Measurements of CH sub 4 , N sub 2 O, CO, H sub 2 O and O sub 3 in the middle atmosphere by the ATMOS experiment on Spacelab 3
M. R. Gunson, C. B. Farmer, R. H. Norton, R. Zander, C. P. Rinsland, J. H. Shaw, Bo‐Cai Gao
Abstract
M. R. Gunson, C. B. Farmer, R. H. Norton, R. Zander, C. P. Rinsland, J. H. Shaw, Bo‐Cai Gao
Abstract
The volume mixing ratios of five minor gases (CH{sub 4}, N{sub 2}O, CO, H{sub 2}O, and O{sub 3}) were retrieved through the middle atmosphere from the analysis of 0.01/cm resolution infrared solar occultation spectra recorded near 28 N and 48 S latitudes with the ATMOS (Atmospheric Trace Molecule Spectroscopy) instrument, flown on board Spacelab 3. The results, which constitute the first simultaneous observations of continuous profiles through the middle atmosphere for these gases, are in general agreement with reported measurements from ground, balloon and satellite-based instruments for the same seasons. In detail, the vertical profiles of these gases show the effects of the upper and middle atmospheric transport patterns dominant during the season of these observations. The profiles inferred at different longitudes around 28 N suggest a near-uniform zonal distribution of these gases. Although based on fewer observations, the sunrise occultation measurements point to a larger variability in the vertical distribution of these gases at 48 S.
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The volume mixing ratios of five minor gases (CH{sub 4}, N{sub 2}O, CO, H{sub 2}O, and O{sub 3}) were retrieved through the middle atmosphere from the analysis of 0.01/cm resolution infrared solar occultation spectra recorded near 28 N and 48 S latitudes with the ATMOS (Atmospheric Trace Molecule Spectroscopy) instrument, flown on board Spacelab 3. The results, which constitute the first simultaneous observations of continuous profiles through the middle atmosphere for these gases, are in general agreement with reported measurements from ground, balloon and satellite-based instruments for the same seasons. In detail, the vertical profiles of these gases show the effects of the upper and middle atmospheric transport patterns dominant during the season of these observations. The profiles inferred at different longitudes around 28 N suggest a near-uniform zonal distribution of these gases. Although based on fewer observations, the sunrise occultation measurements point to a larger variability in the vertical distribution of these gases at 48 S.
Key concepts: Occultation, Atmosphere (unit), Sunrise, Trace gas, Atmosphere of Earth, Mixing ratio, Atmospheric sciences, Middle latitudes