EVAPORATION AND SOLAR IRRADIANCE AS REGULATORS OF SEA-SURFACE TEMPERATURE IN ANNUAL AND INTERANNUAL CHANGES

Seven years of net surface solar irradiance (S) derived from cloud inf ormation provided by the International Satellite Cloud Climatology Pro ject and 4 years of surface latent heat flux (E) derived from observat ions of the special sensor microwave imager were used to examine the r elation between surface heat fluxes and sea surface temperature (T(s)) in their global geographical distribution, seasonal cycle, and intera nnual variation. The relations of seasonal changes imply that evaporat ion cooling is significant over most of the ocean and that solar heati ng is the main drive for the change of T(s) away from the equatorial w ave guide where ocean dynamics may be more important. However, T(s) is not the most direct and significant factor in the seasonal changes of S and E over most of the ocean; the solar incident angle may be more important to S, and wind speed and air humidity are found to correlate better with E. Significant local correlations between anomalies of T( s) and S and between anomalies of T(s) and E are found in the central equatorial Pacific; both types of correlation are negative. In this ar ea, organized deep convection overlies the warm ocean, forms high clou ds, and reduces S, while the low wind speed and high humidity that res ult from surface convergence reduce E. The negative correlation is not present in the surrounding areas where equally warm water and strong T(s) anomalies are found under a subsiding atmosphere without similarl y strong S and E anomalies. Correlation between anomalies of temperatu re tendency and the fluxes is weak, indicating that other factors are more influential in changing upper ocean heat balance during El Nino. The result shows that the relations between T(s) and the flux componen ts, in annual and interannual timescales, are not universal and not co nsistent with the local negative feedback postulations which require t hat an increase in T(s) would result in an increase in local evaporati ve cooling and a decrease in local solar heating of the ocean. Large-s cale atmospheric circulation changes clouds, winds, and humidity; they , in turn, influence the fluxes significantly. The influence of ocean dynamics in changing T(s) in the tropical ocean can not be ignored.