Unexpected Cooling effect in Saturn’s upper atmosphere

A simple calculation to give the expected temperature of a planet’s upper atmosphere balances the amount of sunlight absorbed by the energy lost to the lower atmosphere. But the calculated values don’t tally with the actual observations of the Gas Giants: they are consistently much hotter.

It has long been thought that the culprit behind the heating process was the ionosphere, being driven by the planet’s magnetic field, or magnetosphere. By using numerical models of Saturn’s atmosphere the researchers found that the net effects of the winds driven by polar energy inputs is not to heat the atmosphere but to actually cool it.

Professor Alan Aylward, of the UCL Department of Physics & Astronomy, and an author of the study, explains: “The aurora has been studied for over a hundred years, yet our discovery takes us back to first principles. We need to re-examine our basic assumptions about planetary atmospheres and what causes the observed heating.”

“Studying what happens on planets such as Saturn gives us an insight into what happens closer to home. Planets can lose their atmospheres as we see with Mars. Do we completely understand how this happens? Are there mechanisms heating the gas and causing it to escape that we do not yet fully understand? By studying what happens in other atmospheres we may find clues to Earth’s future.”

The study was funded by the UK Particle Physics and Astronomy Research Council (PPARC) and Sun Microsystems Ltd and carried out using the HiPerSPACE facility at University College London.

Contacts

Gill Ormrod – PPARC Press Office
Tel: 01793 442012. Email: gill.ormrod@pparc.ac.uk
Professor Alan Aylward, UCL Department of Physics & Astronomy
Tel: +44 (0)20 7679 2446, Email: a.aylward@ucl.ac.uk
Judith H Moore, UCL Media Relations
Tel: +44 (0) 20 7679 7678, Mobile: +44 (0)77333 075 96, Email: judith.moore@ucl.ac.uk