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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

SST biases in the Southern Ocean. 5) North Pacific The increased radiative heating of the North Pacific in CM3 helps to counteract the cold North Pacific bias found in CM2.1, which was associated with excessive sea ice cover (see Fig. 9 discussed in section 2c ). As a result, the broadly cool North Pacific in CM2.1 has been pushed back in CM3 to a weaker bias of the North Pacific gyre, with a slight warming along the coast of North America. 6) West coast of America and Africa Both CM3 and CM2

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