Dynamic Antarctic ice sheet during the early to mid-Miocene
Geological data indicate that there were major variations in Antarctic ice sheet volume and extent during the early to mid-Miocene. Simulating such large-scale changes is problematic because of a strong hysteresis effect, which results in stability once the ice sheets have reached continental size....
Published in: | Proceedings of the National Academy of Sciences |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2016
|
Subjects: | |
Online Access: | https://hdl.handle.net/1983/898df9bb-9315-4ebf-aa23-f761e0a93c1b https://research-information.bris.ac.uk/en/publications/898df9bb-9315-4ebf-aa23-f761e0a93c1b https://doi.org/10.1073/pnas.1516130113 http://www.scopus.com/inward/record.url?scp=84962183165&partnerID=8YFLogxK |
id |
ftubristolcris:oai:research-information.bris.ac.uk:publications/898df9bb-9315-4ebf-aa23-f761e0a93c1b |
---|---|
record_format |
openpolar |
spelling |
ftubristolcris:oai:research-information.bris.ac.uk:publications/898df9bb-9315-4ebf-aa23-f761e0a93c1b 2024-05-19T07:32:29+00:00 Dynamic Antarctic ice sheet during the early to mid-Miocene Gasson, Edward DeConto, Robert M. Pollard, David Levy, Richard H. 2016-03-29 https://hdl.handle.net/1983/898df9bb-9315-4ebf-aa23-f761e0a93c1b https://research-information.bris.ac.uk/en/publications/898df9bb-9315-4ebf-aa23-f761e0a93c1b https://doi.org/10.1073/pnas.1516130113 http://www.scopus.com/inward/record.url?scp=84962183165&partnerID=8YFLogxK eng eng https://research-information.bris.ac.uk/en/publications/898df9bb-9315-4ebf-aa23-f761e0a93c1b info:eu-repo/semantics/restrictedAccess Gasson , E , DeConto , R M , Pollard , D & Levy , R H 2016 , ' Dynamic Antarctic ice sheet during the early to mid-Miocene ' , Proceedings of the National Academy of Sciences of the United States of America , vol. 113 , no. 13 , pp. 3459-3464 . https://doi.org/10.1073/pnas.1516130113 Antarctic ice sheet Miocene Oxygen isotopes Sea level article 2016 ftubristolcris https://doi.org/10.1073/pnas.1516130113 2024-04-30T23:47:03Z Geological data indicate that there were major variations in Antarctic ice sheet volume and extent during the early to mid-Miocene. Simulating such large-scale changes is problematic because of a strong hysteresis effect, which results in stability once the ice sheets have reached continental size. A relatively narrow range of atmospheric CO 2 concentrations indicated by proxy records exacerbates this problem. Here, we are able to simulate large-scale variability of the early to mid-Miocene Antarctic ice sheet because of three developments in our modeling approach. (i) We use a climate-ice sheet coupling method utilizing a high-resolution atmospheric component to account for ice sheet-climate feedbacks. (ii) The ice sheet model includes recently proposed mechanisms for retreat into deep subglacial basins caused by ice-cliff failure and ice-shelf hydrofracture. (iii)We account for changes in the oxygen isotopic composition of the ice sheet by using isotope-enabled climate and ice sheet models. We compare our modeling results with ice-proximal records emerging from a sedimentological drill core from the Ross Sea (Andrill-2A) that is presented in a companion article. The variability in Antarctic ice volume that we simulate is equivalent to a seawater oxygen isotope signal of 0.52-0.66‰, or a sea level equivalent change of 30-36 m, for a range of atmospheric CO 2 between 280 and 500 ppm and a changing astronomical configuration. This result represents a substantial advance in resolving the long-standing model data conflict of Miocene Antarctic ice sheet and sea level variability. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Ross Sea University of Bristol: Bristol Research Proceedings of the National Academy of Sciences 113 13 3459 3464 |
institution |
Open Polar |
collection |
University of Bristol: Bristol Research |
op_collection_id |
ftubristolcris |
language |
English |
topic |
Antarctic ice sheet Miocene Oxygen isotopes Sea level |
spellingShingle |
Antarctic ice sheet Miocene Oxygen isotopes Sea level Gasson, Edward DeConto, Robert M. Pollard, David Levy, Richard H. Dynamic Antarctic ice sheet during the early to mid-Miocene |
topic_facet |
Antarctic ice sheet Miocene Oxygen isotopes Sea level |
description |
Geological data indicate that there were major variations in Antarctic ice sheet volume and extent during the early to mid-Miocene. Simulating such large-scale changes is problematic because of a strong hysteresis effect, which results in stability once the ice sheets have reached continental size. A relatively narrow range of atmospheric CO 2 concentrations indicated by proxy records exacerbates this problem. Here, we are able to simulate large-scale variability of the early to mid-Miocene Antarctic ice sheet because of three developments in our modeling approach. (i) We use a climate-ice sheet coupling method utilizing a high-resolution atmospheric component to account for ice sheet-climate feedbacks. (ii) The ice sheet model includes recently proposed mechanisms for retreat into deep subglacial basins caused by ice-cliff failure and ice-shelf hydrofracture. (iii)We account for changes in the oxygen isotopic composition of the ice sheet by using isotope-enabled climate and ice sheet models. We compare our modeling results with ice-proximal records emerging from a sedimentological drill core from the Ross Sea (Andrill-2A) that is presented in a companion article. The variability in Antarctic ice volume that we simulate is equivalent to a seawater oxygen isotope signal of 0.52-0.66‰, or a sea level equivalent change of 30-36 m, for a range of atmospheric CO 2 between 280 and 500 ppm and a changing astronomical configuration. This result represents a substantial advance in resolving the long-standing model data conflict of Miocene Antarctic ice sheet and sea level variability. |
format |
Article in Journal/Newspaper |
author |
Gasson, Edward DeConto, Robert M. Pollard, David Levy, Richard H. |
author_facet |
Gasson, Edward DeConto, Robert M. Pollard, David Levy, Richard H. |
author_sort |
Gasson, Edward |
title |
Dynamic Antarctic ice sheet during the early to mid-Miocene |
title_short |
Dynamic Antarctic ice sheet during the early to mid-Miocene |
title_full |
Dynamic Antarctic ice sheet during the early to mid-Miocene |
title_fullStr |
Dynamic Antarctic ice sheet during the early to mid-Miocene |
title_full_unstemmed |
Dynamic Antarctic ice sheet during the early to mid-Miocene |
title_sort |
dynamic antarctic ice sheet during the early to mid-miocene |
publishDate |
2016 |
url |
https://hdl.handle.net/1983/898df9bb-9315-4ebf-aa23-f761e0a93c1b https://research-information.bris.ac.uk/en/publications/898df9bb-9315-4ebf-aa23-f761e0a93c1b https://doi.org/10.1073/pnas.1516130113 http://www.scopus.com/inward/record.url?scp=84962183165&partnerID=8YFLogxK |
genre |
Antarc* Antarctic Ice Sheet Ice Shelf Ross Sea |
genre_facet |
Antarc* Antarctic Ice Sheet Ice Shelf Ross Sea |
op_source |
Gasson , E , DeConto , R M , Pollard , D & Levy , R H 2016 , ' Dynamic Antarctic ice sheet during the early to mid-Miocene ' , Proceedings of the National Academy of Sciences of the United States of America , vol. 113 , no. 13 , pp. 3459-3464 . https://doi.org/10.1073/pnas.1516130113 |
op_relation |
https://research-information.bris.ac.uk/en/publications/898df9bb-9315-4ebf-aa23-f761e0a93c1b |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1073/pnas.1516130113 |
container_title |
Proceedings of the National Academy of Sciences |
container_volume |
113 |
container_issue |
13 |
container_start_page |
3459 |
op_container_end_page |
3464 |
_version_ |
1799470538826973184 |