Seasonality of the Pacific decadal oscillation - Climate Prediction ...

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Fig. 2. PDO-related monthly ocean temperature anomalies (shading, o C) and correlation (contour) with the PDO PC time series at 37 o N across the North Pacific in the CFS. The anomalies are obtained by regressing ocean temperature anomaly vs. the PC time series of the first EOF of North Pacific SST in individual 30-yr segments. The anomalies are based on the ensemble average of 16 members and are associated with one standard deviation fluctuations in the PC time series for months from January to August. The correlation coefficients are also based on the ensemble average of the 16 members. Contours are ±0.3, ±0.5, and ±0.7 with negative contours dashed. 26
Fig. 3. Same as in Fig. 2, but based on 29-yr (1982–2010) ocean temperature from the GODAS and the first EOF of North Pacific SST from the OISST. 27
Page 1 and 2: AMERICAN METEOROLOGICAL SOCIETY Jou
Page 3 and 4: ABSTRACT The seasonality of the Pac
Page 5 and 6: The PDO can also modulate the impac
Page 7 and 8: ealizations provides an estimate of
Page 9 and 10: more connection with SST variabilit
Page 11 and 12: and April the cold temperature anom
Page 13 and 14: wind over the North Pacific region
Page 15 and 16: first EOF of the 1000-hPa zonal win
Page 17 and 18: heat flux. This indicates that shor
Page 19 and 20: SST response to the surface wind le
Page 21 and 22: Barnett, T. P., D. W. Pierce, R. Sa
Page 23 and 24: Newman, M. E., and P. D. Sardeshmuk
Page 25 and 26: Figure Captions Fig. 1. Spatial pat
Page 27: Fig. 1. Spatial patterns of SST ass
Page 31 and 32: Fig. 5. Same as in Fig. 4, but base
Page 33 and 34: Fig. 7. Same as in Fig. 6, but base
Page 35 and 36: Fig. 9. Seasonal variations of area

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