An assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part II: Liquid freshwater

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• 作者：Qiang Wang ; ^a ; ^{Qiang.Wang@awi.de" class="auth_mail" title="E-mail the corresponding author} ; Mehmet Ilicak^b ; Rü ; diger Gerdes^a ; Helge Drange^c ; Yevgeny Aksenov^d ; David A Bailey^e ; Mats Bentsen^b ; Arne Biastoch^f ; Alexandra Bozec^g ; Claus Bö ; ning^f ; Christophe Cassou^h ; Eric Chassignet^g ; Andrew C. Coward^d ; Beth Curryⁱ ; Gokhan Danabasoglu^e ; Sergey Danilov^a ; Elodie Fernandez^h ; Pier Giuseppe Fogli^j ; Yosuke Fujii^k ; Stephen M. Griffies^l ; Doroteaciro Iovino^j ; Alexandra Jahn^e ; ^m ; Thomas Jung^a ; ⁿ ; William G. Large^e ; Craig Leeⁱ ; Camille Lique^o ; ^p ; Jianhua Lu^g ; Simona Masina^j ; ^t ; A.J. George Nurser^d ; Benjamin Rabe^a ; Christina Roth^f ; David Salas y Mé ; lia^q ; Bonita L. Samuels^l ; Paul Spence^r ; ^s ; Hiroyuki Tsujino^k ; Sophie Valcke^h ; Aurore Voldoire^q ; Xuezhu Wang^a ; Steve G. Yeager^e
• 关键词：Arctic Ocean ; Freshwater ; Sea ice ; CORE II atmospheric forcing
• 刊名：Ocean Modelling
• 出版年：2016
• 出版时间：March 2016
• 年：2016
• 卷：99
• 期：Complete
• 页码：86-109
• 全文大小：5882 K

文摘

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d="para0001">Arctic liquid freshwater budget simulated in 14 CORE-II models is studied.

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d="para0002">The models better represent the temporal variability than the mean state.

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d="para0003">Multi-model mean (MMM) FW fluxes compare well with observations.

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d="para0004">MMM FWC shows an upward trend in the recent years, with an underestimated rate.

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d="para0005">FW flux interannual variability is more consistent where volume flux determines it.

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