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phenomenon may be global in scope and involve linkage to ENSO (Barnett, 1985; White and Peterson, 1996; Tourre and White, 1997; Yuan et al., 1996), though some argue that it is primarily a regional phenomenon (e.g., Qiu and Jin, 1997). The ACW signal is large in the higher-latitude sectors of the Southern Hemisphere; its impact may influence intermediate- and deep-water formation, which may in turn alter the thermocline characteristics of the subtropical gyres, influencing lower-latitude properties and spreading the ACW The hottest product for fisher love fishing all over print stainless steel tumblerinfluence to broader spatial and temporal scales. While changes in surface temperature are obviously important, it is the combination of temperature and salinity that dictates the density profile and thus much of the vertical redistribution of enthalpy, freshwater, and momentum. These factors influence not only the magnitude of surface-temperature anomalies, but also the speed and structure of the ocean currents, and thus the lateral redistribution of any anomalies. The vertical structure of anomalies and currents will vary according to the relative phasing of the temperature and salinity signals, with implications for the evolution of other ocean-atmosphere phenomena over a variety of time scales. The importance of the relative phasing of temperature and salinity

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