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  • Air–Sea Interactions from the Diurnal to the Intraseasonal during the PISTON, MISOBOB, and CAMP2Ex Observational Campaigns in the Tropics x
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Simon P. de Szoeke

situ are important for validating sea surface temperature (SST) retrievals ( Emery et al. 2001 ; Donlon et al. 2002 ; Gentemann et al. 2003 ). Accurate SST measurements are also critical for modeling surface turbulent sensible and latent heat flux with bulk aerodynamic formulas ( Fairall et al. 1996a , b ). The warm layer has a strong effect on the bulk fluxes where differences between SST and air temperature are small. Interactions between the ocean, atmosphere, and surrounding land in the Bay

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