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

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WES: Atlantic Response Role of the WES Feedback: • Regression of April-May-June surface specific humidity on the ENSO January index for CCM3-SOM- ENSO and WES-off-ENSO runs. • Less cross-equatorial transport of moisture in the absence of WES feedback 06-19-2008 CCSM Workshop 2008 to ENSO CCM3-SOM-ENSO WES-off-ENSO
WES: Atlantic Response Role of the WES Feedback: ITCZ response 06-19-2008 CCSM Workshop 2008 to ENSO • Regression of April-May-June precipitation on the ENSO January index for CCM3-SOM-ENSO and WES-off-ENSO runs. • Subsidence during El-Nino events • Northward movement of the ITCZ during El-Nino events only in the presence of WES feedback CCM3-SOM-ENSO WES-off-ENSO
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 and 10: Tropical Atlantic Variability 06-19
Page 11 and 12: Annual Cycle of SST and LHFLX SST E
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: WES: Atlantic Response Role of the

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

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