. This drives downwind deflection of ice shelf channels of several meters per year. The depth variable structures indicate formation of an ice shelf channel junction by basal melting. We conclude that many ice shelf channels are seeded at the grounding line. Their morphology farther seaward is shaped on different length scales by ice dynamics, the ocean, and the atmosphere. These processes act on finer (subkilometer) scales than are captured by most ice, atmosphere, and ocean models, yet the dynamics of ice shelf channels may have broader implications for ice shelf stability. Plain Language Summary Ice flows from Antarctica's interior toward the coast. At the contact point between ice and ocean, the ice becomes afloat and forms fast‐flowing ice shelves. Snowfall continuously accumulates at the ice shelf surface, and at the ice shelf bottom the relatively warm ocean water can melt ... Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves GEO-LEOe-docs (FID GEO) Contact Point ENVELOPE(-56.997,-56.997,-63.374,-63.374) East Antarctica Roi Baudouin ENVELOPE(24.461,24.461,-70.438,-70.438) Journal of Geophysical Research: Earth Surface 125 7 |
institution |
Open Polar |
collection |
GEO-LEOe-docs (FID GEO) |
op_collection_id |
ftsubggeo |
language |
English |
topic |
ddc:551 glaciology geophysics Antarctica ice shelves ice‐ocean interaction ice shelf channels |
spellingShingle |
ddc:551 glaciology geophysics Antarctica ice shelves ice‐ocean interaction ice shelf channels Drews, R. Schannwell, C. Ehlers, T. A. Gladstone, R. Pattyn, F. Matsuoka, K. 1 Department of Geoscience University of Tübingen Tübingen Germany 2 Arctic Centre University of Lapland Rovaniemi Finland 3 Laboratoire de Glaciologie Université Libre de Bruxelles Brussels Belgium 4 Norwegian Polar Institute Tromsø Norway Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data |
topic_facet |
ddc:551 glaciology geophysics Antarctica ice shelves ice‐ocean interaction ice shelf channels |
description |
Ice shelves around Antarctica can provide back stress for outlet glaciers and control ice sheet mass loss. They often contain narrow bands of thin ice termed ice shelf channels. Ice shelf channel morphology can be interpreted through surface depressions and exhibits junctions and deflections from flowlines. Using ice flow modeling and radar, we investigate ice shelf channels in the Roi Baudouin Ice Shelf. These are aligned obliquely to the prevailing easterly winds. In the shallow radar stratigraphy, syncline and anticline stacks occur beneath the upwind and downwind side, respectively. The structures are horizontally and vertically coherent, except near an ice shelf channel junction where patterns change structurally with depth. Deeper layers truncate near basal incisions. Using ice flow modeling, we show that the stratigraphy is ∼9 times more sensitive to atmospheric variability than to oceanic variability. This is due to the continual adjustment toward flotation. We propose that syncline‐anticline pairs in the shallow stratigraphy are caused by preferential snow deposition on the windward side and wind erosion at the downwind side. This drives downwind deflection of ice shelf channels of several meters per year. The depth variable structures indicate formation of an ice shelf channel junction by basal melting. We conclude that many ice shelf channels are seeded at the grounding line. Their morphology farther seaward is shaped on different length scales by ice dynamics, the ocean, and the atmosphere. These processes act on finer (subkilometer) scales than are captured by most ice, atmosphere, and ocean models, yet the dynamics of ice shelf channels may have broader implications for ice shelf stability. Plain Language Summary Ice flows from Antarctica's interior toward the coast. At the contact point between ice and ocean, the ice becomes afloat and forms fast‐flowing ice shelves. Snowfall continuously accumulates at the ice shelf surface, and at the ice shelf bottom the relatively warm ocean water can melt ... |
format |
Article in Journal/Newspaper |
author |
Drews, R. Schannwell, C. Ehlers, T. A. Gladstone, R. Pattyn, F. Matsuoka, K. 1 Department of Geoscience University of Tübingen Tübingen Germany 2 Arctic Centre University of Lapland Rovaniemi Finland 3 Laboratoire de Glaciologie Université Libre de Bruxelles Brussels Belgium 4 Norwegian Polar Institute Tromsø Norway |
author_facet |
Drews, R. Schannwell, C. Ehlers, T. A. Gladstone, R. Pattyn, F. Matsuoka, K. 1 Department of Geoscience University of Tübingen Tübingen Germany 2 Arctic Centre University of Lapland Rovaniemi Finland 3 Laboratoire de Glaciologie Université Libre de Bruxelles Brussels Belgium 4 Norwegian Polar Institute Tromsø Norway |
author_sort |
Drews, R. |
title |
Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data |
title_short |
Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data |
title_full |
Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data |
title_fullStr |
Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data |
title_full_unstemmed |
Atmospheric and Oceanographic Signatures in the Ice Shelf Channel Morphology of Roi Baudouin Ice Shelf, East Antarctica, Inferred From Radar Data |
title_sort |
atmospheric and oceanographic signatures in the ice shelf channel morphology of roi baudouin ice shelf, east antarctica, inferred from radar data |
publishDate |
2020 |
url |
https://doi.org/10.1029/2020JF005587 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8495 |
long_lat |
ENVELOPE(-56.997,-56.997,-63.374,-63.374) ENVELOPE(24.461,24.461,-70.438,-70.438) |
geographic |
Contact Point East Antarctica Roi Baudouin |
geographic_facet |
Contact Point East Antarctica Roi Baudouin |
genre |
Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctica East Antarctica Ice Sheet Ice Shelf Ice Shelves |
op_relation |
doi:10.1029/2020JF005587 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8495 |
op_rights |
This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. |
op_doi |
https://doi.org/10.1029/2020JF005587 |
container_title |
Journal of Geophysical Research: Earth Surface |
container_volume |
125 |
container_issue |
7 |
_version_ |
1801381078448996352 |