A new model to explain both the Ly-alpha bulge of Jupiter and the heat
ing excess of the jovian upper atmosphere is presented. Based on an id
ealized representation of the auroral activity, we precisely describe
how thermospheric winds, which may form near the northern and southern
oval maximum activity regions in the jovian aurora, could propagate a
long the planet surface and collide at the jovian equator near 100 deg
rees longitudinal system III. In this collision, part of the energy is
converted to random wave motion and heat, and the remaining energy is
transferred to two lateral outgoing jets. The random motion and heat
enhance the atomic Ii cross section, explaining the excess observed fo
r both the brightness and the width of the Ly-alpha line. The kinetic
energy carried by the northern and southern jets spreads over the whol
e planet surface as thermal energy, explaining the heating excess obse
rved for the jovian upper atmosphere. The resulting dynamics and energ
y budget of the jovian upper atmosphere are carefully described. (C) 1
995 Academic Press, Inc.