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(wind forcing and associated thermocline response, or ”heave”) and thermodynamics . For example, there is a cooling of the dominant regional convective water mass, known as 18ºC water, from the mid-1950s to about 1970, and then a warming till the mid- 1990s. The cooling and warming are in phase with those in the Greenland-Iceland-Norwegian Seas, and opposite in phase to those in the Labrador Sea and the NAO (Dickson et al., 1996). In addition to improving model representations of the hydrologic cycle, we must also better document its temporal variability. The distribution of water vapor in the atmosphere, particularly the vertical distribution, needs to be better Top carp fishing all over print stainless steel tumblerunderstood, because considerable controversy surrounds it. One theory about anthropogenic enhancement of the greenhouse effect suggests that increases in moisture in lower levels of the atmosphere will be offset by decreases in the upper troposphere, reducing surface warming while cooling upper layers. If this offset does indeed occur, it would greatly reduce the net warming that would otherwise be anticipated to result from an increase in total atmospheric water vapor (see, e.g., Lindzen, 1996). As mentioned previously, direct measurements of water vapor in the upper levels of the atmosphere are difficult to make, and the results have been contradictory. Clearly, accurate treatment of upper-level water vapor is essential to realistic modeling of the climate

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