Europa, the enigmatic moon of Jupiter, is believed to be home to a subsurface ocean of liquid water. However, future missions to explore Europa's ocean may need to dig deep. Research suggests that water does not stay in a liquid state near Europa's surface for longer than a few tens of thousands of years - the blink of an eye in geological terms. Klara Kalousova will present this work at the European Planetary Science Congress in Madrid on Tuesday 25 September 2012.
Europa is mainly made from rock and iron, with a water shell around 100km deep beneath a crust of solid ice. The ocean is warmed sufficiently to maintain its liquid state by heat produced as a by-product of gravitational pulling to-and-fro from Jupiter.
Pockets of liquid water could be tantalisingly close to the surface. However, Kalousova, from the University of Nantes and Charles University in Prague, believes these would be short-lived. She explains, "A global water ocean may be present, but relatively deep below the surface - around 25 to 50km. There could be areas of liquid water at much shallower depths, say around 5km, but these would only exist for a few tens of thousands of years before migrating downwards."
Kalousova reached these conclusions by mathematically modelling mixtures of liquid water and solid ice under different conditions. She found that due to factors such as density and viscosity differences, liquid water migrates rapidly downwards through partially molten ice and eventually reaches the subsurface ocean.
This is a model. I do not know the level of confidence that ought to be attached to it.
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