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Stephen M. Griffies, Michael Winton, Leo J. Donner, Larry W. Horowitz, Stephanie M. Downes, Riccardo Farneti, Anand Gnanadesikan, William J. Hurlin, Hyun-Chul Lee, Zhi Liang, Jaime B. Palter, Bonita L. Samuels, Andrew T. Wittenberg, Bruce L. Wyman, Jianjun Yin, and Niki Zadeh

model owing to insufficient grid resolution, we employ the exchange scheme described by Griffies et al. (2005) . The SSS biases for these regions expose limitations of this scheme, though we note that the more modest biases in the Mediterranean Sea illustrate that the scheme has some utility for this particular marginal sea. 2) Arctic Ocean There is a salty bias in the Arctic basin in both CM2.1 and CM3. There is some indication that the biases are larger near the shelves north of Siberia. The

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