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

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Fig. 8. Lag correlations between the PC time series of the first EOF of monthly 1000-hPa zonal wind and SST over the North Pacific in the CFS coupled run for each 30- yr period (light blue) and ensemble average (black) of the 16 correlation coefficients at different lags and those using 29-yr 1000-hPa zoanl wind from R2 and OISST (red). Negative (positive) lag means the 1000-hPa zonal wind leading (lagging) the SST. 32
Fig. 9. Seasonal variations of area-averaged (20 o –65 o N, 125 o E–120 o W) (a) monthly mean variance of the 1000-hPa zonal wind anomaly associated with the first EOF, (b) climatological MLD, and (c) square root of the zonal wind variance in month N–1 divided by the MLD in month N. Blue lines are for 16 individual members from the CFS, black lines for ensemble means, and red lines for observations (R2 and GODAS). 33
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 and 28: Fig. 1. Spatial patterns of SST ass
Page 29 and 30: Fig. 3. Same as in Fig. 2, but base
Page 31 and 32: Fig. 5. Same as in Fig. 4, but base
Page 33: Fig. 7. Same as in Fig. 6, but base

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

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