New observations and reanalysis of previous measurements suggest an up
ward revision of the measured thermospheric nitric oxide density. Our
previous model of NO production by fast N(S-4) atom collisions with O-
2 has been updated. It includes the effect of soft solar X rays, Auger
electrons, and a detailed treatment of N-2 dissociative ionization ch
annels. In addition, new calculations indicate that the transfer of tr
anslational energy in N + N-2 collisions is less efficient than in the
hard sphere approximation. This result leads to reevaluation of the e
nergy dependent relaxation cross section and to an upward revision of
the reacting efficiency of collisions of N with O-2 to form nitric oxi
de. The calculated peak NO density increases by a factor of similar to
2 when the effect of superthermal nitrogen atoms is included. The mod
el response of the N(S-4) energy distribution function and NO density
to solar cycle variations is presented. The NO density at 110 km chang
es from 5.4 x 10(7) to 1.3 x 10(8) cm(-3) when the solar F-10.7 index
varies from 70 to 245, but its response depends on the magnitude of th
e soft X ray increase with solar activity.