Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation
In a transient simulation of the last deglaciation with a fully coupled model (TraCE-21000), an overshoot of the Atlantic Meridional Overturning Circulation (AMOC) is simulated and proposed as a key factor for the onset of the Bolling-Allerod (BA) warming event. There is collaborating evidence for a...
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Online Access: | https://hdl.handle.net/20.500.11897/395702 https://doi.org/10.5194/cp-7-935-2011 |
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ftpekinguniv:oai:localhost:20.500.11897/395702 2023-05-15T17:29:31+02:00 Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation Cheng, J. Liu, Z. He, F. Otto-Bliesner, B. L. Colose, C. Cheng, J (reprint author), Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Minist Educ, Nanjing 210044, Peoples R China. Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Minist Educ, Nanjing 210044, Peoples R China. Nanjing Univ Informat Sci & Technol, Coll Atmospher Sci, Nanjing 210044, Peoples R China. Univ Wisconsin, Ctr Climat Res, Madison, WI 53706 USA. Univ Wisconsin, Dept Atmospher & Ocean Sci, Madison, WI 53706 USA. Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China. Natl Ctr Atmospher Res, Climate & Global Dynam Div, Boulder, CO 80307 USA. SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY 12222 USA. 2011 https://hdl.handle.net/20.500.11897/395702 https://doi.org/10.5194/cp-7-935-2011 en eng climate of the past CLIMATE OF THE PAST.2011,7,(3),935-940. 926277 1814-9324 http://hdl.handle.net/20.500.11897/395702 doi:10.5194/cp-7-935-2011 WOS:000295356800016 SCI CLIMATE SYSTEM MODEL THERMOHALINE CIRCULATION VERSION-3 CCSM3 DEEP CONVECTION VARIABILITY OCEAN SIMULATION MECHANISM COLLAPSE RECOVERY Journal 2011 ftpekinguniv https://doi.org/20.500.11897/395702 https://doi.org/10.5194/cp-7-935-2011 2021-08-01T10:22:26Z In a transient simulation of the last deglaciation with a fully coupled model (TraCE-21000), an overshoot of the Atlantic Meridional Overturning Circulation (AMOC) is simulated and proposed as a key factor for the onset of the Bolling-Allerod (BA) warming event. There is collaborating evidence for an AMOC overshoot at the BA in various proxy reconstructions although the mechanism governing its behavior is not well understood. Here, we present two new sensitivity experiments to explicitly illustrate the impact of North Atlantic - GIN Sea exchange on the AMOC's deglacial evolution. Results show that this oceanic exchange dominates the convection restarting in the GIN Sea, the occurrence of the AMOC overshoot, and the full BA warming. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000295356800016&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Geosciences, Multidisciplinary Meteorology & Atmospheric Sciences SCI(E) 3 ARTICLE 3 935-940 7 Journal/Newspaper North Atlantic Peking University Institutional Repository (PKU IR) Climate of the Past 7 3 935 940 |
institution |
Open Polar |
collection |
Peking University Institutional Repository (PKU IR) |
op_collection_id |
ftpekinguniv |
language |
English |
topic |
CLIMATE SYSTEM MODEL THERMOHALINE CIRCULATION VERSION-3 CCSM3 DEEP CONVECTION VARIABILITY OCEAN SIMULATION MECHANISM COLLAPSE RECOVERY |
spellingShingle |
CLIMATE SYSTEM MODEL THERMOHALINE CIRCULATION VERSION-3 CCSM3 DEEP CONVECTION VARIABILITY OCEAN SIMULATION MECHANISM COLLAPSE RECOVERY Cheng, J. Liu, Z. He, F. Otto-Bliesner, B. L. Colose, C. Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation |
topic_facet |
CLIMATE SYSTEM MODEL THERMOHALINE CIRCULATION VERSION-3 CCSM3 DEEP CONVECTION VARIABILITY OCEAN SIMULATION MECHANISM COLLAPSE RECOVERY |
description |
In a transient simulation of the last deglaciation with a fully coupled model (TraCE-21000), an overshoot of the Atlantic Meridional Overturning Circulation (AMOC) is simulated and proposed as a key factor for the onset of the Bolling-Allerod (BA) warming event. There is collaborating evidence for an AMOC overshoot at the BA in various proxy reconstructions although the mechanism governing its behavior is not well understood. Here, we present two new sensitivity experiments to explicitly illustrate the impact of North Atlantic - GIN Sea exchange on the AMOC's deglacial evolution. Results show that this oceanic exchange dominates the convection restarting in the GIN Sea, the occurrence of the AMOC overshoot, and the full BA warming. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000295356800016&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Geosciences, Multidisciplinary Meteorology & Atmospheric Sciences SCI(E) 3 ARTICLE 3 935-940 7 |
author2 |
Cheng, J (reprint author), Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Minist Educ, Nanjing 210044, Peoples R China. Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Minist Educ, Nanjing 210044, Peoples R China. Nanjing Univ Informat Sci & Technol, Coll Atmospher Sci, Nanjing 210044, Peoples R China. Univ Wisconsin, Ctr Climat Res, Madison, WI 53706 USA. Univ Wisconsin, Dept Atmospher & Ocean Sci, Madison, WI 53706 USA. Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China. Natl Ctr Atmospher Res, Climate & Global Dynam Div, Boulder, CO 80307 USA. SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY 12222 USA. |
format |
Journal/Newspaper |
author |
Cheng, J. Liu, Z. He, F. Otto-Bliesner, B. L. Colose, C. |
author_facet |
Cheng, J. Liu, Z. He, F. Otto-Bliesner, B. L. Colose, C. |
author_sort |
Cheng, J. |
title |
Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation |
title_short |
Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation |
title_full |
Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation |
title_fullStr |
Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation |
title_full_unstemmed |
Impact of North Atlantic - GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation |
title_sort |
impact of north atlantic - gin sea exchange on deglaciation evolution of the atlantic meridional overturning circulation |
publisher |
climate of the past |
publishDate |
2011 |
url |
https://hdl.handle.net/20.500.11897/395702 https://doi.org/10.5194/cp-7-935-2011 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
SCI |
op_relation |
CLIMATE OF THE PAST.2011,7,(3),935-940. 926277 1814-9324 http://hdl.handle.net/20.500.11897/395702 doi:10.5194/cp-7-935-2011 WOS:000295356800016 |
op_doi |
https://doi.org/20.500.11897/395702 https://doi.org/10.5194/cp-7-935-2011 |
container_title |
Climate of the Past |
container_volume |
7 |
container_issue |
3 |
container_start_page |
935 |
op_container_end_page |
940 |
_version_ |
1766123670429761536 |