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observed are small, they are significant in that they involve vast quantities of water, and therefore must be related to large-scale persistent changes in the environment at the air-sea interface (see, e.g., Coles et al., 1996; Zenk and Hogg, 1996). An abyssal warming and a decline in bottom-water transport were observed in at the equator at the northern end of the Brazil Basin; the temperatures involved were all lower than measurements made in the same location in 1972, 1983, and 1989, however, suggesting recovery from some intervening cold event (Hall et al., 1997). Hall et al. also found a pronounced seasonal cycle in the deep circulation. This rapid cycling suggests that the deep limb of the THC is less isolated from higher-frequency forcing than might be expected, and that perhaps in the tropics the Hot carp fishing all over print stainless steel tumblerbehaviors of the deep/cold and shallow/warm limbs of the THC are dynamically coupled. Temperature variations have also been documented below the surface. Figure 5-22 shows the 500 m temperature difference between two 5-year averages 15 years apart . Differences of more that half a degree are clearly seen. Similar results have been found in two deeper surveys (Roemmich and Wunsch, 1984; Parilla et al., 1994). Also, the heat content of the upper ocean near Bermuda appears to have increased since the 1970s, and the thermocline to have moved correspondingly . These observations reflect interdecadal changes in both the properties and the volume of the upper water mass, in response to changes in the dynamics

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