Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3
The transient response of the Atlantic Meridional Overturning Circulation (AMOC) to a deglacial ice-sheet retreat is studied using the Community Climate System Model version 3 (CCSM3), with a focus on orographic effects rather than meltwater discharge. It is found that the AMOC weakens significantly...
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ftawi:oai:epic.awi.de:36169 2023-05-15T16:40:09+02:00 Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 Zhu, Jiang Liu, Zhengyu Zhang, Xu Eisenman, Ian Liu, Wei 2014-09-16 application/pdf https://epic.awi.de/id/eprint/36169/ https://epic.awi.de/id/eprint/36169/1/2014gl060891.pdf http://onlinelibrary.wiley.com/enhanced/doi/10.1002/2014GL060891/ https://hdl.handle.net/10013/epic.44204 https://hdl.handle.net/10013/epic.44204.d001 unknown Wiley https://epic.awi.de/id/eprint/36169/1/2014gl060891.pdf https://hdl.handle.net/10013/epic.44204.d001 Zhu, J. , Liu, Z. , Zhang, X. orcid:0000-0003-1833-9689 , Eisenman, I. and Liu, W. (2014) Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 , Geophysical Research Letters, 41 (17), pp. 6252-6258 . doi:10.1002/2014GL060891 <https://doi.org/10.1002/2014GL060891> , hdl:10013/epic.44204 EPIC3Geophysical Research Letters, Wiley, 41(17), pp. 6252-6258, ISSN: 0094-8276 Article peerRev 2014 ftawi https://doi.org/10.1002/2014GL060891 2021-12-24T15:39:46Z The transient response of the Atlantic Meridional Overturning Circulation (AMOC) to a deglacial ice-sheet retreat is studied using the Community Climate System Model version 3 (CCSM3), with a focus on orographic effects rather than meltwater discharge. It is found that the AMOC weakens significantly (41%) in response to the deglacial ice-sheet retreat. The AMOC weakening follows the decrease of the Northern Hemisphere ice-sheet volume linearly, with no evidence of abrupt thresholds. A wind-driven mechanism is proposed to explain the weakening of the AMOC: lowering the Northern Hemisphere ice sheets induces a northward shift of the westerlies, which causes a rapid eastward sea-ice transport and expanded sea-ice cover over the subpolar North Atlantic; this expanded sea ice insulates the ocean from heat loss and leads to suppressed deep convection and a weakened AMOC. A sea ice-ocean positive feedback could be further established between the AMOC decrease and sea-ice expansion. Article in Journal/Newspaper Ice Sheet North Atlantic Sea ice Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Geophysical Research Letters 41 17 6252 6258 |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
The transient response of the Atlantic Meridional Overturning Circulation (AMOC) to a deglacial ice-sheet retreat is studied using the Community Climate System Model version 3 (CCSM3), with a focus on orographic effects rather than meltwater discharge. It is found that the AMOC weakens significantly (41%) in response to the deglacial ice-sheet retreat. The AMOC weakening follows the decrease of the Northern Hemisphere ice-sheet volume linearly, with no evidence of abrupt thresholds. A wind-driven mechanism is proposed to explain the weakening of the AMOC: lowering the Northern Hemisphere ice sheets induces a northward shift of the westerlies, which causes a rapid eastward sea-ice transport and expanded sea-ice cover over the subpolar North Atlantic; this expanded sea ice insulates the ocean from heat loss and leads to suppressed deep convection and a weakened AMOC. A sea ice-ocean positive feedback could be further established between the AMOC decrease and sea-ice expansion. |
format |
Article in Journal/Newspaper |
author |
Zhu, Jiang Liu, Zhengyu Zhang, Xu Eisenman, Ian Liu, Wei |
spellingShingle |
Zhu, Jiang Liu, Zhengyu Zhang, Xu Eisenman, Ian Liu, Wei Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 |
author_facet |
Zhu, Jiang Liu, Zhengyu Zhang, Xu Eisenman, Ian Liu, Wei |
author_sort |
Zhu, Jiang |
title |
Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 |
title_short |
Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 |
title_full |
Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 |
title_fullStr |
Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 |
title_full_unstemmed |
Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 |
title_sort |
linear weakening of the amoc in response to receding glacial ice sheets in ccsm3 |
publisher |
Wiley |
publishDate |
2014 |
url |
https://epic.awi.de/id/eprint/36169/ https://epic.awi.de/id/eprint/36169/1/2014gl060891.pdf http://onlinelibrary.wiley.com/enhanced/doi/10.1002/2014GL060891/ https://hdl.handle.net/10013/epic.44204 https://hdl.handle.net/10013/epic.44204.d001 |
genre |
Ice Sheet North Atlantic Sea ice |
genre_facet |
Ice Sheet North Atlantic Sea ice |
op_source |
EPIC3Geophysical Research Letters, Wiley, 41(17), pp. 6252-6258, ISSN: 0094-8276 |
op_relation |
https://epic.awi.de/id/eprint/36169/1/2014gl060891.pdf https://hdl.handle.net/10013/epic.44204.d001 Zhu, J. , Liu, Z. , Zhang, X. orcid:0000-0003-1833-9689 , Eisenman, I. and Liu, W. (2014) Linear Weakening of the AMOC in response to Receding Glacial Ice Sheets in CCSM3 , Geophysical Research Letters, 41 (17), pp. 6252-6258 . doi:10.1002/2014GL060891 <https://doi.org/10.1002/2014GL060891> , hdl:10013/epic.44204 |
op_doi |
https://doi.org/10.1002/2014GL060891 |
container_title |
Geophysical Research Letters |
container_volume |
41 |
container_issue |
17 |
container_start_page |
6252 |
op_container_end_page |
6258 |
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1766030532248862720 |