Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM
The mechanisms involved in the variability of Atlantic Meridional Overturning Circulation (AMOC) are studied using a 2000-yr control simulation of the coupled Fast Ocean-Atmosphere Model (FOAM). This study identifies a coupled mode between SST and surface heat flux in the North Atlantic at the decad...
Published in: | Advances in Atmospheric Sciences |
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Main Authors: | , , |
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Format: | Journal/Newspaper |
Language: | English |
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大气科学进展英文版
2014
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.11897/214825 https://doi.org/10.1007/s00376-013-3021-3 |
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author | Huang, Boyin Zhu Jiang Yang Haijun |
author2 | Huang, BY (reprint author), NOAA, Natl Climat Data Ctr, Asheville, NC 28801 USA. NOAA, Natl Climat Data Ctr, Asheville, NC 28801 USA. Peking Univ, Lab Climate & Ocean Atmosphere Studies, Sch Phys, Beijing 100871, Peoples R China. Peking Univ, Dept Atmospher & Ocean Sci, Sch Phys, Beijing 100871, Peoples R China. |
author_facet | Huang, Boyin Zhu Jiang Yang Haijun |
author_sort | Huang, Boyin |
collection | Peking University Institutional Repository (PKU IR) |
container_issue | 2 |
container_start_page | 241 |
container_title | Advances in Atmospheric Sciences |
container_volume | 31 |
description | The mechanisms involved in the variability of Atlantic Meridional Overturning Circulation (AMOC) are studied using a 2000-yr control simulation of the coupled Fast Ocean-Atmosphere Model (FOAM). This study identifies a coupled mode between SST and surface heat flux in the North Atlantic at the decadal timescale, as well as a forcing mode of surface heat flux at the interannual timescale. The coupled mode is regulated by AMOC through meridional heat transport. The increase in surface heating in the North Atlantic weakens the AMOC approximately 10 yr later, and the weakened AMOC in turn decreases SST and sea surface salinity. The decreased SST results in an increase in surface heating in the North Atlantic, thus forming a positive feedback loop. Meanwhile, the weakened AMOC weakens northward heat transport and therefore lowers subsurface temperature approximately 19 yr later, which prevents the AMOC from weakening. In the forcing mode, the surface heat flux leads AMOC by approximately 4 yr. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000334180700001&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Meteorology & Atmospheric Sciences SCI(E) 中国科技核心期刊(ISTIC) 中国科学引文数据库(CSCD) 2 ARTICLE boyin.huang@noaa.gov 2 241-251 31 |
format | Journal/Newspaper |
genre | North Atlantic North atlantic Thermohaline circulation |
genre_facet | North Atlantic North atlantic Thermohaline circulation |
id | ftpekinguniv:oai:localhost:20.500.11897/214825 |
institution | Open Polar |
language | English |
op_collection_id | ftpekinguniv |
op_container_end_page | 251 |
op_doi | https://doi.org/20.500.11897/214825 https://doi.org/10.1007/s00376-013-3021-3 |
op_relation | ADVANCES IN ATMOSPHERIC SCIENCES.2014,31,(2),241-251. 784904 0256-1530 http://hdl.handle.net/20.500.11897/214825 1861-9533 doi:10.1007/s00376-013-3021-3 WOS:000334180700001 |
op_source | SCI |
publishDate | 2014 |
publisher | 大气科学进展英文版 |
record_format | openpolar |
spelling | ftpekinguniv:oai:localhost:20.500.11897/214825 2025-01-16T23:32:30+00:00 Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM Huang, Boyin Zhu Jiang Yang Haijun Huang, BY (reprint author), NOAA, Natl Climat Data Ctr, Asheville, NC 28801 USA. NOAA, Natl Climat Data Ctr, Asheville, NC 28801 USA. Peking Univ, Lab Climate & Ocean Atmosphere Studies, Sch Phys, Beijing 100871, Peoples R China. Peking Univ, Dept Atmospher & Ocean Sci, Sch Phys, Beijing 100871, Peoples R China. 2014 https://hdl.handle.net/20.500.11897/214825 https://doi.org/10.1007/s00376-013-3021-3 en eng 大气科学进展英文版 ADVANCES IN ATMOSPHERIC SCIENCES.2014,31,(2),241-251. 784904 0256-1530 http://hdl.handle.net/20.500.11897/214825 1861-9533 doi:10.1007/s00376-013-3021-3 WOS:000334180700001 SCI Atlantic Meridional Overturning Circulation AMOC variability coupled mode and forcing mode NORTH-ATLANTIC THERMOHALINE CIRCULATION DECADAL VARIABILITY CLIMATE-CHANGE MODEL OSCILLATION PRECIPITATION SIMULATION TRANSPORTS Journal 2014 ftpekinguniv https://doi.org/20.500.11897/214825 https://doi.org/10.1007/s00376-013-3021-3 2021-08-01T08:35:01Z The mechanisms involved in the variability of Atlantic Meridional Overturning Circulation (AMOC) are studied using a 2000-yr control simulation of the coupled Fast Ocean-Atmosphere Model (FOAM). This study identifies a coupled mode between SST and surface heat flux in the North Atlantic at the decadal timescale, as well as a forcing mode of surface heat flux at the interannual timescale. The coupled mode is regulated by AMOC through meridional heat transport. The increase in surface heating in the North Atlantic weakens the AMOC approximately 10 yr later, and the weakened AMOC in turn decreases SST and sea surface salinity. The decreased SST results in an increase in surface heating in the North Atlantic, thus forming a positive feedback loop. Meanwhile, the weakened AMOC weakens northward heat transport and therefore lowers subsurface temperature approximately 19 yr later, which prevents the AMOC from weakening. In the forcing mode, the surface heat flux leads AMOC by approximately 4 yr. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000334180700001&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Meteorology & Atmospheric Sciences SCI(E) 中国科技核心期刊(ISTIC) 中国科学引文数据库(CSCD) 2 ARTICLE boyin.huang@noaa.gov 2 241-251 31 Journal/Newspaper North Atlantic North atlantic Thermohaline circulation Peking University Institutional Repository (PKU IR) Advances in Atmospheric Sciences 31 2 241 251 |
spellingShingle | Atlantic Meridional Overturning Circulation AMOC variability coupled mode and forcing mode NORTH-ATLANTIC THERMOHALINE CIRCULATION DECADAL VARIABILITY CLIMATE-CHANGE MODEL OSCILLATION PRECIPITATION SIMULATION TRANSPORTS Huang, Boyin Zhu Jiang Yang Haijun Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM |
title | Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM |
title_full | Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM |
title_fullStr | Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM |
title_full_unstemmed | Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM |
title_short | Mechanisms of Atlantic Meridional Overturning Circulation(AMOC) Variability in a Coupled Ocean-Atmosphere GCM |
title_sort | mechanisms of atlantic meridional overturning circulation(amoc) variability in a coupled ocean-atmosphere gcm |
topic | Atlantic Meridional Overturning Circulation AMOC variability coupled mode and forcing mode NORTH-ATLANTIC THERMOHALINE CIRCULATION DECADAL VARIABILITY CLIMATE-CHANGE MODEL OSCILLATION PRECIPITATION SIMULATION TRANSPORTS |
topic_facet | Atlantic Meridional Overturning Circulation AMOC variability coupled mode and forcing mode NORTH-ATLANTIC THERMOHALINE CIRCULATION DECADAL VARIABILITY CLIMATE-CHANGE MODEL OSCILLATION PRECIPITATION SIMULATION TRANSPORTS |
url | https://hdl.handle.net/20.500.11897/214825 https://doi.org/10.1007/s00376-013-3021-3 |