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Derivation of OH Concentrations from LIMS Measurements

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Abstract

Stratospheric concentrations of OH have been derived from LIMS measurements of minor constituents. Two methods have been used. Assuming that HNO3 and NO2 are in photochemical steady state, LIMS measurements of these species, with knowledge of appropriate rate constants and a calculation of the HNO3 photolysis rate, allow nearly global fields of OH to be derived. The derived profiles show satisfactory agreement with model calculations and the limited number of in situ observations. As a check on our method, OH has also been derived by calculations of its sources and sinks using the LIMS measurements of H2O. The two methods agree extremely well in low latitudes. At higher latitudes the agreement is less satisfactory. This is discussed in terms of the diurnal behaviour of the species and the time constant of the HNO3/NO2 equilibrium.

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© 1985 ECSC, EEC, EAEC, Brussels and Luxembourg

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Pyle, J.A., Zavody, A.M., Harries, J.E., Moffat, P.H. (1985). Derivation of OH Concentrations from LIMS Measurements. In: Zerefos, C.S., Ghazi, A. (eds) Atmospheric Ozone. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-5313-0_14

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  • DOI: https://doi.org/10.1007/978-94-009-5313-0_14

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-8847-3

  • Online ISBN: 978-94-009-5313-0

  • eBook Packages: Springer Book Archive

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