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A series of simulations at R15, T21, T31, T63, and T106 horizontal
truncations has been completed. Minor changes to the parameters in the
cloud parameterization were made to minimize the differences in the
global average fractional cloudiness between resolutions. These
changes are described in Williamson et al. (1993). The simulations all
used the climatological monthly averaged SSTs of Shea et al. (1992).
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