After the discussion about warm or cold water freezing faster terminated in post 955...
I'm not sure why you're doing this, I've told you the context of the question, the context of the question is the discussion between Andre and myself of the validity of using the stefan boltzman law to derive an equilibrium temperature and what that tells us about the greenhouse effect.
...then for the next 23 consecutive posts (but with a few brief comment posts interspersed) concerned with some aspect of the GH effect. Including in posts words like: atmosphere, clear sky, IR gases, & their absorption as function of wave length, etc.)
Right. Andre proposed we consider the scenario of an atmosphere that is transparent to IR radiation. This scenario has been doing the rounds in a number of blogs run by people opposed to the idea of anthropogenic global warming, and I would like to get back to it, but, you're single handedly derailing that discussion. That is where the discussion started, but, the discussion has moved on since then, it has evolved, we're now talking about a very specific, very important piece of that scenario. First we need to agree on how much energy is intercepted. Then we need to agree on how much of that intercepted energy is absorbed. Then we can begin to discuss what happens to that energy once it has been absorbed. Do you get it yet?
After an initial typos Trippy re-state his question here: Trippy asserts the solar energy given to each* is the same, but I have disagreed as problem is not just one of how much flux fails to continues its original path into space, but one of the relative absorption vs. reflection (or scattering).
Yes and no. These are considerations in the Stefan Boltzman equation, but they're not relevant to the discussion because the disc and the sphere have identical properties. That's the point. I was making sure that Andre and I were in agreement on the total flux intercepted by the earth, and the treatment of that, before I moved onto more complicated questions like how much of this is absorbed, scattered, or reflected.
At first I assumed that both had atmospheres, due to the 23 prior posts discussing that, but soon Trippy made it clear he was assuming bare disk and sphere. I continued to assume the real sun, 0.5degrees wide at 1AU and realistic absorption coefficient decreasing greatly as the light ray's angle from normal incidence approached 90 degrees. This obviously means the sphere absorbs less energy than the disk does.
In otherwords, this is because you have failed to keep up with the discussion. I've given you the correct context of the question - Andre and I were discussing the Stefan Boltzman law and the relevance of equilibrium temperature in discussions of global warming. Calculating the equilibrium temperature requires knowledge of how much flux is intercepted by the object as well as knowledge of how much of that energy is absorbed or reflected - IE the albedo of the object. I was making sure we agreed on the very first step before we moved on.
I noted however that if the sun angle from the disk normal is not fixed at zero because the sun appears to rotate around the disk like it does around the Earth, then the opposite is true as the sunlight is always falling normally on some part of the sphere. Trippy then clarified that we were to assume the sun remained normal to some point on both sphere and disk.
As I have stated repeatedly the context of the discussion is the stefan boltzman equation and the equilibrium temperature.
I, and I think Trippy too, assume that both are geometrically perfect. I. e. no tiny hills, etc. but are smooth at least on the scale of light wave lengths (and of course are completely opaque.)
I still complain that the word “intercept” is troublesome when speaking of “energy intercepted.”An aluminum sphere “intercepts” (gets in the way of) the same flux as a carbon one of same diameter does but scatters most of it back into space instead of absorbs most of its energy as the carbon sphere does.
You've confused yourself, and you're confusing the conversation. Here you're talking about Albedo, which is a consideration in the calculation of the equilibrium temperature, but not directly related to the question asked. The disc and the sphere have the same properties. The first step of calculating the equilibrium temperature is to calculate the total flux absorbed which is dependent on the total flux intercepted and the albedo. The total power striking an objects surface is proportional to its cross sectional area and its distance from the emitting body - this is why a sphere and a disc with identical properties intercept and absorb the same amount of total energy, because they have they same cross-sectional area. The disc is the cross-section of the sphere.
Thus with Trippy's clarified assumptions (The 0.5 degree wide real sun, 1AU from Earth diameter disk and sphere always remaining stationary on the axis of the disk) Then the answer to the question is that the disk absorbs much more energy (intercepts more energy in spite of getting in the way of the same amount)* than the sphere does due to the rapid decrease in absorption coefficient with increasing angle of incidence as the spot the sunlight is falling on approaches the polar regions of the sphere.
No, if they have identical properties, they intercept and absorb identical amounts of
total energy. We're talking about total energy integrated across the whole body, not the energy at the surface at a specific location. As I keep saying to you, you're considering the energy distribution across the surface not the total energy absorbed by the body.
* The thread's subject is about the solar energy absorbed, not about how effectively an energy flux is blocked from continuing its original path. In post 993, Trippy seems to agree that we are concerned about energy absorbed, not just blocked from continuing its original path:
First rule of holes. Stop digging. Andre and I were taking the same approach, taking the discussion back to the last thing we could agree on. As a consequence, we've gone right back to the Stefan-Boltzman law, and I was attempting to make sure that Andre agreed on the calculation of the total power absorbed at the surface. In order to calculate the total energy absorbed by an object that is radiatively heated we first need to know how much total energy is blocked by the object. The energy absorbed is a fraction of the energy blocked, the rest is reflected, however, before we can discuss how much is absorbed or reflected at specific locations on the surface, and then finally how that energy is redistributed accross the entire surface.
The simple fact of the matter is that the equation for calculating the power emitted by the sun is $$P_{Semt} = 4\pi R^2_s \sigma T^4_s$$ and the power intercepted by the earth is $$P_{SE} = P_{S emt}\frac{\pi R^2_e}{4\pi D^2}$$ in other words, it's the total power emitted by the sun multiplied by the cross sectional area of the earth as a fraction of the area of a sphere with a radius of 1AU because a disc and a sphere with identical properties absorb the same amount of total power because the total power is proportional to the cross sectional area of the sphere which is the same as the surface area of the disc.