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

  • Qiang Wang
  • , Mehmet Ilicak
  • , Rüdiger Gerdes
  • , Helge Drange
  • , Yevgeny Aksenov
  • , David A. Bailey
  • , Mats Bentsen
  • , Arne Biastoch
  • , Alexandra Bozec
  • , Claus Böning
  • , Christophe Cassou
  • , Eric Chassignet
  • , Andrew C. Coward
  • , Beth Curry
  • , Gokhan Danabasoglu
  • , Sergey Danilov
  • , Elodie Fernandez
  • , Pier Giuseppe Fogli
  • , Yosuke Fujii
  • , Stephen M. Griffies
  • Doroteaciro Iovino, Alexandra Jahn, Thomas Jung, William G. Large, Craig Lee, Camille Lique, Jianhua Lu, Simona Masina, A. J.George Nurser, Benjamin Rabe, Christina Roth, David Salas y Mélia, Bonita L. Samuels, Paul Spence, Hiroyuki Tsujino, Sophie Valcke, Aurore Voldoire, Xuezhu Wang, Steve G. Yeager
  • Helmholtz Centre for Polar and Marine Sciences
  • Uni Research
  • University of Bergen
  • National Oceanography Centre Southampton
  • National Center for Atmospheric Research
  • GEOMAR Helmholtz Centre for Ocean Research Kiel
  • Florida State University
  • Applied Physics Laboratory
  • CNRS
  • Euro Mediterranean Center on Climage Change
  • Japan Meteorological Agency
  • National Oceanic and Atmospheric Administration
  • University of Colorado Boulder
  • University of Bremen
  • University of Oxford
  • Département Ressources
  • Istituto Nazionale di Geofisica e Vulcanologia (INGV)
  • Météo-France/CNRS
  • University of New South Wales

Résultats de recherche: Contribution à un journalArticleRevue par des pairs

Résumé

The Arctic Ocean simulated in 14 global ocean-sea ice models in the framework of the Coordinated Ocean-ice Reference Experiments, phase II (CORE-II) is analyzed in this study. The focus is on the Arctic liquid freshwater (FW) sources and freshwater content (FWC). The models agree on the interannual variability of liquid FW transport at the gateways where the ocean volume transport determines the FW transport variability. The variation of liquid FWC is induced by both the surface FW flux (associated with sea ice production) and lateral liquid FW transport, which are in phase when averaged on decadal time scales. The liquid FWC shows an increase starting from the mid-1990s, caused by the reduction of both sea ice formation and liquid FW export, with the former being more significant in most of the models. The mean state of the FW budget is less consistently simulated than the temporal variability. The model ensemble means of liquid FW transport through the Arctic gateways compare well with observations. On average, the models have too high mean FWC, weaker upward trends of FWC in the recent decade than the observation, and low consistency in the temporal variation of FWC spatial distribution, which needs to be further explored for the purpose of model development.

langue originaleAnglais
Pages (de - à)86-109
Nombre de pages24
journalOcean Modelling
Volume99
Les DOIs
étatPublié - 1 mars 2016

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