Abstract
We discuss a realistic forward modelling and retrieval algorithm for temperature and ozone sounding developed to process data received by the planned Sun Monitor and Atmospheric Sounder (SMAS) instrument. The SMAS sensor concept employs the solar occultation technique and is primarily aiming at mesospheric profiles. The SMAS sensor provides self-calibrating transmission data, which allows the accurate derivation of profiles of molecular oxygen, molecular nitrogen, atomic oxygen, and ozone and temperature. We concentrated on data between 180 nm and 250 nm to analyse transmission data for ozone and temperature profiling. In order to enable a good and fast retrieval algorithm performance, a detailed view of the absorption behaviour of the solar irradiance in the considered wavelength region is necessary and will be presented in this work. In particular, some emphasis is placed on evaluating different fast forward modelling approximations for the SMAS channels in the Schumann-Runge bands (180–205 nm). Exemplary retrieval results for ozone are shown as well.
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References
Kirchengast G (1998) End-to-end GNSS Occultation Performance Simulator overview and exemplary applications. Wissenschaftl Ber 2/1998, IGAM, Univ of Graz, Austria, 138 pp
Kirchengast G, Fritzer J, Ramsauer J (2002) End-to-end GNSS Occultation Performance Simulator version 4 (EGOPS4) software user manual (overview and reference manual). Tech Rep ESA/ESTEC-3/2002, IGAM, Univ of Graz, Austria, 472 pp 342 C. Rehrl and G. Kirchengast
Lumpe JD, Chang CS, Strickland DJ (1991) Atmospheric constituent density profiles from full disk solar occultation experiments. J Quant Spectrosc Rad Transfer 46: 483–506
Minschwaner K, Anderson GP, Hall LA, Yoshino K (1992) Polynomial Coefficients for Calculations. J Geophys Res 97: 10103–10108
Minschwaner K, Starke V (2000) Photodissociation of nitric oxide in the middle and upper atmosphere. Phys Chem Earth manuscript no ST9. 2–022, Dept of Physics, New Mexico Inst of Mining and Technology, Socorro, New Mexico
Molina LT, Molina MJ (1986) Absolute absorption cross sections of ozone in the 185- to 350-nm wavelength range. J Geophys Res 91: 14501–14508
Nicolet M, Cielik S, Kennes R (1980) Atmospheric absorption in the 02 S-R band spectral range and photodissociation rates in the stratosphere and mesosphere. Planet Space Sci 28: 85–103
Rehrl C (2000) Mesospheric temperature and ozone sounding based on solar occultation data M Sc thesis, 124 pp, IGAM, Univ of Graz, Austria
Rieder MJ, Kirchengast G (2001) Error analysis for mesospheric temperature profiling by absorptive occultation sensors. Ann Geophys 19: 71–81
Smith GR, Hunten DM (1990) Study of planetary atmospheres by absorptive occultations. Rev of Geophys 28: 117–143
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© 2004 Springer-Verlag Berlin Heidelberg
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Rehrl, C., Kirchengast, G. (2004). Mesospheric Temperature and Ozone Sounding by the SMAS Solar Occultation Sensor. In: Kirchengast, G., Foelsche, U., Steiner, A.K. (eds) Occultations for Probing Atmosphere and Climate. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-09041-1_29
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DOI: https://doi.org/10.1007/978-3-662-09041-1_29
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-06108-0
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