What is the solar system moon with the densest atmosphere? Most space fans know that the answer is Titan; with a surface atmospheric pressure of 1.4 bars, its air is thicker than Earth's. A few of you might know that Triton's is the next densest. But what's the third? Fourth? Do any other moons even have atmospheres? In fact, they do; and one such atmosphere has just been discovered.
No other moon's atmosphere is quite like Titan's smoggy sky. From space, we can see straight to the other moons' surfaces, with no clouds or haze in the way. Most moons' atmospheres are extremely tenuous, so much so that their constituent molecules never collide with each other. Such collisionless atmospheres are called exospheres. The Moon has an exosphere, as does the planet Mercury.
A very few moons have atmospheres that are dense enough for their gas molecules to collide with each other. This can happen even in a pretty thin atmosphere. Triton's had a surface pressure of 14 microbars when Voyager 2 flew by. As the seasons have progressed on Triton the atmospheric pressure has increased by a factor of three or four, but it's still 20,000 times less dense than Earth's. Still, when air molecules can collide, you can have wind, and even weather. Such an atmosphere can also offer a moon's surface some protection from the particles flung around in giant planet magnetospheres. You can see on Triton how upper-level winds blow the tops of its geysers away. If we're very lucky, we'll see similar features when New Horizons passes Pluto this summer. (Pluto's atmosphere is denser than Triton's.)
NASA / JPL / Ted Stryk
Triton color global view
Voyager 2 acquired the images for this high-resolution mosaic of Triton on August 25, 1989. The south pole is at the left; several of Triton's famous south polar geysers are visible. Toward the equator at right, Triton is covered with a strange "cantaloupe terrain".
So which moons other than Titan and Triton have weather? We think there are two. The third-densest atmosphere in the solar system is Io's. From observations with the Submillimeter Array, Arielle Moullet and three coauthors measured sulfur dioxide, sulfur monoxide, and sodium chloride in its air. (Yes, salt is a constituent of Io's atmosphere!) Some of these gases, probably including all of the salt, is fed directly to Io's atmosphere by its constantly erupting volcanoes, but there's too much sulfur dioxide for all of it to be volcanic; some of it has to come from sublimating sulfur dioxide frost.
NASA / JPL / SSI / Gordan Ugarkovic
Animation of Tvashtar and Pele's Plumes
This animation, composed of UV3 frames from the Cassini Imaging Science Subsystem (ISS) taken on January 2, 2001 and magnified by a factor of 2, shows plumes from Io's Tvashtar and Pele Paterae (volcanoes).
At the surface, the peak pressure is around 1.9 nanobars -- that is to say, Earth's atmosphere is 200 million times denser than Io's. But it's still an atmosphere, and a variable one. Io's surface breathes over the course of its day, exhaling sulfur dioxide as it warms in sunlight, and pulling it back down to the surface as it cools at night. The volcanoes heat their local areas, making patches of denser atmosphere and out-flowing winds.
One of the weirdest things in Io's atmosphere is a consequence of it having no magnetic field while being embedded inside Jupiter's. Jupiter's magnetic field sweeps across Io's atmosphere once each Jupiter day, slamming into the back of Io's atmosphere. The magnetic field moves the ions in Io's atmosphere, but not the neutral molecules, so the moving ions crash into the neutral molecules, moving as a current through Io's resistant neutral atmosphere. The interaction of Jupiter's magnetic field with Io's ionosphere has a visible manifestation as a glowing Io footprint within Jupiter's aurora. (For further reading, I recommend this PDF of a PowerPoint presentation on Io's atmosphere that had no name on it -- please speak up in the comments if you know whose presentation it is!)
NASA/ESA, John Clarke (University of Michigan)
Satellite footprints in Jupiter's northern aurora
Auroras are curtains of light resulting from high-energy electrons racing along the planet's magnetic field into the upper atmosphere. The electrons excite atmospheric gases, causing them to glow. The image shows the main oval of the aurora, which is centered on the magnetic north pole, plus more diffuse emissions inside the polar cap. Though the aurora resembles the same phenomenon that crowns Earth's polar regions, the Hubble image shows unique emissions from the magnetic "footprints" of three of Jupiter's largest moons. (These points are reached by following Jupiter's magnetic field from each satellite down to the planet). Auroral footprints can be seen in this image from Io (along the left hand limb), Ganymede (near the center), and Europa (just below and to the right of Ganymede's auroral footprint). These emissions, produced by electric currents generated by the satellites, flow along Jupiter's magnetic field, bouncing in and out of the upper atmosphere. They are unlike anything seen on Earth.
Galileo captured this global view of Callisto on its 11th orbit of Jupiter, on November 5, 1997.
Cunningham and coauthors used the Cosmic Origins Spectrograph on Hubble to detect the telltale ultraviolet emission of atomic oxygen and determine its abundance. Oxygen probably forms at Callisto when water ice molecules at the surface are split into hydrogen and oxygen atoms; some of the lightweight hydrogen escapes from the atmosphere entirely, leaving the heavier oxygen behind. John Spencer (who was second author on the paper) helped me convert from atmospheric column abundances to surface pressures. Cunningham and coauthors' work suggests that Callisto's leading hemisphere has a surface atmospheric pressure of 26 picobars -- that is, it is 40 billion times less dense than Earth's -- but that the air over its trailing hemisphere may be 10 times denser.
A dynamic atmosphere, even though very thin, slightly shifts our view of Callisto. Callisto is the outermost of the Galilean satellites and also, to use a highly technical term, the deadest. Its gravity field suggests that, unlike the other Galilean moons, it never got warm enough to differentiate into a rocky core and icy mantle, remaining instead a primitive mixture of ice and rock all the way down. A couple of years ago, Jeff Moore postulated that Titan might not have internal geological activity and may just be "Callisto with weather." It turns out that Callisto may have weather! Callisto's atmosphere is more than dense enough for its molecules to collide with each other.
Oxygen atmospheres form at Europa and Ganymede for the same reason that they form at Callisto. But their oxygen atmospheres are a factor of a few less dense than Callisto's, making theirs exospheres, not collisional atmospheres. No wind, and no weather. (At least not at present.)
So here you go: the unlikely set of four solar system moons known to have atmospheres dense enough for weather. In order: Saturn's moon Titan; Neptune's moon Triton; and Jupiter's moons Io and Callisto.
NASA / JPL / SSI / Ted Stryk / Jason Perry / Emily Lakdawalla
Moons with atmospheres
There are four moons in the solar system that are known to have collisional atmospheres. In order of decreasing atmospheric column density, they are: Saturn's Titan, Neptune's Triton, and Jupiter's Io and Callisto.