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...

Full description

Bibliographic Details
Published in:Advances in Atmospheric Sciences
Main Authors: Huang, Boyin, Zhu Jiang, Yang Haijun
Other Authors: 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.
Format: Journal/Newspaper
Language:English
Published: 大气科学进展英文版 2014
Subjects:
Online Access:https://hdl.handle.net/20.500.11897/214825
https://doi.org/10.1007/s00376-013-3021-3
_version_ 1821637973114880000
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