A general model is presented for the production of images of thermosph
eric dayglow emissions. Ultraviolet images are generated that are rele
vant to remote sensing of the principal constituents of the thermosphe
re (O and N2) and the ionosphere (O+). The emission features considere
d here are 1356-angstrom (O), Lyman-Birge-Hopfield bands of N2 between
1650 and 1715 angstrom, and 834 angstrom (O+). The MSIS-86 and Intern
ational Reference Ionosphere models were used as climatological repres
entations of the distributions of neutrals and ions, respectively. We
describe the generation of the images beginning with the production of
volume-emission-rate profiles. A detailed description of the generali
zed image-generation technique is given. This technique permits us to
change the observer's altitude and viewing geometry without incurring
a large computational burden. The images produced by this technique de
monstrate the potential of airglow imaging systems for remote sensing
of global variability in thermospheric composition.