The role of wind-evaporation-SST feedback in tropical variability

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WES Feedback and SST Anomaly Propagation Strong seasonal cycle in the E.Pacific because of shallow mixed layer SST anomalies propagate westward Control Run SST Anomaly Longitude Longitude 06-19-2008 CCSM Workshop 2008
Annual Cycle of SST and LHFLX SST Equatorial Pacific (2S-2N) LHFLX 06-19-2008 Control CCSM Run Workshop 2008 WES-off-SOM Run
Page 1 and 2: The Role of the Wind-Evaporation-Se
Page 3 and 4: Role of WES Feedback The WES feedba
Page 5 and 6: Mechanistic Experiments SST CCM3-SO
Page 7 and 8: Experimental Set-up Experiment Set
Page 9: Tropical Atlantic Variability 06-19
Page 13 and 14: Experiment Set 4: 06-19-2008 CCSM W
Page 15 and 16: Tropical Response to High Latitude
Page 17 and 18: 06-19-2008 CCSM Workshop 2008 Intro
Page 19 and 20: Spring Season CCM3 Runs: Mean State
Page 21 and 22: Seasonal Cycle of SST, q over Equat
Page 23 and 24: 1. ITCZ Asymmetry: Introduction: Ro
Page 25 and 26: PC analysis (Ruiz-Barrados et al.,
Page 27 and 28: Traditional Approach: 06-19-2008 CC
Page 29 and 30: Change in the variability of Precip
Page 31 and 32: WES: Tropical Response to High Lati
Page 33 and 34: WES: Tropical Response to High Lati
Page 35 and 36: WES: Atlantic Response ENSO Respons
Page 37 and 38: WES: Atlantic Response Atlantic Res
Page 39 and 40: WES: Atlantic Response Partitioning
Page 41 and 42: WES: Atlantic Response Role of the
Page 43: WES: Atlantic Response Role of the

The role of wind-evaporation-SST feedback in tropical variability

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