Galileo energetic particles detector (EPD) data are presented from several
close encounters of the spacecraft with Jupiter's moon Europa. These data r
eveal significant decreases in electron and ion count rates very close to t
he moon and a few Europa radii downstream. The relation between count rate
decreases and satellite absorption is analyzed because these particles sput
ter and chemically modify Europa's surface. Decreases on the plasma wake si
de of the satellite have radial extents comparable to satellite dimensions.
Furthermore, some energetic particle wakes are shifted toward Jupiter from
predicted locations. At some wake locations, electron fluxes do not get ab
ove instrument background levels. Corresponding electrons are lost preferen
tially on Europa's trailing hemisphere. Upstream of Europa during the E12 e
ncounter, deep decreases in energetic ion count rates are observed for some
instrument look directions. These decreases are associated with satellite
absorption because the E12 closest approach altitude is smaller than releva
nt ion gyroradii. Other E12 decreases, such as a "bite-out" corresponding t
o a peak in the measured magnetic field intensity, are associated with "sec
ondary" drifts in the radial direct:ion caused by the field gradient. Pitch
angle distributions measured during the E15 encounter (when Galileo was in
Europa's wake) show much higher fluxes of locally mirroring particles than
would be expected in a simple absorption signature. We suggest that a frac
tion of the upstream population escapes absorption because of the pileup of
magnetic flux on Europa's trailing hemisphere.