An assessment of Antarctic Circumpolar Current and Southern Ocean meridional overturning circulation during 1958-2007 in a suite of interannual CORE-II simulations
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- 作者：Riccardo Farneti ; a ; rfarneti@ictp.it" class="auth_mail" title="E-mail the corresponding author ; Stephanie M. Downesb ; Stephen M. Griffiesc ; Simon J. Marslandd ; Erik Behrense ; Mats Bentsenf ; Daohua Bid ; Arne Biastoche ; Claus Bö ; ninge ; Alexandra Bozecg ; Vittorio M. Canutoh ; Eric Chassignetg ; Gokhan Danabasoglui ; Sergey Danilovj ; Nikolay Dianskyk ; Helge Drangel ; Pier Giuseppe Foglim ; Anatoly Gusevk ; Robert W. Hallbergc ; Armando Howardh ; s ; Mehmet Ilicakf ; Thomas Jungj ; Maxwell Kelleyh ; William G. Largei ; Anthony Leboissetierh ; n ; Matthew Longi ; Jianhua Lug ; Simona Masinam ; o ; Akhilesh Mishrag ; Antonio Navarram ; o ; A.J. George Nurserp ; Lavinia Patarae ; Bonita L. Samuelsc ; Dmitry Sidorenkoj ; Hiroyuki Tsujinoq ; Petteri Uotilad ; r ; Qiang Wangj ; Steve G. Yeageri
- 关键词：Global ocean&ndash ; sea ice modeling ; Model comparisons ; Southern Ocean meridional overturning circulation ; Antarctic Circumpolar Current ; Southern Ocean dynamics
- 刊名：Ocean Modelling
- 出版年：2015
- 出版时间：September 2015
- 年：2015
- 卷：93
- 期：Complete
- 页码：84-120
- 全文大小：7540 K
文摘
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We focus on ACC and Southern Ocean MOC during 1958–2007 in 17 CORE-II forced models.
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Most CORE-II simulations are close to eddy saturation.
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Most CORE-II simulations are far from showing signs of eddy compensation.
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Constant in time or space k results in poor representation of mesoscale eddy effects.
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MOC has larger sensitivity than ACC transport even in eddy saturated state.