Pacific Decadal Oscillation in CCSM3 Large Ensemble Experiment June18 2008 Haiyan Teng and Grant Branstator NCAR CGD 13th Annual CCSM Workshop CCWG.

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Presentation transcript:

Pacific Decadal Oscillation in CCSM3 Large Ensemble Experiment June18 2008 Haiyan Teng and Grant Branstator NCAR CGD 13th Annual CCSM Workshop CCWG

CCSM3 T42 Large Ensemble Experiment CCSM3 Large Ensemble Experiment CCSM3 T42 Large Ensemble Experiment T42 One historical run 1870-1999  30-member A1B scenario, 2000-2061 ocn/lnd/ice same initial data; atm 1999-12-03 to 2000-01-14 Bassi, Bluesky, Bluevista, Blueice CCSM CVWG & CCWG Data post processed & published at ESG (Gary Strand) Ongoing projects: CVWG webpage, or contact Adam Phillips

Frankignoul and Hasselmann (1977) …… Obs Mechanism of PDO Atmospheric noise? Hasselmann (1976) Frankignoul and Hasselmann (1977) …… Atm-ocn coupled mode? Latif and Barnett (1994, 1996) Neelin and Weng (1999) Kwon and Deser (2006) Atm response to the decadal SST anomalies? CCSM3 Alexander et al. (2006): PDO lacks connections to the Tropics in CCSM3 The mechanism of the decadal SST variability is important for decadal climate prediction. http://www.jisao.washington.edu/pdo/

0-300m annual mean ocean temperature at 140°E-200°E, 40°N-50°N

monthly 10-20yr filtered SST from 900-yr CCSM3 T42 PDcntrl run Complex EOF Analysis monthly 10-20yr filtered SST from 900-yr CCSM3 T42 PDcntrl run CEOF1(40%) amplitude 180° phase ~ 70 episodes -180°

Probability density function of the PDO phase in the 30 members

SLP/SST composite based on CEOF temporal phase  (~70 cases)

Ocean Temp at 40°N: Composite (shading) & Climatology (contour)

Upper 300m ocn TEMP composite based on CEOF temporal phase 

Ocean top 300 m heat budget T+1- T T/t = - V·T +w_adv@300m+ Sur_flx phase T+1- T -180° -150° -120° -90° -60° -30°

300m/curl() composite based on CEOF temporal phase  (~70 cases)

Summary Some decadal predictability is suggested in the first ten years in the large ensemble experiment The decadal ocean temperature anomalies are mainly caused by horizontal temperature advection and surface heat flux. The deep ocean doesn’t play an active role. The air-sea coupling needs to be further studied.