The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation
Highâ€latitude Northern Hemisphere climate during the last glacial period was characterized by a series of abrupt climate changes, known as Dansgaardâ€Oeschger (DO) events, which were recorded in Greenland ice cores as shifts in the oxygen isotopic composition of the ice. These shifts in inferred No...
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ftcaltechauth:oai:authors.library.caltech.edu:z4mhv-sdc58 2024-09-15T18:10:08+00:00 The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation Hines, Sophia K. V. Thompson, Andrew F. Adkins, Jess F. 2019-04 https://doi.org/10.1029/2018pa003415 unknown American Geophysical Union https://github.com/shiness11/DynBoxTwoB4L https://doi.org/10.1029/2018pa003415 oai:authors.library.caltech.edu:z4mhv-sdc58 eprintid:94246 resolverid:CaltechAUTHORS:20190328-112956704 info:eu-repo/semantics/openAccess Other Paleoceanography and Paleoclimatology, 34(4), 490-510, (2019-04) Abrupt climate change Glacial ocean circulation Ocean circulation Hysteresis info:eu-repo/semantics/article 2019 ftcaltechauth https://doi.org/10.1029/2018pa003415 2024-08-06T15:35:03Z Highâ€latitude Northern Hemisphere climate during the last glacial period was characterized by a series of abrupt climate changes, known as Dansgaardâ€Oeschger (DO) events, which were recorded in Greenland ice cores as shifts in the oxygen isotopic composition of the ice. These shifts in inferred Northern Hemisphere highâ€latitude temperature have been linked to changes in Atlantic meridional overturning strength. The response of ocean overturning circulation to forcing is nonâ€linear and a hierarchy of models have suggested that it may exist in multiple steady state configurations. Here, we use a timeâ€dependent coarseâ€resolution isopycnal model with four density classes and two basins, linked by a Southern Ocean to explore overturning states and their stability to changes in external parameters. The model exhibits hysteresis in both the steadyâ€state stratification and overturning strength as a function of the magnitude of North Atlantic Deep Water (NADW) formation. Hysteresis occurs as a result of two nonâ€linearities in the modelâ€â€â€the surface buoyancy distribution in the Southern Ocean and the vertical diffusivity profile in the Atlantic and Indoâ€Pacific basins. We construct a metric to assess circulation configuration in the model, motivated by observations from the Last Glacial Maximum, which show a different circulation structure from the modern. We find that circulation configuration is primarily determined by NADW density. The model results are used to suggest how ocean conditions may have influenced the pattern of DO events across the last glacial cycle. © 2019 American Geophysical Union. Received 6 JUN 2018; Accepted 4MAR 2019; Accepted article online 15MAR 2019; Published online 5 APR 2019. We would like to thank Raffaele Ferrari, Emily Newsom, Andrew Stewart, David Marshall, James Rae, and Andrea Burke for helpful discussions, and two anonymous reviewers, whose comments improved the manuscript. S. K. V. H. received support from NSF grants OCEâ€1503129 and OCEâ€1204211 and the ... Article in Journal/Newspaper Greenland Greenland ice cores NADW North Atlantic Deep Water North Atlantic Southern Ocean Caltech Authors (California Institute of Technology) Paleoceanography and Paleoclimatology 34 4 490 510 |
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Open Polar |
collection |
Caltech Authors (California Institute of Technology) |
op_collection_id |
ftcaltechauth |
language |
unknown |
topic |
Abrupt climate change Glacial ocean circulation Ocean circulation Hysteresis |
spellingShingle |
Abrupt climate change Glacial ocean circulation Ocean circulation Hysteresis Hines, Sophia K. V. Thompson, Andrew F. Adkins, Jess F. The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation |
topic_facet |
Abrupt climate change Glacial ocean circulation Ocean circulation Hysteresis |
description |
Highâ€latitude Northern Hemisphere climate during the last glacial period was characterized by a series of abrupt climate changes, known as Dansgaardâ€Oeschger (DO) events, which were recorded in Greenland ice cores as shifts in the oxygen isotopic composition of the ice. These shifts in inferred Northern Hemisphere highâ€latitude temperature have been linked to changes in Atlantic meridional overturning strength. The response of ocean overturning circulation to forcing is nonâ€linear and a hierarchy of models have suggested that it may exist in multiple steady state configurations. Here, we use a timeâ€dependent coarseâ€resolution isopycnal model with four density classes and two basins, linked by a Southern Ocean to explore overturning states and their stability to changes in external parameters. The model exhibits hysteresis in both the steadyâ€state stratification and overturning strength as a function of the magnitude of North Atlantic Deep Water (NADW) formation. Hysteresis occurs as a result of two nonâ€linearities in the modelâ€â€â€the surface buoyancy distribution in the Southern Ocean and the vertical diffusivity profile in the Atlantic and Indoâ€Pacific basins. We construct a metric to assess circulation configuration in the model, motivated by observations from the Last Glacial Maximum, which show a different circulation structure from the modern. We find that circulation configuration is primarily determined by NADW density. The model results are used to suggest how ocean conditions may have influenced the pattern of DO events across the last glacial cycle. © 2019 American Geophysical Union. Received 6 JUN 2018; Accepted 4MAR 2019; Accepted article online 15MAR 2019; Published online 5 APR 2019. We would like to thank Raffaele Ferrari, Emily Newsom, Andrew Stewart, David Marshall, James Rae, and Andrea Burke for helpful discussions, and two anonymous reviewers, whose comments improved the manuscript. S. K. V. H. received support from NSF grants OCEâ€1503129 and OCEâ€1204211 and the ... |
format |
Article in Journal/Newspaper |
author |
Hines, Sophia K. V. Thompson, Andrew F. Adkins, Jess F. |
author_facet |
Hines, Sophia K. V. Thompson, Andrew F. Adkins, Jess F. |
author_sort |
Hines, Sophia K. V. |
title |
The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation |
title_short |
The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation |
title_full |
The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation |
title_fullStr |
The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation |
title_full_unstemmed |
The role of the Southern Ocean in abrupt transitions and hysteresis in glacial ocean circulation |
title_sort |
role of the southern ocean in abrupt transitions and hysteresis in glacial ocean circulation |
publisher |
American Geophysical Union |
publishDate |
2019 |
url |
https://doi.org/10.1029/2018pa003415 |
genre |
Greenland Greenland ice cores NADW North Atlantic Deep Water North Atlantic Southern Ocean |
genre_facet |
Greenland Greenland ice cores NADW North Atlantic Deep Water North Atlantic Southern Ocean |
op_source |
Paleoceanography and Paleoclimatology, 34(4), 490-510, (2019-04) |
op_relation |
https://github.com/shiness11/DynBoxTwoB4L https://doi.org/10.1029/2018pa003415 oai:authors.library.caltech.edu:z4mhv-sdc58 eprintid:94246 resolverid:CaltechAUTHORS:20190328-112956704 |
op_rights |
info:eu-repo/semantics/openAccess Other |
op_doi |
https://doi.org/10.1029/2018pa003415 |
container_title |
Paleoceanography and Paleoclimatology |
container_volume |
34 |
container_issue |
4 |
container_start_page |
490 |
op_container_end_page |
510 |
_version_ |
1810447741208231936 |