Planets & Solar System
Uranus inside and out It has a very similar structure to Neptune but this ice giant still retains its mysteries The term ‘gas giant’ implies that Uranus is solely composed of gases, but studies indicate that it actually has a core of silicate rock, encased in ices and topped with a gaseous layer. The core must be very small, since Uranus is the second-least dense planet. It likely takes up only 20 per cent of the planet’s radius. The ice mantle surrounding the core is fluid, with volatiles like methane, ammonia and water. In fact, this electrically conducive fluid is often called an ammoniawater ocean by experts. The outer layer is mostly helium and hydrogen. Uranus is also much cooler inside than the other gas giants – it’s actually the coldest planet in the Solar System. Neptune radiates 2.61 times the heat that Uranus does. We aren’t sure why Uranus is so cold in comparison, but it may have been struck by a large body that forced it to expel most of the heat it had when formed, or there could be a complex system at work in the atmosphere that keeps core heat from getting out. The atmosphere contains three layers: the thermosphere, the stratosphere and the troposphere. The lowest layer, the troposphere, is the most interesting and is rich in volatile ices like methane and ammonia. It has four cloud layers: methane, hydrogen sulphide and ammonia, ammonium hydrosulphide, and water clouds at the upper limit. We’ve only observed the top two layers, along with a hazy layer above them. The stratosphere sits between the troposphere and the outermost layer, the thermosphere. Uranus tends to look light bluish or greenish in colour, and it has faint darker bands. The overall colour is due to the way that
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methane absorbs visible and nearinfrared light. Until Voyager 2 explored Uranus’s atmosphere, we didn’t know much about its features. The probe found a bright polar cap at the south pole, as well as a lighter band called a collar. There were darker bands in the southern hemisphere and about ten lighter clouds around the middle latitudes. The timing of Voyager 2’s arrival meant that it could not fully observe the northern hemisphere. In the Nineties, Hubble and groundbased telescopes like the Keck Observatory began to see more atmospheric features on Uranus. They spotted many more clouds in the northern hemisphere, which are brighter and at a higher elevation than the ones in the southern hemisphere. They also observed in 2007 that the southern collar had nearly disappeared, while one in the north had grown.
