North Atlantic simulations in Coordinated Ocean-ice Reference Experiments phase II (CORE-II). Part II: Inter-annual to decadal variability
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- 作者：Gokhan Danabasoglu ; a ; gokhan@ucar.edu" class="auth_mail" title="E-mail the corresponding author ; Steve G. Yeagera ; Who M. Kimb ; Erik Behrensc ; Mats Bentsend ; Daohua Bie ; Arne Biastochc ; Rainer Bleckf ; g ; Claus Bö ; ningc ; Alexandra Bozech ; Vittorio M. Canutog ; Christophe Cassoui ; Eric Chassigneth ; Andrew C. Cowardj ; Sergey Danilovk ; Nikolay Dianskyl ; Helge Drangem ; Riccardo Farnetin ; Elodie Fernandezi ; o ; Pier Giuseppe Foglip ; Gael Forgetq ; Yosuke Fujiir ; Stephen M. Griffiess ; Anatoly Gusevl ; Patrick Heimbachq ; Armando Howardg ; t ; Mehmet Ilicakd ; Thomas Jungk ; Alicia R. Karspecka ; Maxwell Kelleyg ; William G. Largea ; Anthony Leboissetierg ; Jianhua Luh ; Gurvan Madecu ; Simon J. Marslande ; Simona Masinap ; v ; Antonio Navarrap ; v ; A.J. George Nurserj ; Anna Piraniw ; Anastasia Romanoug ; x ; David Salas y Mé ; liay ; Bonita L. Samuelss ; Markus Scheinertc ; Dmitry Sidorenkok ; Shan Sunf ; Anne-Marie Treguierz ; Hiroyuki Tsujinor ; Petteri Uotilae ; aa ; Sophie Valckei ; Aurore Voldoirey ; Qiang Wangk ; Igor Yashayaevab
- 关键词：Global ocean &ndash ; sea-ice modelling ; Ocean model comparisons ; Atmospheric forcing ; Inter-annual to decadal variability and mechanisms ; Atlantic meridional overturning circulation variability ; Variability in the North Atlantic
- 刊名：Ocean Modelling
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：97
- 期：Complete
- 页码：65-90
- 全文大小：7659 K
文摘
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Inter-annual to decadal variability in AMOC from CORE-II simulations is presented.
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AMOC variability shows three stages, with maximum transports in mid- to late-1990s.
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North Atlantic temporal variability features are in good agreement among simulations.
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Such agreements suggest variability is dictated by the atmospheric data sets.
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Simulations differ in spatial structures of variability due to ocean dynamics.