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Ivana Cerovečki and Matthew R. Mazloff

be addressed in future work. Acknowledgments IC was supported by the National Science Foundation (NSF) Ocean Sciences Grants OCE-0850869 and OCE-1357072 to the Scripps Institution of Oceanography and by the New International Fellowship Mobility Programme for Experienced Researchers (NEWFELPRO) under the European Union's Seventh Framework Programme for research, technological development and demonstration (FP7-PEOPLE-2011-COFUND-MCA, Grant Agreement 291823). MRM acknowledges the NSF for support of

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Ross Tulloch, Raffaele Ferrari, Oliver Jahn, Andreas Klocker, Joseph LaCasce, James R. Ledwell, John Marshall, Marie-Jose Messias, Kevin Speer, and Andrew Watson

span the top 1900 m, are all less than 35 m thick. 1 The Interim European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-Interim; Simmons et al. 2006 ) 6-h winds and buoyancy fluxes force the model’s surface, and the Ocean Comprehensive Atlas (OCCA; Forget 2010 ) provides monthly transports, heat and salt fluxes, as well as sea ice area and thickness at the lateral boundaries. Initial model conditions are an interpolation of the 1° × 1° resolution OCCA state on 1 January 2005

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