Role of the Bering Strait on the hysteresis of the ocean conveyor belt circulation and glacial climate stability
Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80–11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets we...
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| Published in | Proceedings of the National Academy of Sciences - PNAS Vol. 109; no. 17; pp. 6417 - 6422 |
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| Main Authors | , , , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
United States
National Academy of Sciences
24.04.2012
National Acad Sciences |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80–11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets were still forming. Here we show, with a fully coupled state-of-the-art climate model, that closing the Bering Strait and preventing its throughflow between the Pacific and Arctic Oceans during the glacial period can lead to the emergence of stronger hysteresis behavior of the ocean conveyor belt circulation to create conditions that are conducive to triggering abrupt climate transitions. Hence, it is argued that even for greenhouse warming, abrupt climate transitions similar to those in the last glacial time are unlikely to occur as the Bering Strait remains open. |
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| AbstractList | Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80–11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets were still forming. Here we show, with a fully coupled state-of-the-art climate model, that closing the Bering Strait and preventing its throughflow between the Pacific and Arctic Oceans during the glacial period can lead to the emergence of stronger hysteresis behavior of the ocean conveyor belt circulation to create conditions that are conducive to triggering abrupt climate transitions. Hence, it is argued that even for greenhouse warming, abrupt climate transitions similar to those in the last glacial time are unlikely to occur as the Bering Strait remains open. Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80-11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets were still forming. Here we show, with a fully coupled state-of-the-art climate model, that closing the Bering Strait and preventing its throughflow between the Pacific and Arctic Oceans during the glacial period can lead to the emergence of stronger hysteresis behavior of the ocean conveyor belt circulation to create conditions that are conducive to triggering abrupt climate transitions. Hence, it is argued that even for greenhouse warming, abrupt climate transitions similar to those in the last glacial time are unlikely to occur as the Bering Strait remains open. [PUBLICATION ABSTRACT] Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80-11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets were still forming. Here we show, with a fully coupled state-of-the-art climate model, that closing the Bering Strait and preventing its throughflow between the Pacific and Arctic Oceans during the glacial period can lead to the emergence of stronger hysteresis behavior of the ocean conveyor belt circulation to create conditions that are conducive to triggering abrupt climate transitions. Hence, it is argued that even for greenhouse warming, abrupt climate transitions similar to those in the last glacial time are unlikely to occur as the Bering Strait remains open.Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80-11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets were still forming. Here we show, with a fully coupled state-of-the-art climate model, that closing the Bering Strait and preventing its throughflow between the Pacific and Arctic Oceans during the glacial period can lead to the emergence of stronger hysteresis behavior of the ocean conveyor belt circulation to create conditions that are conducive to triggering abrupt climate transitions. Hence, it is argued that even for greenhouse warming, abrupt climate transitions similar to those in the last glacial time are unlikely to occur as the Bering Strait remains open. Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80–11 thousand years before present, but were nearly absent during interglacial periods and the early stages of glacial periods, when major ice-sheets were still forming. Here we show, with a fully coupled state-of-the-art climate model, that closing the Bering Strait and preventing its throughflow between the Pacific and Arctic Oceans during the glacial period can lead to the emergence of stronger hysteresis behavior of the ocean conveyor belt circulation to create conditions that are conducive to triggering abrupt climate transitions. Hence, it is argued that even for greenhouse warming, abrupt climate transitions similar to those in the last glacial time are unlikely to occur as the Bering Strait remains open. |
| Author | Wu, Bingyi Otto-Bliesner, Bette Timmermann, Axel Hu, Aixue Meehl, Gerald A Abe-Ouchi, Ayako Kimoto, Masahide Han, Weiqing Large, William Washington, Warren M Lambeck, Kurt Liu, Zhengyu |
| Author_xml | – sequence: 1 fullname: Hu, Aixue – sequence: 2 fullname: Meehl, Gerald A – sequence: 3 fullname: Han, Weiqing – sequence: 4 fullname: Timmermann, Axel – sequence: 5 fullname: Otto-Bliesner, Bette – sequence: 6 fullname: Liu, Zhengyu – sequence: 7 fullname: Washington, Warren M – sequence: 8 fullname: Large, William – sequence: 9 fullname: Abe-Ouchi, Ayako – sequence: 10 fullname: Kimoto, Masahide – sequence: 11 fullname: Lambeck, Kurt – sequence: 12 fullname: Wu, Bingyi |
| BackLink | https://www.ncbi.nlm.nih.gov/pubmed/22493225$$D View this record in MEDLINE/PubMed |
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| Snippet | Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from... Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80-11... Abrupt climate transitions, known as Dansgaard-Oeschger and Heinrich events, occurred frequently during the last glacial period, specifically from 80–11... |
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| StartPage | 6417 |
| SubjectTerms | Arctic region Atmospheric circulation climate Climate change Climate models Climatology Convection Fresh water Glaciers Global warming Greenhouse effect Greenhouses hysteresis Interglacial periods Marine Ocean circulation Oceans Paleoclimatology Physical Sciences Sea level Sea transportation |
| Title | Role of the Bering Strait on the hysteresis of the ocean conveyor belt circulation and glacial climate stability |
| URI | https://www.jstor.org/stable/41588544 http://www.pnas.org/content/109/17/6417.abstract https://www.ncbi.nlm.nih.gov/pubmed/22493225 https://www.proquest.com/docview/1009880453 https://www.proquest.com/docview/1009802767 https://www.proquest.com/docview/1069194204 https://www.proquest.com/docview/1999944149 https://pubmed.ncbi.nlm.nih.gov/PMC3340043 |
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