Jupiter's moon Europa possesses a tenuous atmosphere that is thought to be constantly replenished by erosion of its water ice surface (Johnson et al., 2009;McGrath et al., 2009). The main species in the bound atmosphere are expected to be molecular oxygen (O 2 ), H 2 , and H 2 O (Shematovich et al., 2005;Smyth & Marconi, 2006). The first evidence for this atmosphere was provided by a far-ultraviolet (FUV) spectrum of Europa taken by the Hubble Space Telescope, which revealed emissions at 1,304 Å and 1,356 Å. These emissions were related to atomic oxygen multiplets around these wavelengths, but the persistently brighter disk-averaged OI1356 Å emission intensity (Hall et al., 1995(Hall et al., , 1998 is in agreement only with electron impact dissociative excitation on molecular oxygen as source. The ratio of the intensities of the FUV oxygen multiplets at 1,356 Å and 1,304 Å, (OI) E r I(OI1365 Å)/I(OI1304 Å), has become a standard diagnostic to probe for atmospheric composition at Jupiter's moons (