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

More documents

Recommendations

Info

Heat Flux Bulk Formulations: LH Flux = u*(q s- q*)B SH Flux = u*(T s-T*)D Experimental Set-up SST u* = reference height w ind speed q* = specific humidity at reference height qs = specific humidity at surface T* = Temperature at reference height Ts = Temperature at surface B, D: Bulk Coefficients WES off: Prescribe u* while computing Fluxes 06-19-2008 CCSM Workshop 2008 + WIND EVAPORATION
Experimental Set-up Experiment Set 1: To understand the variability associated with WES feedback Control Run: 80 years WES-off-SOM Run: 80 years Experiment Set 2: To study the Equatorial Annual Cycle WES-off-NoANN Run: 40 years • u* prescribed as annual mean, no seasonal cycle 06-19-2008 CCSM Workshop 2008
Page 1 and 2: The Role of the Wind-Evaporation-Se
Page 3 and 4: Role of WES Feedback The WES feedba
Page 5: Mechanistic Experiments SST CCM3-SO
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 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

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?