He uses Kirchhoff's law and the two energy balances (ground to lower atmosphere, upper atmosphere to space) to derive the result: The long
wave upward radiation from the surface is limited to 1.5 times the short wave downward radiation from the Sun.
Not exact matches
This quantity represents the difference in the intensity of the long - and short -
wave infrared
radiation at these two wavelengths that travels
upward from the atmosphere to the satellite, and it is traditionally used to differentiate between water and ice clouds.
The internal kinetic energy is taken as the
upward long
wave energy flux at the top of the atmosphere, and the potential energy is the
upward radiation flux from the surface.
There is: we can measure the wavelengths of long -
wave radiation leaving the Earth (
upward radiation).
We can examine the spectrum of
upward long -
wave radiation in 1970 and 1997 to see if there are changes.
For instance, when the long
wave radiation from the upper few micrometers of the ocean is
upward, the skin temperature is usually cooler than the bulk SST.Latent and sensible heat fluxes can cool the sea surface further if the air is dryer or colder.
The partition of the outgoing long
wave radiation into
upward atmospheric emittance and surface transmitted
radiation components is based on the accurate computation of the true greenhouse - gas optical thickness for the radiosonde data.