Simultaneous mixing ratio profiles of stratospheric NO and NO2as derived from balloon-borne infrared solar spectra

作者: R. D. Blatherwick , A. Goldman , D. G. Murcray , F. J. Murcray , G. R. Cook

DOI: 10.1029/GL007I006P00471

关键词: Mixing ratioDiurnal temperature variationMaterials scienceInfrared spectroscopyInfraredComputational physicsSunsetAtmospheric sciencesSpectral lineMixing (physics)StratosphereGeneral Earth and Planetary SciencesGeophysics

摘要: Balloon-borne infrared solar spectra at ∼0.02 cm−1 resolution obtained during sunset are used for the derivation of simultaneous vertical mixing ratio profiles NO and NO2. A simplified photochemical model diurnal variation is included in analysis.

参考文章(8)
J. S. Garing, R. W. Fenn, F. E. Volz, R. A. McClatchey, J. E. A. Selby, Optical Properties of the Atmosphere (Third Edition) ,(1972)
R. A. McClatchey, Optical Properties of the Atmosphere (Revised) Defense Technical Information Center. ,(1971) , 10.21236/AD0726116
L. S. Rothman, S. A. Clough, R. A. McClatchey, L. G. Young, D. E. Snider, A. Goldman, AFGL trace gas compilation. Applied Optics. ,vol. 17, pp. 507- 507 ,(1978) , 10.1364/AO.17.000507
F. J. Murcray, A. Goldman, D. G. Murcray, G. R. Cook, J. W. Van Allen, R. D. Blatherwick, Identification of isolated NO lines in balloon-borne infrared solar spectra Geophysical Research Letters. ,vol. 7, pp. 673- 676 ,(1980) , 10.1029/GL007I009P00673
A. Goldman, R.S. Saunders, Analysis of atmospheric infrared spectra for altitude distribution of atmospheric trace constituents—I. Method of analysis Journal of Quantitative Spectroscopy & Radiative Transfer. ,vol. 21, pp. 155- 161 ,(1979) , 10.1016/0022-4073(79)90027-X
E. Niple, W. G. Mankin, A. Goldman, D. G. Murcray, F. J. Murcray, Stratospheric NO2and H2O mixing ratio profiles from high resolution infrared solar spectra using nonlinear least squares Geophysical Research Letters. ,vol. 7, pp. 489- 492 ,(1980) , 10.1029/GL007I007P00489