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T he ocean surface heat budget comprises radiative and turbulent components: the radiative components are solar shortwave and thermal longwave, both of which are strongly affected by cloud; the turbulent heat flux components are the direct transfer of sensible heat and the evaporative transfer of latent heat. Although direct measurements of the turbulent fluxes are possible, they remain a research activity due to the high cost of the measurements. Measurement of the radiative components isdoi:10.1175/2008bams2639.1 fatcat:cih4e5zcvbfhzn2gkzxhkuvjgy