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Ocean-Atmospheric Response to North Pacific Wind Stress Forcing: A Coupled Perspective. Lixin Wu Physical Oceanography Laboratory Ocean University of China Qingdao, China. Collaborators: Chun Li and Liping Zhang, Ocean University of China
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Ocean-AtmosphericResponse to North Pacific Wind Stress Forcing: A Coupled Perspective Lixin Wu Physical Oceanography Laboratory Ocean University of China Qingdao, China Collaborators: Chun Li and Liping Zhang, Ocean University of China Zhengyu Liu, University of Wisconsin-Madison
Wind and SLP 77-88 and 71-76 Deser et al. (1996, J Climate)
SST and Surface wind Curl>0 Westerly Curl<0 76/77 Easterly Curl<0 Curl>0
KOE SST and NPI WSP SST and NPI SST Lead NPI Lead
After shift Curl<0 Prior to shift Curl>0 Possible Mechanism for mid-70s Climate Shift 40oN 30oN Wu, Lee and Liu (2005, J. Climate)
R Green-Function Approach
FOAM OGCM Simulation Ocean Current upper 500m SST anomaly Mean Anomaly
FOAM Coupled Heat flux SST Heat flux and surface wind
FC: Current Anomalies upper 500m Ocean Current upper 500m Current Diff of FC&PCG PCG: Ocean Current Anomalies upper 500m 1cm/s
1m/s NDJ JFM MAM MJJ
STC: Subtropical-tropical Cell PCG-STC anomaly FC-STC anomaly
Z850 Z250 PC-TP JFM JAS
Rossby Cooling WES Cooling STC Summary for coupled adjustment NP EQ WES-STC Relay Teleconnection Wu et al. (2007, Clim. Dyn.)
Discussions: Understanding Coupled O/A interaction over the Midlatitudes 1. Modeling Methodology Roadmap: AGCM+SSTAGCM_ML+HF CGCM+ IV CGCM +WindStress 2. Timescale Interaction: mean/ synoptic/ season/interannual/decadal 3. Spatial-scale Interaction: Frontal vs. Basin scale 4. Local/Remote interaction: Tropics, North Atlantic etc.
North Atlantic-North Pacific: Resonance Li and Wu (2009, Climate Dynamics, in press)