The greenhouse effect analogy of global warming is that atmospheric carbon dioxide CO$_2$ absorbs some of the infrared radiation emitted by the Earth, and redirects a portion of that radiation back down to the Earth's surface, thereby heating the surface more than it would have done if that radiation had been able to escape into space.

Global warming is then simplistically explained to the general public by the idea that as atmospheric CO$_2$ concentrations rise, more infrared radiation is absorbed by CO$_2$ and re-emitted back down to Earth, causing increased heating of the Earth.

However, this explanation is not technically correct, because at present atmospheric CO$_2$ concentrations, just one kilometer of atmosphere is sufficient to fully absorb all the infrared radiation emitted by the Earth, at the wavelengths at which CO$_2$ absorbs.

Carbon dioxide absorbs infrared at the wavelengths of 2.7, 4.3 and 15 µm, and the CO$_2$ in the first kilometer of atmosphere alone is able to completely absorb all infrared at these wavelengths.

So the infrared absorption process is already fully saturated, and thus further increases in atmospheric CO$_2$ will not lead to any additional absorption. This is why the simplistic explanation provided for the general public does not seem to be technically correct, even though it roughly outlines the idea.

I found one blog article by Clive Best that tries to explain the actual process behind CO$_2$'s ability to cause global warming. Judging from that article, the actual process is more complex than the simple explanation provided for public consumption. However, I don't fully understand the explanation given in the article (and from what I did manage to understand, I am not sure if it is fully correct).

So I wonder if anyone here can provide an easy to understand explanation of the actual mechanism by which increased atmospheric CO$_2$ leads to global warming. Or perhaps if you know any good articles that explain it, please can you post the links.

I tried to find some info on the actual mechanism of global warming via Google, by using search terms such as "mechanism of greenhouse effect in global warming", but was surprised to find very little information available.

I also asked this question on physics.stackexchange.com here.

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    $\begingroup$ The explanation, while it may be simplified, is not "simplistic". (You might consider entertaining the idea that you've made a mistake in your math.) For a basic explanation, start here: history.aip.org/climate/index.htm If you want to go deeper, consider a text on climate physics such as Ray Pierrehumbert's "Principles of Planetary Climate". $\endgroup$ – jamesqf Jan 16 at 19:21
  • $\begingroup$ @jamesqf, the explanation provided to the general public is simplistic: it's a reduced complexity explanation. Whereas there is nothing wrong with giving a simplified explanation: that's always desirable. $\endgroup$ – Hip89 Jan 16 at 20:11
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    $\begingroup$ @ebv, surely you must realize that when complex physics is involved, that excludes most of the population from properly understanding it. I have degree in physics, so I am hoping to be able to understand the mechanism of global warming. But don't expect your average person in the street to understand. $\endgroup$ – Hip89 Jan 17 at 13:20
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    $\begingroup$ There is an excellent blog article by Spencer Weart realclimate.org/index.php/archives/2007/06/… that explains why the saturation at the surface argument is incorrect. It is energy balance at the top of the atmosphere that determines whether the planet warms or cools, the absorption at the surface is largely irrelevant. $\endgroup$ – Dikran Marsupial Jan 17 at 15:04
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    $\begingroup$ BTW I would be wary of Clive Bests blog. He is a very bright chap, but tends to be resistant to correction/criticism. Being clever is not a substitute for experience and research, you'll just make the same mistakes that climatologists made 30 years ago all over again. They were clever people as well! ;o) $\endgroup$ – Dikran Marsupial Jan 17 at 15:15

Borrowing an explanation from one of my other answers, the basic mechanism of the greenhouse effect is roughly as follows (note this is also a simplified model)

The Earth is in (to all intents and purposes) a vacuum, so it can only gain or lose heat via radiation. The sun emits most of its radiation at visible and UV wavelengths. The Earth's atmosphere is fairly transparent at these wavelengths and so the Sun's radiation mostly passes through it and hits the surface. Some of this radiation (determined by the Earth's albedo) is reflected from the surface back out into space, but the rest is absorbed by the surface, which causes the surface to be warm. The surface loses heat by radiating in infra-red wavelengths. Greenhouse gases absorb some of the IR radiation, which causes the atmosphere to warm up (the GHG molecules transfer some of this heat to non-greenhouse gasses by collisions, but heat is also transferred upwards by convection). The warm atmosphere re-radiates some of this energy both upwards into space and downwards back to the surface. The part that is radiated downwards is also known as "back-radiation" (and is directly observable). Now the important factor is not the amount of outbound IR radiated from the surface that is absorbed, but the altitude at which there are not enough greenhouse gases above to absorb the IR radiated upwards from that layer, so that it can escape out into space. The lapse rate means that the temperature of the atmosphere decreases with increasing height. This means that the more CO2 we put into the atmosphere, the higher this emitting layer becomes, and the colder it is. As the amount of IR radiated depends on the temperature of this layer, if this height increases then the amount of IR radiated from the planet falls, leading to an energy imbalance, with the planet absorbing more of the sun's radiation than it emits as IR, and so the planet warms up. This continues until the radiating layer warms up enough for the outbound IR to be in balance with the incoming radiation from the sun. So the more CO2, the warmer the mean surface temperature, all things being otherwise equal.

Thus it is irrelevant that most IR emitted by the surface is absorbed by the atmosphere, it is the height from which IR is not absorbed that matters. If it is colder than the surface, it will emit less IR than the surface is emitting and hence less energy is radiated into space.

For a more detailed explanation of why absorption at the surface is of little relevance, see this RealClimate article by Spencer Weart.

Just to add a historical note, this explanation goes back at least as far as Ekholm's paper of 1901 "On The Variations Of The Climate Of The Geological And Historical Past And Their Causes":

The atmosphere plays a very important part of a double character as to the temperature at the earth’s surface, of which the one was first pointed out by Fourier, the other by Tyndall. Firstly, the atmosphere may act like the glass of a green-house, letting through the light rays of the sun relatively easily, and absorbing a great part of the dark rays emitted from the ground, and it thereby may raise the mean temperature of the earth’s surface. Secondly, the atmosphere acts as a heat store placed between the relatively warm ground and the cold space, and thereby lessens in a high degree the annual, diurnal, and local variations of the temperature.

There are two qualities of the atmosphere that produce these effects. The one is that the temperature of the atmosphere generally decreases with the height above the ground or the sea-level, owing partly to the dynamical heating of descending air currents and the dynamical cooling of ascending ones, as is explained in the mechanical theory of heat. The other is that the atmosphere, absorbing but little of the insolation and the most of the radiation from the ground, receives a considerable part of its heat store from the ground by means of radiation, contact, convection, and conduction, whereas the earth’s surface is heated principally by direct radiation from the sun through the transparent air.

It follows from this that the radiation from the earth into space does not go on directly from the ground, but on the average from a layer of the atmosphere having a considerable height above sea-level. The height of that layer depends on the thermal quality of the atmosphere, and will vary with that quality. The greater is the absorbing power of the air for heat rays emitted from the ground, the higher will that layer be, But the higher the layer, the lower is its temperature relatively to that of the ground ; and as the radiation from the layer into space is the less the lower its temperature is, it follows that the ground will be hotter the higher the radiating layer is.”

[Ekholm, 1901, p19-20]

(h/t Steve Easterbrook's blog article)

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  • $\begingroup$ This is very interesting, thank you! If I may ask, could you please clarify the statement "the more CO2 we put into the atmosphere, the higher this emitting layer becomes"? Why does an increased concentration of CO2 move the upper boundary of the layer higher up? And is the change in concentration of CO2 quantitatively consistent with a significant change in this layer's thickness? I'm asking because I was talking about this at work with some colleagues today, and one of them argued that there is no evidence that reducing CO2 emissions will improve anything, which baffled me a lot. $\endgroup$ – user6376297 Jan 17 at 17:56
  • $\begingroup$ Thank you very much for your answer, @Dikran Marsupial. I am starting to get the picture, but I am still struggling to intuitively understand your statement: "If it is colder than the surface, it will emit less IR than the surface is emitting and hence less energy is radiated into space." Because if the heat is being transported up to a higher layer in the atmosphere before departing as radiation into space, wouldn't the heat just increase the temperature of that higher layer, until such time as its radiant output to space is in equilibrium with the heat energy input to that higher layer? $\endgroup$ – Hip89 Jan 17 at 18:05
  • $\begingroup$ @user6376297 CO2 is "well mixed" in the atmosphere, so if we add more CO2 to the atmosphere, there will be more CO2 above the old effective radiating layer and it will absorb some of the IR emitted from that layer. This means that on average, more of the IR that escapes will be from slightly higher in the atmosphere than before. There isn't really an identifiable layer, in reality there is a distribution of heights from which IR escapes to space, but adding CO2 shifts the distribution a bit higher. $\endgroup$ – Dikran Marsupial Jan 17 at 18:19
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    $\begingroup$ The atmosphere isn't any taller, it is just the height at which IR radiation can escape into space without being absorbed by greenhouse gasses rises. AIUI most of the heat transfer within the atmosphere is by convection rather than conduction or radiation, and it is that that sets up the lapse rate (the decrease in temperature with increasing height). Because there is a lapse rate, if you want the upper atmosphere to warm, you need the surface to warm as well. $\endgroup$ – Dikran Marsupial Jan 18 at 15:06
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    $\begingroup$ FYI, here is a post from SE\physics that seems related to what is being discussed here. I confess that I scrolled to the bottom, skipping all the equations... and unfortunately I couldn't understand the conclusion :( $\endgroup$ – user6376297 Jan 18 at 18:23

CO2 is dark in the longwave infra red wavelenght so the higher the consentration is the darker the atmosphere will be in this wavelenght.and as you probably know darker colours absorb more heat.

CO2 is not a very powerful greenhouse gas but the amount of it in our atmosphere make this effect the dominating source for the heating we can see today.

Lots of other gases have a larger heating potential than CO2 but their consentration is low at the moment,The more complex a gas is the more heating potential it will have this is due to the size of the individual gas molecules(CO2 have 3 molecules and methane have 5 so it will look darker in the long wave infra red band and therefor have a stronger heating potential).

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    $\begingroup$ I don't think this answers the question. $\endgroup$ – Semidiurnal Simon Jan 19 at 21:25

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