
We’re heading out of this world for today’s post, to examine the atmospheric compositions of the other planets in the solar system, as well as our own. Practically every other planet in our solar system can be considered to have an atmosphere, apart from perhaps the extremely thin, transient atmosphere of Mercury, with the compositions varying from planet to planet. Different conditions on different planets can also give rise to particular effects.
Mercury
Mercury doesn’t really have an atmosphere in the strictest sense of the word – its incredibly thin atmosphere is estimated to be over a trillion times thinner than Earth’s. Its gravity is about 38% that of Earth, so it isn’t capable of retaining much of an atmosphere, and in addition, its proximity to the sun means that the solar wind can carry gases away from the surface. Particles from the solar wind, coupled with the vapourisation of surface rock as a result of meteor impacts, are probably the largest contributors to Mercury’s atmosphere.
Venus
Venus is similar to Earth in several respects: its density, size, mass, and volume are all comparable. The atmosphere is where the similarities end, however. The atmospheric pressure is around 92 times that found at sea level on Earth, with the main gas being carbon dioxide – the result of previous volcanic eruptions on the planet’s surface. Higher in the atmosphere, the planet also has clouds which are a mixture of sulfur dioxide and sulfuric acid. There is a thick layer of carbon dioxide below these clouds, which subjects the surface of the planet to an intense greenhouse effect. Surface temperature on Venus is around 480˚C – much too hot to sustain life as we know it.
Earth
Earth’s atmosphere is composed primarily of nitrogen and oxygen, which are essential for the life which inhabits the planet. The composition of the atmosphere is a direct consequence of the plant life. Plants take in carbon dioxide and expel oxygen through photosynthesis, and without them doing so, it’s likely that the percentage of carbon dioxide in the atmosphere would be significantly higher.
The greenhouse effect that carbon dioxide is partially responsible for is the result of molecules of greenhouse gases absorbing infrared radiation, which is re-radiated towards the surface of the planet and surrounding atmosphere. Without this natural warming effect, temperatures on Earth would be significantly lower worldwide. The greenhouse effect is not the same as global warming – this is the intensification of the natural greenhouse effect via the emission of further greenhouse gases into the atmosphere by human activities. Venus is an extreme example of the runaway consequences of increased global warming!
Mars
The atmosphere of Mars is, much like Venus, composed primarily of carbon dioxide. Having mentioned the extreme greenhouse effect present on Venus as a consequence of the high carbon dioxide levels, it may seem puzzling that the surface temperature of Mars reaches a maximum of 35˚C. This is because the atmosphere of Mars is significantly thinner than that of Venus, so although the proportion of carbon dioxide is comparable, the actual concentration is much lower. The dustiness of the atmosphere gives Mars its characteristic appearance.
Jupiter
Jupiter is the first of the gas giants, and the largest planet in the solar system. Its atmosphere is, interestingly, fairly similar to the composition of the Sun. Unlike the inner planets, there isn’t a clear point at which the atmosphere of Jupiter stops, and the liquid interior of the planet begins. Around a third of the way towards the planet’s core, the pressure is high enough for hydrogen to exist as a metallic liquid, which can conduct electricity and is responsible for Jupiter’s electromagnetic field. Jupiter’s banded cloud system contains varying amounts of ammonia, water, and ammonia-sulfur compound clouds, and also complex sulfur, phosphorous and carbon compounds.
Saturn
Much like Jupiter, the upper clouds in Saturn’s atmosphere are thought to be composed mainly of ammonia ice, with clouds of ammonia hydrosulfide and water lower down. The sulfur present in the atmosphere gives a pale yellow hue to the ammonia clouds. Although not present on the graphic, Saturn’s moon Titan has possibly the most intriguing atmosphere in the solar system, which is the only nitrogen rich atmosphere outside of Earth’s. It’s the only other body in the solar system on which stable surface liquid has ben confirmed, as well as the only other body where it rains – though the rain is liquid methane, rather than water, and it’s estimated there are centuries between each rainfall at specific locations on the surface.
Uranus
The atmosphere of Uranus is, like Jupiter and Saturn, mostly hydrogen and helium. However, the slightly higher levels of methane, particularly in the upper atmosphere, cause greater absorption of red light from the sun, in turn causing the planet to appear a blue-cyan colour. Uranus has the coldest atmosphere in the solar system, at approximately -224˚C, and its atmosphere contains much more water ice than Jupiter and Saturn as a consequence of this.
Neptune
As with Uranus, the blue colouration of Neptune is partially a consequence of the presence of methane – however, as Neptune is a deeper blue, it’s thought that some unknown constituent of the atmosphere must also contribute towards the colour. As the stratosphere of Neptune contains more gaseous hydrocarbons than Uranus, its temperature is marginally higher. Neptune is also home to the strongest winds in the solar system, with their speeds potentially as high as 600 metres per second.
EDIT: Pluto
Pluto hasn’t been a planet for a fair few years now, but that’s no reason to leave it out of the fun. On that note, after posting this, I threw this graphic together, so that Pluto doesn’t feel left out in the cold:

EDIT 2: As some have been asking for a version of the graphic including atmospheric pressures of each planet, I’ve produced a PDF version of the graphic that includes this data. Additionally, as another bonus graphic, here’s the atmospheric composition of Titan, where it rains methane every few centuries:
The graphic in this article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License. See the site’s content usage guidelines.
References & Further Reading
- Planets of the Solar System – Journey Through the Galaxy
- The Planets – Planets of the Solar System
- Evolution of Atmospheres
47 Comments
Barry Piper
Typo: “Sulfur gives gas belts an yellow cast”
Guest
Not in the U.S. It’s correct as originally written. Besides, using ‘an’ in this context both looks and sounds silly. 😛
Compound Interest
It did originally look and sound silly! The sentence originally said ‘sulfur gives gas belts an orange cast’, then whilst designing it I changed ‘orange’ to ‘yellow’ without changing the ‘an’. Forgot to mention here that I’ve since fixed it!
Carol
I love how everything is organized in the info graphic.
Helen M.
Very Informative post.. Info graphics have used in such a manner that helps to understand post in a better manner. Thanks for sharing.. Waiting for your next share… Keep writing..
DigNative
First, I love your infographics; thank you very much for your efforts in preparing and sharing them under a free license! I noticed that there are no PDF versions of the Pluto and Titan infographics available for download. Could you provide these versions too, please?
Additionally, I noticed that the download button on this page points to a PNG version, while I suppose it should point to http://www.compoundchem.com/wp-content/uploads/2014/07/The-Atmospheres-of-the-Solar-System.pdf. So I think this is maybe a mistake.
Thank you very much again!
Compound Interest
Thanks! And thanks for letting me know the download button only points to the PNG version. I’ve updated it now so that the download button points to a zip containing the PDFs of the three graphics. I’ve also added a zip file of print-friendly versions of all three graphics, which you can reach via the ‘printable versions’ button. Hope that helps!
DigNative
Thank you very much and keep up the good work!
DigNative
Sorry for disturbing you again: I noticed that both buttons now point to the same ZIP archive containing only the PDF print versions. On your server there is also a ZIP archive containing the PDF original versions (http://www.compoundchem.com/wp-content/uploads/2014/07/Solar-System-Atmospheres-PRINT.zip ), but it is named “print”. So I think the naming of the ZIP archives should be quite the reverse.
Compound Interest
Ah, sorry about that, must have got the naming mixed up when I created the ZIP files. Should be fixed now!
vish
where can i buy this?
Compound Interest
It’s available to purchase on the site’s Redbubble page, which you can reach by clicking the ‘purchase large posters’ button at the bottom of the article.
DrG
Nice, but there are a couple of mistakes: on Venus “There is a thick layer of carbon monoxide below these clouds, which subjects the surface of the planet to an intense greenhouse effect. ” This is not right. There is not a distinct layer of carbon monoxide below the clouds, and CO is a minor greenhouse gas. The main greenhouse gases are CO2, water vapor and SO2. Just trying to be helpful…. David Grinspoon
Compound Interest
Apologies for that, it’s a while since I wrote this article but I’m certain that was intended to read as carbon dioxide, not carbon monoxide! Not sure how it escaped notice for so long, but thanks for bringing it to my attention – now amended.
tim
Thanks for this, one of the best infographics I’ve seen in a while. Do you know whether the H2 and O2 doesn’t just spontaneously combust into H2O? Is it because the atmosphere is so thin?
Compound Interest
Cheers! Mercury’s atmosphere really is ridiculously thin, barely deserving of the term ‘atmosphere’ if we’re honest, which is why the oxygen and hydrogen don’t just spontaneously combust.
Comments are closed.