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subject to the criticism that the atmospheric response could change the variability, they illustrate the role of purely oceanic interactions in inducing variability. For longer time scales, for some regions, and for some climatic phenomena, the ocean is not simply a well-mixed layer passively responding to flux anomalies forced by the Amazing baby bear face all over printed slippersatmosphere. The ocean may also have active modes of internal variability that force an atmospheric response, or participate actively in coupled ocean-atmosphere modes of variability on the dec-cen time scale. The ocean’s active role in dec-cen climate variability involves several local mechanisms. The ocean’s redistribution of freshwater is a dominant agent in the hydrologic cycle. It compensates almost completely for the meridional transport of water vapor in the atmosphere. The remainder of the contribution from river flow is approximately an order of magnitude smaller. There are significant differences in the patterns of net water flux into the various ocean basins. For instance, the North Pacific receives much more precipitation than the North Atlantic. As a result, the North Pacific is a fresher ocean that does not support deep-water formation or a significant thermohaline circulation, as previously mentioned. This limits the amount of heat it can carry through

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