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studies have been able to glean evidence of decadal-scale variability from what data are available. The dominant SST variations in the Pacific Basin were discussed in Chapter 3 (see Figures 3-6 through 3-9). The dec-cen pattern shown in Figure 3-8 has a broader The hottest vintage baby bear face all over printed slippersmeridional SST-anomaly pattern in the tropics than the ENSO pattern shown in Figure 3-6, and has clearly stronger values of mid-latitude SST relative to the tropical values. Thus, the analysis representative of longer time scales (Figure 3-8) indicates that the equatorial and mid-latitude regions contribute comparably strong anomalies, and that the regional contributions to climate are greater in geographical extent than the contributions from interannual-scale variability. The time coefficient of the interdecadal pattern in Figure 3-8 exhibits “regime shifts” in 1976 . Since the mid-latitude manifestation of this mode is so strong, it can be identified with a specifically North Pacific oscillation now called the Pacific Decadal Oscillation . The PDO can be

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