The ice front as a topographic barrier for ocean heat transport
Antarctic ice shelves are the link between the Southern Ocean and the Antarctic Ice Sheet. The floating ice shelves restrain the seaward flow of the grounded ice, which is balanced by iceberg calving and ocean-induced basal melting. An increase in oceanic heat flux towards the West Antarctic ice she...
Published in: | Nature |
---|---|
Main Author: | |
Other Authors: | |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
Published: |
The University of Bergen
2021
|
Subjects: | |
Online Access: | https://hdl.handle.net/11250/2760582 |
id |
ftunivbergen:oai:bora.uib.no:11250/2760582 |
---|---|
record_format |
openpolar |
spelling |
ftunivbergen:oai:bora.uib.no:11250/2760582 2023-05-15T14:13:27+02:00 The ice front as a topographic barrier for ocean heat transport Steiger, Nadine orcid:0000-0002-7533-6583 2021-06-07T13:29:24.188Z application/pdf https://hdl.handle.net/11250/2760582 eng eng The University of Bergen Paper I: Wåhlin, A.K., Steiger, N., Darelius, E., Assmann, K.M., Glessmer, M.S., Ha, H.K., Herraiz-Borreguero, L., Heuzé, C., Jenkins, A., Kim, T.W., Mazur, A.K., Sommeria, J., Viboud, S. (2020), Ice front blocking of ocean heat transport to an Antarctic ice shelf, Nature 578: 568–571. The article is not available in BORA due to publisher restrictions. The published version is available at: https://doi.org/10.1038/s41586-020-2014-5 Paper II: Steiger, N., Darelius, E., Wåhlin, A. K., Assmann, K. M. Intermittent reduction in ocean heat transport into the Getz Ice Shelf cavity during strong wind events. The article is not available in BORA. Paper III: Steiger, N., Darelius, E., Kimura, S., Patmore, R. D., Wåhlin, A. K. The dynamics of a barotropic current at an ice front. The article is not available in BORA. container/ae/9a/7a/f3/ae9a7af3-2663-4b6e-a7a6-882b2b189719 urn:isbn:9788230844588 urn:isbn:9788230857403 https://hdl.handle.net/11250/2760582 In copyright http://rightsstatements.org/page/InC/1.0/ Copyright the Author. All rights reserved Doctoral thesis 2021 ftunivbergen https://doi.org/10.1038/s41586-020-2014-5 2023-03-14T17:39:39Z Antarctic ice shelves are the link between the Southern Ocean and the Antarctic Ice Sheet. The floating ice shelves restrain the seaward flow of the grounded ice, which is balanced by iceberg calving and ocean-induced basal melting. An increase in oceanic heat flux towards the West Antarctic ice shelves during the last decades has caused the ice shelves to thin. Nevertheless, the observed melt rates are lower than expected from the oceanic heat available on the continental shelf, suggesting that not all the heat is used to melt the ice shelves. Ice shelves extend several hundred meters into the ocean and terminate with a vertical wall, the ice front, that poses a topographic barrier to the ocean heat transport towards the sub-ice shelf cavities. Little is known about the influence of the discontinuity in water column thickness on the southward currents that transport warm and dense Circumpolar Deep Water from north of the continental shelf towards the ice shelf cavities. This thesis improves our understanding of the ocean dynamics and the drivers of heat transport variability in the vicinity of the ice front, based on mooring observations in front of the Getz Ice Shelf in West Antarctica, laboratory experiments, and idealized numerical modelling. From the mooring observations, we infer in Paper I that only a small fraction of the southward heat transport eventually reaches the Getz Ice Shelf cavity, due to the different response of the barotropic (depth-constant) and the baroclinic (depth-varying) components of the current to the ice front. The barotropic component is blocked and deflected at the ice front; only the baroclinic, bottom-intensified component enters the ice shelf cavity. Results from laboratory experiments on a rotating platform support these observations. The experiments show that the barotropic current follows lines of constant water column thickness and turns at the ice front, while the baroclinic, dense current follows lines of constant bed topography and enters the cavity without being ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctica Getz Ice Shelf Ice Sheet Ice Shelf Ice Shelves Iceberg* Southern Ocean West Antarctica University of Bergen: Bergen Open Research Archive (BORA-UiB) Antarctic Getz ENVELOPE(-145.217,-145.217,-76.550,-76.550) Getz Ice Shelf ENVELOPE(-126.500,-126.500,-74.250,-74.250) Southern Ocean The Antarctic West Antarctica Nature 578 7796 568 571 |
institution |
Open Polar |
collection |
University of Bergen: Bergen Open Research Archive (BORA-UiB) |
op_collection_id |
ftunivbergen |
language |
English |
description |
Antarctic ice shelves are the link between the Southern Ocean and the Antarctic Ice Sheet. The floating ice shelves restrain the seaward flow of the grounded ice, which is balanced by iceberg calving and ocean-induced basal melting. An increase in oceanic heat flux towards the West Antarctic ice shelves during the last decades has caused the ice shelves to thin. Nevertheless, the observed melt rates are lower than expected from the oceanic heat available on the continental shelf, suggesting that not all the heat is used to melt the ice shelves. Ice shelves extend several hundred meters into the ocean and terminate with a vertical wall, the ice front, that poses a topographic barrier to the ocean heat transport towards the sub-ice shelf cavities. Little is known about the influence of the discontinuity in water column thickness on the southward currents that transport warm and dense Circumpolar Deep Water from north of the continental shelf towards the ice shelf cavities. This thesis improves our understanding of the ocean dynamics and the drivers of heat transport variability in the vicinity of the ice front, based on mooring observations in front of the Getz Ice Shelf in West Antarctica, laboratory experiments, and idealized numerical modelling. From the mooring observations, we infer in Paper I that only a small fraction of the southward heat transport eventually reaches the Getz Ice Shelf cavity, due to the different response of the barotropic (depth-constant) and the baroclinic (depth-varying) components of the current to the ice front. The barotropic component is blocked and deflected at the ice front; only the baroclinic, bottom-intensified component enters the ice shelf cavity. Results from laboratory experiments on a rotating platform support these observations. The experiments show that the barotropic current follows lines of constant water column thickness and turns at the ice front, while the baroclinic, dense current follows lines of constant bed topography and enters the cavity without being ... |
author2 |
orcid:0000-0002-7533-6583 |
format |
Doctoral or Postdoctoral Thesis |
author |
Steiger, Nadine |
spellingShingle |
Steiger, Nadine The ice front as a topographic barrier for ocean heat transport |
author_facet |
Steiger, Nadine |
author_sort |
Steiger, Nadine |
title |
The ice front as a topographic barrier for ocean heat transport |
title_short |
The ice front as a topographic barrier for ocean heat transport |
title_full |
The ice front as a topographic barrier for ocean heat transport |
title_fullStr |
The ice front as a topographic barrier for ocean heat transport |
title_full_unstemmed |
The ice front as a topographic barrier for ocean heat transport |
title_sort |
ice front as a topographic barrier for ocean heat transport |
publisher |
The University of Bergen |
publishDate |
2021 |
url |
https://hdl.handle.net/11250/2760582 |
long_lat |
ENVELOPE(-145.217,-145.217,-76.550,-76.550) ENVELOPE(-126.500,-126.500,-74.250,-74.250) |
geographic |
Antarctic Getz Getz Ice Shelf Southern Ocean The Antarctic West Antarctica |
geographic_facet |
Antarctic Getz Getz Ice Shelf Southern Ocean The Antarctic West Antarctica |
genre |
Antarc* Antarctic Antarctica Getz Ice Shelf Ice Sheet Ice Shelf Ice Shelves Iceberg* Southern Ocean West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Getz Ice Shelf Ice Sheet Ice Shelf Ice Shelves Iceberg* Southern Ocean West Antarctica |
op_relation |
Paper I: Wåhlin, A.K., Steiger, N., Darelius, E., Assmann, K.M., Glessmer, M.S., Ha, H.K., Herraiz-Borreguero, L., Heuzé, C., Jenkins, A., Kim, T.W., Mazur, A.K., Sommeria, J., Viboud, S. (2020), Ice front blocking of ocean heat transport to an Antarctic ice shelf, Nature 578: 568–571. The article is not available in BORA due to publisher restrictions. The published version is available at: https://doi.org/10.1038/s41586-020-2014-5 Paper II: Steiger, N., Darelius, E., Wåhlin, A. K., Assmann, K. M. Intermittent reduction in ocean heat transport into the Getz Ice Shelf cavity during strong wind events. The article is not available in BORA. Paper III: Steiger, N., Darelius, E., Kimura, S., Patmore, R. D., Wåhlin, A. K. The dynamics of a barotropic current at an ice front. The article is not available in BORA. container/ae/9a/7a/f3/ae9a7af3-2663-4b6e-a7a6-882b2b189719 urn:isbn:9788230844588 urn:isbn:9788230857403 https://hdl.handle.net/11250/2760582 |
op_rights |
In copyright http://rightsstatements.org/page/InC/1.0/ Copyright the Author. All rights reserved |
op_doi |
https://doi.org/10.1038/s41586-020-2014-5 |
container_title |
Nature |
container_volume |
578 |
container_issue |
7796 |
container_start_page |
568 |
op_container_end_page |
571 |
_version_ |
1766285920550518784 |