An assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part III: Hydrography and fluxes
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- 作者：Mehmet Ilıcak ; a ; mehmet.ilicak@noaa.gov" class="auth_mail" title="E-mail the corresponding author ; mehmet.ilicak@uni.no" class="auth_mail" title="E-mail the corresponding author ; Helge Drangeb ; c ; Qiang Wangd ; Rü ; diger Gerdesd ; Yevgeny Aksenove ; David Baileyf ; Mats Bentsena ; Arne Biastochg ; Alexandra Bozech ; Claus Bö ; ningg ; Christophe Cassoui ; Eric Chassigneth ; Andrew C. Cowarde ; Beth Curryj ; Gokhan Danabasogluf ; Sergey Danilovd ; Elodie Fernandezi ; Pier Giuseppe Foglik ; Yosuke Fujiil ; Stephen M. Griffiesm ; Doroteaciro Iovinok ; Alexandra Jahnf ; s ; Thomas Jungd ; William G. Largef ; Craig Leej ; Camille Liquen ; u ; Jianhua Luh ; Simona Masinak ; r ; A.J. George Nursere ; Christina Rothg ; David Salas y Mé ; liao ; Bonita L. Samuelsm ; Paul Spencep ; q ; Hiroyuki Tsujinol ; Sophie Valckei ; Aurore Voldoireo ; Xuezhu Wangd ; Steve G. Yeagerf
- 关键词：Arctic Ocean ; Atlantic Water ; St. Anna Trough ; Density currents ; CORE-II atmospheric forcing
- 刊名：Ocean Modelling
- 出版年：2016
- 出版时间：April 2016
- 年：2016
- 卷：100
- 期：Complete
- 页码：141-161
- 全文大小：8677 K
文摘
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We compare the simulated Arctic Ocean in 15 global ocean–sea ice models.
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There is a large spread in temperature bias in the Arctic Ocean between the models.
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Warm bias models have a strong temperature anomaly of inflow of Atlantic Water.
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Dense outflows formed on Arctic shelves are not captured accurately in the models.