摘要: In July 1985 an infrared solar occultation experiment was performed with a balloon-borne, non-scanning, multi-detector grating spectrometer. From the data were retrieved simultaneous mixing ratio profiles of ozone, water vapor, ni... 展开 In July 1985 an infrared solar occultation experiment was performed with a balloon-borne, non-scanning, multi-detector grating spectrometer. From the data were retrieved simultaneous mixing ratio profiles of ozone, water vapor, nitric acid, and CF2Cl2 between 12 and 35 km. The retrieved ozone and water vapor profiles were compared with concurrent in-situ measurements with electrochemical concentration cells (ECCs) and frost-point hygrometers, respectively. The retrieved ozone profile was in good agreement with the correlative data. The retrieved values of water vapor mixing ratio, while close in magnitude to the correlative measurements, differed in their altitude dependence. Although there was no concurrent in-situ data for nitric acid and CF2Cl2, the retrieved profiles were consistent with measurements in the literature. 收起