The bulk parameters of the hot (>20 keV) plasmas of Jupiter's inner ma
gnetosphere, including the vicinity of the Io plasma torus, are presen
ted for the first time (L = 5 to 20 R(J)). The low-energy charged part
icle (LECP) instrument on Voyager 1 that obtained the data presented h
ere was severely overdriven within the inner regions of Jupiter's magn
etosphere. On the basis of laboratory calibrations using a flight spar
e instrument, a Monte Carlo computer algorithm has been constructed th
at simulates the response of the LECP instrument to very high particle
intensities. This algorithm has allowed for the extraction of the hot
plasma parameters in the Jovian regions of interest. The hot plasma c
omponents discussed here dominate over other components with respect t
o such high-order moments as the plasma pressures and energy intensiti
es. Our findings include the following items. (1) Radial pressure grad
ients change from positive (antiplanetward) to negative as one moves o
utward past about 7.3 R(J). While the observed hot plasma distribution
s will impede the radial transport, via centrifugal interchange, of io
genic plasmas throughout the Io plasma torus regions out to 8 R(J), th
e plasma impoundment concept of Siscoe et al. [1981] for explaining th
e so-called ''ramp'' in the flux shell content profile of iogenic plas
mas (7.4-7.8 R(J) [Bagenal, 1994]) is not supported. (2) We predict a
radical ordering for the generation of the aurora, which translates in
to a latitudinal structure for auroral emissions. Planetward of about
12 R(J), intense aurora (10 ergs/(cm(2) s) precipitation) can only be
caused by electron precipitation, whereas outside of about 12 R(J) suc
h intense aurora can only be caused by electron precipitation. Uncerta
inties concerning the causes of Jovian aurora may stem in part from fa
ilures of some observations to resolve the latitudinal structure that
is anticipated here and possibly from changes in the aurora; configura
tion and/or charged particle spectral properties since the Voyager epo
ch.