The Pacific Decadal Oscillation (PDO) is a long-lived El Niño-like pattern of Pacific climate variability, which has a great impact on the global ecosystem.
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PDO indices have been constructed by projecting the observed monthly patterns of North Pacific SST and SLP anomalies onto the characteristic SST and SLP patterns shown in Figures 1 and 2, respectively (Trenberth 1990, Trenberth and Hurrell 1994, Zhang et al.
Figure 4: (top) Characteristic warm-phase PDO October-March air temperature anomalies, in degrees C. This field is based on linear regressions between the gridded surface air temperature data and the SST-based PDO index, shown in the top panel of Figure 3, for the period 1900-1993.
This is true because of the PDO's strong tendency for multi-season and multi-year persistence.