Observations with the High Resolution Imager on the Rontgensatellit re
veal x-ray emissions from Jupiter's equatorial latitudes. The observed
emissions probably result from the precipitation of energetic (>300 k
iloelectron volts per atomic mass unit) sulfur and oxygen ions out of
Jupiter's inner radiation belt, Model calculations of the energy depos
ition by such heavy ion precipitation and of the resulting atmospheric
heating rates indicate that this energy source can contribute to the
high exospheric temperatures (>800 kelvin at 0.01 microbar) measured b
y the Galileo probe's Atmospheric Structure Instrument. Low-latitude e
nergetic particle precipitation must therefore be considered, in addit
ion to other proposed mechanisms such as gravity waves and soft electr
on precipitation, as an important source of heat for Jupiter's thermos
phere.