edu.ucar.opensky::articles:18315 UCAR/NCAR - Library OpenSky Support PO Box 3000 Boulder CO 80307-3000 opensky@ucar.edu http://opensky.ucar.edu/ homepage pointOfContact 2025-12-26T02:52:04.036919 ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data ISO 19115-2:2009(E) https://n2t.org/ark:/85065/d7nv9ktv An assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part III: Hydrography and fluxes 2016-04-01T00:00:00Z publication https://n2t.org/ark:/85065/d7nv9ktv https://doi.org/10.1016/j.ocemod.2016.02.004 Ilıcak, M. author Drange, H. author Wang, Q. author Gerdes, R. author Aksenov, Y. author Bailey, David A. author Bentsen, M. author Biastoch, A. author Bozec, A. author Böning, C. author Cassou, C. author Chassignet, E. author Coward, A. author Curry, B. author Danabasoglu, Gokhan author Danilov, S. author Fernandez, E. author Fogli, P. G. author Fujii, Y. author Griffies, S. author Iovino, D. author Jahn, Alexandra author Jung, T. author Large, William G. author Lee, C. author Lique, C. author Lu, J. author Masina, S. author Nurser, A. author Roth, C. author Salas y Mélia, D. author Samuels, B. author Spence, P. author Tsujino, H. author Valcke, S. author Voldoire, A. author Wang, X. author Yeager, Stephen author UCAR/NCAR - Library publisher In this paper we compare the simulated Arctic Ocean in 15 global ocean–sea ice models in the framework of the Coordinated Ocean-ice Reference Experiments, phase II (CORE-II). Most of these models are the ocean and sea-ice components of the coupled climate models used in the Coupled Model Intercomparison Project Phase 5 (CMIP5) experiments. We mainly focus on the hydrography of the Arctic interior, the state of Atlantic Water layer and heat and volume transports at the gateways of the Davis Strait, the Bering Strait, the Fram Strait and the Barents Sea Opening. We found that there is a large spread in temperature in the Arctic Ocean between the models, and generally large differences compared to the observed temperature at intermediate depths. Warm bias models have a strong temperature anomaly of inflow of the Atlantic Water entering the Arctic Ocean through the Fram Strait. Another process that is not represented accurately in the CORE-II models is the formation of cold and dense water, originating on the eastern shelves. In the cold bias models, excessive cold water forms in the Barents Sea and spreads into the Arctic Ocean through the St. Anna Through. There is a large spread in the simulated mean heat and volume transports through the Fram Strait and the Barents Sea Opening. The models agree more on the decadal variability, to a large degree dictated by the common atmospheric forcing. We conclude that the CORE-II model study helps us to understand the crucial biases in the Arctic Ocean. The current coarse resolution state-of-the-art ocean models need to be improved in accurate representation of the Atlantic Water inflow into the Arctic and density currents coming from the shelves. UCAR/NCAR - Library OpenSky Support PO Box 3000 Boulder CO 80307-3000 opensky@ucar.edu http://opensky.ucar.edu/ homepage pointOfContact PDF Text theme Resource Type 2016-01-01T00:00:00Z publication Copyright 2016 Elsevier. None eng geoscientificInformation