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This question already has an answer here:

I had a question in my school exam. Will the average surface temperature of the Earth be lower or higher, if there was no atmosphere?

Now, the answer expected is "The avg temp will be lower, because of no greenhouse effect."

Isn't this an extremely myopic view of the whole situation? Places where it's night, the temperature will be sub-zero, and places where it's daytime, the temperature will be unbearably high, somewhat like on the moon, right? So the thing is, what's the correct answer? I know my education board is not something to be trusted, so please don't worry about their answer.

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marked as duplicate by John Rennie, David Hammen, ACuriousMind, JamalS, Kyle Kanos Mar 5 '15 at 1:30

This question has been asked before and already has an answer. If those answers do not fully address your question, please ask a new question.

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    $\begingroup$ possible duplicate of Do greenhouse gasses make the world habitable? $\endgroup$ – John Rennie Mar 4 '15 at 15:19
  • $\begingroup$ This is an extremely complex question, because the behavior of the atmosphere is extremely complex. There are a couple of “effects” of the atmosphere I can think from the top of my head: * the greenhouse effect you have mentioned, which heats the planet * the reduced thermal amplitude, which also, on average, heats the planet The last point comes from the fact that, in a simplistic gray-body model, thermal equilibrium fixes the average of T⁴. With this constraint, the greater the thermal amplitude, the lower the average temperature. I certainly have missed many other effects... $\endgroup$ – Edgar Bonet Mar 4 '15 at 15:25
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    $\begingroup$ Without an atmosphere the equilibrium temperature the Earth would be at due just to the sun's luminosity would freeze the oceans. The atmosphere clearly has a heating effect. $\endgroup$ – NeutronStar Mar 4 '15 at 15:31
  • $\begingroup$ See also Earth Science Stack Exchange. $\endgroup$ – gerrit Mar 4 '15 at 15:48
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It is actually very easy to consider this. We don't need any models. we are blessed with a sizable rock at exactly 1 AU from the Sun, a rock with no trace of any atmosphere at all:

Moon
Moon (Source: Wikimedia Commons)

Temperatures on the moon vary from 70K to 390K. Average temperatures, depending on location, vary from 130K at the poles to 220K at the equator (through Wikipedia). Note that due to non-linearities, this is not the same as the equilibrium temperature (255K on Earth). Indeed, as Edgat Bonet points out in his answer, for the same equilibrium temperature, average temperatures will be lower if thermal amplitudes are higher. And they couldn't be much higher than they are on the moon, with its long days and complete lack of atmosphere.

So, something that is different between Earth and Moon causes the Moon to be a lot colder. The most obvious difference is the lack of an atmosphere. In principle, the lack of oceans and clouds and trees also contributes, but since none of those can exist without an atmosphere, it is clear that a planet with an atmosphere is hotter than the same planet without — through both direct and indirect effects.

Note that the lack of the atmosphere is not the only difference between the Earth and the moon. There is internal heat generation, tidal heating, and many other effects. None of those effects come close to the effect of the atmosphere for heating the Earth.

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  • $\begingroup$ Why would you ignore the fact that the moon is a dead rock but the Earth has a lively :-) core full of radioactivity and hot stuff? For example, Iceland is warm on account of hot springs and whatnot. $\endgroup$ – Carl Witthoft Mar 4 '15 at 16:47
  • $\begingroup$ @CarlWitthoft Because that heat source is only on the order of 0.1 W/m². I did not say that the lack of the atmosphere is the only difference. Earth is also heated from inside, by tidal heating, directly by humans, by meteorites entering, by sunlight reflected from the moon, and probably by other factors that are even smaller. All of the above have an effect that is tiny compared to the effect of the atmosphere. $\endgroup$ – gerrit Mar 4 '15 at 17:32
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Simple black body radiation theory (adapted from http://www.atmos.washington.edu/2002Q4/211/notes_greenhouse.html):

The earth receives a certain amount of heat per unit area from the sun - this amount is about 1370 W/m$^2$ for parts of the earth facing the sun when there is no atmosphere. But the earth presents a "disk" with area $\pi R^2$ to the sun, when it is in fact a sphere with an area of $4\pi R^2$. This means that on average the power received per unit area over 24 hours is 1/4 of that, or about 340 W.

Now some of the sun's power is reflected by earth - about 30%. The power left to get rid of by "gray body radiation" is about 240 W/m$^2$.

Using Stefan-Boltmann, with again an emissivity of 0.7, we solve for the "equivalent" temperature of Earth:

$$\Phi = \epsilon \sigma T^4\\ 240 = 0.7 \cdot 5.67 \cdot 10^{-8} T^4\\ T = 278 K$$

If you ignore the emissivity, the value would be even lower - 255 K. This is well below the temperature of Earth (mean value 288 K), suggesting that the atmosphere is indeed helping keep the temperature up. The effect of the atmosphere on surface temperature is much more extreme on Venus (100's of degrees K), where the layer of carbon dioxide is very thick.

Of course all kinds of simplifying assumptions went into the above. For example, the poles will be significantly colder when there is no atmospheric convection to bring heat from the lower latitudes - and the temperature fluctuations between day and night could be enormous. The hotter surface during the day will emit relatively more power (because of that 4th power) so the mean would be lower than the "effective" temperature I calculated above. Either way - the atmosphere absorbs more strongly in the IR than in the visible, and this means that it is easier for sunlight to get in, than for emitted thermal radiation to get out. This helps keep the planet warm. Your school board, in this case, had the right answer.

But the bottom line is - the atmosphere makes earth livable. Changing the composition will change the conditions on earth. But the balance is precarious. Let's not disturb it if we can help it.

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  • $\begingroup$ That is the equivalent temperature (balancing the T⁴s), not the average temperature. $\endgroup$ – gerrit Mar 4 '15 at 23:18
  • $\begingroup$ @gerrit you are right. I intended to imply this with the statement "the mean temperature would be lower" but maybe it got buried. I edited to make the distinction clearer. $\endgroup$ – Floris Mar 4 '15 at 23:46

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