The cryogenic infrared radiance instrumentation for shuttle (CIRRIS) experiment was own onboard STS-39 from 29 April to 1 May 1991. A comprehensive set of spectral and spatial infrared data of atmospheric and Earth terrain data was collected by an interferometer and radiometer. The mission occurred during a major geomagnetic storm (K p ->5), and as a result, a substantial amount of spectral data on bright auroral backgrounds were collected in the midnight sector of the auroral oval. The coincidental timing of the CIRRIS mission, only a few weeks before the eruption of Mount Pinatubo (June 1991), substantially increased the value of the stratospheric data from CIRRIS, which now serves as a clean atmosphere baseline against which various post-Pinatubo observations can be compared to assess the short-and long-term effects of a major volcanic eruption on the stratosphere. In addition, there were a number of unexpected and important scienti c discoveries that resulted from analysis of the CIRRIS high-resolution Earthlimb emission spectra including the identi cation of an important new class of non-local thermodynamic equilibrium emissions resulting from highly rotationally excited diatomic species (OH, NO and NO + ) in the mesosphere and thermosphere. These nonthermal rotational emissions were observed for both day and nighttime conditionsand were not included in or predicted by existing atmosphericmodels before the CIRRIS ight. A brief overview of the instrumentation and data collection methods is presented. A general review of the CIRRIS data and a summary of the most signi cant ndings previously reported by various groups are also presented.
IntroductionScienti c Objectives T HIS paper summarizes the results and major ndings from the cryogenic infrared radiance instrumentation for shuttle (CIRRIS-1A) experiment that was own onboard STS-39 between 29 April and 1 May 1991. This study consisted of a global infrared remote sensing survey that sampled the atmosphere from the nadir up through the Earthlimb to shuttle altitudes of 260 km in the 2.5-25 ¹m wavelength region. The primary objective of this experiment was to obtain simultaneous spectral and spatial measurements of atmospheric emissions for altitudes between 0 and 150 km. Atmospheric species of interest included water, hydroxyl, nitric oxide, ozone, and carbon dioxide during day and night under various levels of geomagnetic activity. Observations covered a range of latitudes from approximately ¡68 to C68 deg during moderate to active geomagnetic activity (K p D 3-7) and also when bright aurora were observed. Data were collected from numerous strong atmospheric emitters, such as OH at 2.7 ¹m and CO 2 at 4.3 and 15 ¹m, NO at 5.3 ¹m, O 3 at 9.6 ¹m, and H 2 O at 6.3 ¹m and in the long wavelength infrared (LWIR) region. Many other trace species were also measured, such as CFC-11 and CFC-12, HNO 3 , CH 4 , and CO. Data were taken simultaneously by three infrared (IR) instruments: 1) an interferometer with an eight position lter wheel, 2) a lter radiometer with 7 wide...