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circulation plays an important role in shaping the three-dimensional properties of the world ocean. It determines the amount of solar radiation reaching the surface, the latent and sensible heat exchange with the ocean surface, the amount of freshwater that falls onto the surface, and the dynamic forcing of the surface ocean circulation. (For a complete description, see the “Ocean Circulation” section of this chapter.) In turn, it is the ocean that plays the major role in The hottest product baby bear with heart all over printed slippersdetermining the dec-cen variability of the Earth’ s climate, mainly through the ocean’s thermal memory and the delayed effect of its sluggish circulation on the atmosphere . The stationary eddies induce large northward transports of heat and moisture, and set up a zonally uneven distribution of climate regimes, in which east and west sides of continents experience different mean and time-varying conditions. There is a strong link in both location and scale between the climate patterns described in Chapter 3 and the stationary eddies. To some extent, the climate patterns can be thought of as fluctuations in the strength and

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