Scientific objectives of the Solar Mesosphere Explorer mission |
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Authors: | Gary E. Thomas Charles A. Barth Elaine R. Hansen Charles W. Hord George M. Lawrence George H. Mount Gary J. Rottman David W. Rusch A. Ian Stewart Ronald J. Thomas Julius London Paul L. Bailey Paul J. Crutzen Robert E. Dickinson John C. Gille Shaw C. Liu John F. Noxon Crofton B. Farmer |
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Affiliation: | (1) Laboratory for Atmospheric and Space Physics, University of Colorado, 80309 Boulder, Colorado, USA;(2) Dopartment of Astro-Geophysics, University of Colorado, 80309 Boulder, Colorado, USA;(3) Department of Aerospace Engineering, University of Colorado, 80309 Boulder, Colorado, USA;(4) National Center for Atmospheric Research, 80303 Boulder, Colorado, USA;(5) Aeronomy Laboratory, National Oceanic and Atmospheric Administration, 80303 Boulder, Colorado, USA;(6) Division of Geological and Planetary Sciences, California Institute of Technology, 91125 Pasadena, California, USA;(7) Present address: Jet Propulsion Laboratory, California Institute of Technology, 91103 Pasadena, California, USA |
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Abstract: | The 1981–82 Solar Mesosphere Explorer (SME) mission is described. The SME experiment will provide a comprehensive study of mesospheric ozone and the processes which form and destroy it. Five instruments will be carried on the spinning spacecraft to measure the ozone density and its altitude distribution from 30 to 80 km, monitor the incoming solar ultraviolet radiation, and measure other atmospheric constituent which affect ozone. The polar-orbiting spacecraft will be placed into a 3pm-3 am Sun-synchronous orbit. The atmospheric measurements will scan the Earth's limb and measure: (1) the mesospheric and stratospheric ozone density distribution by inversion of Rayleigh-scattered ultraviolet limb radiance, and the thermal emission from ozone at 9.6 m; (2) the water vapor density distribution by inversion of thermal emission at 6.3 m; (3) the ozone photolysis rate by inversion of the O2(1 g) 1.27 m limb radiance; (4) the temperature profile by a combination of narrow-band and wide-band measurements of the 15 m thermal emission by CO2; and, (5) theNO2 density distribution by inversion of Rayleighscattered limb radiance at 0.439 m. The solar ultraviolet monitor will measure both the 0.2–0.31 m spectral region and the Lyman-alpha (0.1216 m) contribution to the solar irradiance. This combination of measurements will provide a rigorous test of the photochemical equilibrium theory of the mesospheric oxygen-hydrogen system, will determine what changes occur in the ozone distribution as a result of changes in the incoming solar radiation, and will detect changes that may occur as a result of meteorological disturbances. |
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Keywords: | Solar Mesosphere Explorer Ozone Water vapor Solar ultraviolet monitor Limb radiance |
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