The role of wind-evaporation-SST feedback in tropical variability
The role of wind-evaporation-SST feedback in tropical variability
The role of wind-evaporation-SST feedback in tropical variability
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WES Feedback and <strong>SST</strong><br />
Anomaly Propagation<br />
Strong seasonal cycle <strong>in</strong> the E.Pacific because <strong>of</strong> shallow mixed<br />
layer<br />
<strong>SST</strong> anomalies propagate westward<br />
Control Run<br />
<strong>SST</strong> Anomaly<br />
Longitude Longitude<br />
06-19-2008 CCSM Workshop 2008