The evaporative, conductive and
radiative processes combined then set up a thermal gradient causing an upward flow of energy from water to air from where that 1 mm layer touches the ocean bulk below, up across the cooler layer then to the Knudsen layer by reversing the normal (warm at the top and cool at the bottom) temperature gradient which exists from that 1 mm layer down to the ocean bottom.
Not exact matches
Don't climate models break the Earth (mostly atmosphere) into billions of small volumes, each of which has a density, temp, humidity,
radiative flux, albedo etc. and then isn't a climate simulation the
process of
combining the behavior of these billions of volumes to simulate large scale phenomena?
We can not measure total
radiative forcing, with or without temperature feedbacks, because
radiative and non-
radiative atmospheric transfer
processes combined with seasonal, latitudinal, and altitudinal variabilities defeat all attempts at reliable measurement.