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  • GFDL'S Coupled Model-3 (CM3): Dynamics, Physical Parameterizations, and Simulations x
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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

when assessing model differences. Though the interior bias patterns differ in scale, they exhibit a strong correlation since the ocean components are nearly the same. b. Content of this paper Section 2 begins the paper with a discussion of salient properties of the ocean surface, including sea surface temperature, salinity, sea ice, and sea level. Section 3 then considers some of the water mass biases seen in the ocean interior, with the dominant bias arising from the heat in CM3 associated with

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