[1] The Spatial Infrared Imaging Telescope III (SPIRIT III) radiometer on the Midcourse Space Experiment satellite (MSX), observed enhanced 4.3 mm emission from a very well characterized aurora over the Barents Sea on 9 February 1997, in conjunction with observations by the POLAR and FAST satellites, the Loparskaya ground site, and ultraviolet and visible spectrometers aboard MSX. Measurements of the auroral location, form, spatial extent and dosing conditions were applied to specify the component of auroral 4.3 mm radiance due to the slowly produced and optically thick CO 2 n 3 (001-000) transition. An analysis based on the Auroral Atmospheric Radiance Code (AARC) indicates: (1) the emission originates near and beyond the tangent point; (2) the optically thick CO 2 n 3 radiation is largely self absorbed by the intervening atmosphere; and (3) the auroral enhancement is predominantly due to NO + Dv = 1 vibrational state transitions. In addition, the analysis indicates that the previously reported laboratory result for the NO + v ! 1 vibrational yield from the reaction, N + + O 2, is insufficient to account for the observed 4.3 mm emission. In order to explain the current results, we propose that there is additional production from the reaction, N 2 + + O, forming NO + in vibrational levels 0, 1, and 2 with relative populations of approximately 0.25, 0.5, and 0.25, respectively. The combined production processes yield an energetic electron induced efficiency of 0.56 ± 0.18 photons per auroral ion pair for NO + Dv = 1 emission at altitudes equal to or greater than 112 km.