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Scientific objectives of the Solar Mesosphere Explorer mission
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
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
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 mgrm; (2) the water vapor density distribution by inversion of thermal emission at 6.3 mgrm; (3) the ozone photolysis rate by inversion of the O2(1Deltag) 1.27 mgrm limb radiance; (4) the temperature profile by a combination of narrow-band and wide-band measurements of the 15 mgrm thermal emission by CO2; and, (5) theNO2 density distribution by inversion of Rayleighscattered limb radiance at 0.439 mgrm. The solar ultraviolet monitor will measure both the 0.2–0.31 mgrm spectral region and the Lyman-alpha (0.1216 mgrm) 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.
Keywords:Solar Mesosphere Explorer  Ozone  Water vapor  Solar ultraviolet monitor  Limb radiance
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