The stability of the Io plasma torus-atmosphere interaction is examine
d. A simple plasma deflection model describes how transients in the pl
asma flux and the content of the atmosphere affect the ionospheric con
ductance, limiting the plasma bombardment and, hence, the supply of at
mospheric species to the torus. The supply of the torus is seen to be
determined by the thermal structure of the plasma, namely, the amount
of low energy plasma producing atmospheric erosion vs. that which prod
uces ionization, so that the torus supply rate is not simply proportio
nal to the torus ion density.