  We use a new Atmospheric Chemistry and Energetics one-dimensional (ACE1D)
thermospheric model to show that the energies deposited by the solar soft
x-rays in the lower thermosphere at altitudes between 100 -150 km (Bailey et
al. 2000), affects the temperature of the entire Earth's thermosphere even at
altitudes well above 300 km. By turning off the input solar flux in the
different wavelength bins of the model iteratively, we are able to demonstrate
that the maximum change in exospheric temperature is due to the changes in the
soft x-ray solar bins. We also show, using the thermodynamic heat equation,
that the molecular diffusion via non-thermal photoelectrons, is the main source
of heat transfer to the upper ionosphere/thermosphere and results in the
increase of the temperature of the neutral atmosphere. Moreover, these
temperature change and heating effects of the solar soft x-rays are comparable
to that of the strong HeII 30.4nm emission. Lastly, we show that the
uncertainties in the solar flux irradiance at these soft x-rays wavelengths
result in corresponding uncertainties in modeled exospheric temperature and the
uncertainties increase with increased solar activity.
