Retrieval of NO2 vertical profiles from ground‐based UV‐visible measurements: Method and validation

Vertical profiles of NO2 are retrieved from ground-based UV-visible slant columns by sequential estimation, using a forward model that consists of a stacked box photochemical model and a radiative transfer model. The retrieval method is characterized, and a rigorous error analysis is presented. The vertical resolution of the retrieved profiles is shown to vary from 5 to 10 km, depending on the retrieval altitude. The retrieved profiles are found to be moderately sensitive to the assumed vertical profiles of ozone and aerosol, to the range of solar zenith angles of the observations, and to the error in the slant column. However, in the altitude range 10 to 35 km they are relatively insensitive to a priori information and agreed well with profiles from simultaneous balloon-borne measurements.

[1]  Jacques Piquard,et al.  Ozone and nitrogen dioxide vertical distributions by UV‐visible solar occultation from balloons , 1994 .

[2]  Barney J. Conrath,et al.  Vertical Resolution of Temperature Profiles Obtained from Remote Radiation Measurements. , 1972 .

[3]  J. Noxon,et al.  Nitrogen Dioxide in the Stratosphere and Troposphere Measured by Ground-Based Absorption Spectroscopy , 1975, Science.

[4]  J. Russell,et al.  About a possible reference model for stratospheric NO2 , 1987 .

[5]  R. S. Hyde,et al.  Stratospheric NO2: 1. Observational method and behavior at mid‐latitude , 1979 .

[6]  Stanley C. Solomon,et al.  On the interpretation of zenith sky absorption measurements , 1987 .

[7]  D. R. Hanson,et al.  The reaction probabilities of ClONO2 and N2O5 on 40 to 75% sulfuric acid solutions , 1991 .

[8]  David John Lary,et al.  The potential impact of the reaction OH+ClO→HCl+O2 on polar ozone photochemistry , 1995 .

[9]  Rolando R. Garcia,et al.  A new numerical model of the middle atmosphere. 2: Ozone and related species , 1994 .

[10]  F. Götz Ozone in the Atmosphere , 1951 .

[11]  G. Backus,et al.  Numerical Applications of a Formalism for Geophysical Inverse Problems , 1967 .

[12]  M. V. Roozendael,et al.  Ozone and NO2 air‐mass factors for zenith‐sky spectrometers: Intercomparison of calculations with different radiative transfer models , 1995 .

[13]  Recovery of stratospheric ozone over the United States in the winter of 1993–1994 , 1994 .

[14]  Aleksandr S. Elokhov,et al.  Estimation of tropospheric and stratospheric NO2 from spectrometric measurements of column NO2 abundances , 1995, Other Conferences.

[15]  J. Kerr,et al.  Nitrogen Dioxide Concentrations in the Atmosphere , 1973, Nature.

[16]  John J. Olivero,et al.  Retrieval error comparison for several inversion techniques used in limb-scanning millimeter-wave spectroscopy , 1995 .

[17]  J. A. Pyle,et al.  A two‐dimensional mean circulation model for the atmosphere below 80km , 1975 .

[18]  P. Crutzen The influence of nitrogen oxides on the atmospheric ozone content , 1970 .

[19]  James B. Kerr,et al.  Altitude distributions of stratospheric constituents from ground‐based measurements at twilight , 1991 .

[20]  S. Oltmans,et al.  Ozone loss in the lower stratosphere over the United States in 1992-1993: Evidence for heterogeneous chemistry on the Pinatubo aerosol , 1994 .

[21]  James M. Russell,et al.  Analysis of UARS data in the southern polar vortex in September 1992 using a chemical transport model , 1996 .

[22]  C. Rodgers,et al.  Retrieval of atmospheric temperature and composition from remote measurements of thermal radiation , 1976 .

[23]  C. Rodgers Characterization and Error Analysis of Profiles Retrieved From Remote Sounding Measurements , 1990 .

[24]  S. Solomon,et al.  On the depletion of Antarctic ozone , 1986, Nature.

[25]  Howard K. Roscoe,et al.  Ozone measurements by zenith-sky spectrometers: An evaluation of errors in air-mass factors calculated by radiative transfer models , 1995 .