To determine the location of a star's habitable zone, one must first learn how much
total radiation it emits.
Under steady - state conditions, the total radiation absorbed by the Earth must match
the total radiation emitted by the Earth; that's what radiative balance or imbalance means in the climate literature.
Not exact matches
Although only 1 percent of the sun's energy is
emitted at ultraviolet wavelengths between 200 and 300 nanometers, the decrease in this
radiation from 1 July 1981 to 30 June 1985 accounted for 19 percent of the decrease in the
total irradiance over the same period.»
Eventually the surface reaches a point where it
emits enough IR that the half making it out into space balance the
total amount of incoming SW and LW
radiation.
Each higher and cooler layer in turn
emits thermal
radiation corresponding to its temperature; and much of that also escapes directly to space around the absorption bands of the higher atmosphere layers; and so on; so that the
total LWIR emission from the earth should then be a composite of roughly BB spectra but with source temepratures ranging ove the entire surface Temeprature range, as well as the range of atmospheric
emitting Temperatures.
Thus, long - term variations of TSI (with account for their direct and secondary, based on feedback effects, influence) are the main fundamental cause of climate changes since variations of the Earth climate is mainly determined by a long - term imbalance between the energy of solar
radiation entering the upper layers of the Earth's atmosphere and the
total energy
emitted from the Earth back to space.»
Prof Claes Johnson (see Computational Blackbody
Radiation) and I are in
total agreement as to the reason being that blackbodies do not convert the energy in
radiation that was
emitted spontaneously by a cooler source than their own temperature.
You can not measure
total incident or
emitted radiation with any instrument known to man.
The first shell will recieve 235w / m2 and heat to some temperature where it will
emit a
total of
radiation that will keep it in equilibrium with the surroundings.
The shell will still have to
emit the
total radiation of the planet to space, but the planet will not be warmed as much by the
radiation of the shell.
It is assumed that all the solar
radiation from relevant absorption band makes it to the CO2 boxes through all the other boxes and does this constantly with no loss and if it did the model might be correct, as it is there are tens of thousands of other boxes between each CO2 box so the absorption and the storing and the re
emitting of this narrow band can not be
total or anywhere near
total and the incoming source is not constant nor does all all the solar
radiation actually make it the CO2 boxes, it would only be a proportion the rest being intercepted and dissipated beforehand.
The
total radiation leaving one side of the layer is the external
radiation reflected back by the interface,
radiation emitted internally by the layer and transmitted through the interface,
radiation scattered by sites inside the layer and transmitted through the interface, and
radiation transmitted through the layer from the surroundings on the opposite side.
Total internal reflection of scattered and internally
emitted radiation affects the
radiation leaving the layer and the temperature profile.
-- Yes, it may be correct in so far as they can say that; «around 10 % of the wavebands
emitted by IR
radiation are made up of wave - lengths that can not be absorbed by «Greenhouse Gases» (GHGs), but that can not possibly mean that 0.04 %, in the case of CO2 concentration but certainly less than 10 % of the Atmosphere as a
total has got what must be a «supernatural» ability to stop LWR.
This is because some of the gases absorb and
emit radiation at the same frequencies as others, so that the
total greenhouse effect is not simply the sum of the influence of each gas.
The right side is
total absorbed solar
radiation — upward
emitted atmospheric
radiation.
If that «aperure» surface, happens to be a real planar aperture in the thermally impenetrable wall of the cavity, then
radiation will be
emitted from that aperture in the same cosice (Lambertian) pattern, and the
total emitted energy, will simply be pi times the axial intensity (normal to the aperture).
First, the quote is not dealing with what the result of reabsorbing its own
radiation is but how to calculate the
total emitted power of a body with a complex shape.
It clearly shows that the
total emitted radiation from the surface is 38.9 MJ while the
total solar absorbed over the same period is 24.0 MJ.