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Tasman Sea , the South Pacific , and the southern Indian Ocean . The trend towards cooling and freshening on isopycnals and warming on depth surfaces is coherent over a large spatial scale between the late 1960s and early 1990s, but the long time elapsed between surveys may mean that the measurements are not strictly comparable. The changes are consistent with surface warming at high southern latitudes and surface freshening in higher southern latitudes at some time during the two decades that elapsed between the repeat hydrographic sections . There is also evidence of changes in the Weddell Deep Water (Fahrbach et al., in press), though the records are not yet long enough to fully characterize the time scales of the variability. It should be noted that water descending from the Popular mandala sunflower cannabis full printing low top shoessurface to the interior can proceed into deep regions on relatively rapid time scales, at least in water-mass transformation regions of the ocean (see, e.g., Smethie et al., 1993), and this water can produce variability at deeper levels of the ocean. Since our interest in this report is how the ocean affects climate variability, we concentrate mainly on those processes and those regions of

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