I find it hard to believe, but the end of Cassini’s original 4-year mission is just around the corner, this June 30. Planning has been underway for a couple of years on a two-year extended mission. That mission will take Cassini through Saturn’s northern spring equinox (the moment when the Sun passes through Saturn’s equatorial plane from its southern hemisphere to its northern hemisphere). While not official, that makes the name Cassini Equinox Mission a logical choice for the extended mission, and while less economical, certainly more comprehensible than “XM”.
The discussion at last week’s Cassini Project Science Group meeting centered around plans for an “XXM” which, hopefully, will soon be known as the Cassini Solstice Mission. That name would be appropriate if plans succeed to keep Cassini running through the summer of 2017 when the north pole of Saturn (and therefore also its moons) is pointed most directly at the Sun (that is, Saturn’s northern summer solstice).
So, what’s the big deal about Saturn’s solstice? Now that Cassini has spent four years studying the Saturn environment (about 1/8th of a Saturn year) we have seen changes in just about every component of the Saturn System that take place over the seasonal timescale. The atmosphere of Saturn undergoes exceptionally strong seasonal variations because the rings cast an enormous shadow on one hemisphere near solstice, and virtually no shadow at all near equinox. Titan’s lakes currently appear to be largely confined to the wintery north pole. What will happen to those lakes as summer comes to the north? Enceladus’s southern pole geysers are not driven by the Sun, but there are indications that it and the dusty E ring it feeds undergo large changes on timescales of several years. Solar radiation pressure pushes the dust particles in the E ring; this may lead to large-scale deformation and warping of the ring as the Sun gets high above the ring plane toward solstice. The main rings are also exhibiting a variety of phenomena that unfold over days, months, and years. The F ring in particular seems to be host to a chaotic environment where moons form and break apart. Waves in the rings propagate across the rings at just a few millimeters per second. With many years of observations we will be able to see real structural changes in the rings as the moons producing these waves undergo small changes in their orbits due to interactions with other moons. There are also a myriad unanswered questions that simply require more observations to answer, such as what is responsible for keeping all those gaps in the rings open, and what do the north polar regions of the icy satellites look like?
There’s no fixed timetable, but the end of the Cassini Equinox Mission is not until June 2010, so it could easily be another year before there is firm guidance from NASA headquarters on the Cassini Solstice Mission. One factor that will be considered is what to do with the spacecraft at the end of the mission. In order to avoid possible biological contamination of Titan and Enceladus, Cassini may be crashed into Saturn after some exciting flights through the gap between the rings and the planet. Or it may be crashed into an icy moon, or perhaps even sent off to interplanetary space, though this final option would negatively impact the science returned from the Saturn system in the solstice mission.