Comparison of measured and modeled stratospheric UV/Visible actinic fluxes at large solar zenith angles

Measured and modeled stratospheric filter sensitivity weighted ultraviolet/visible (UV/vis) actinic fluxes—approximating the NO2 photolysis rate coefficients (jNO2)— are compared. The measurements were performed with two calibrated 2π-actinometers assembled on the azimuth angle-controlled LPMA/DOAS (Laboratoire de Physique Moleculaire et Applications/Differential Optical Absorption Spectroscopy) gondola during a series of balloon flights. Since the actinometer's spectral sensitivity curve did not exactly match the actinic spectrum of NO2 and the skylight's spectrum shape changes with atmospheric height and solar illumination, only proxies (proxy-)jNO2 rather than true jNO2 values were monitored during balloon ascents (0–30 km) for solar zenith angle (SZA) 75° < SZA < 86°, and at balloon float altitude during solar occultation (86° < SZA < 95°). The measured direct and diffuse total proxy-jNO2 values compare excellently with radiative transfer (RT) modeling. That finding allows us to rule out uncertainties in computing UV/vis actinic fluxes as a significant factor in the still insufficient modeling of stratospheric NO2 at large SZAs.

[1]  S. Madronich Photodissociation in the atmosphere: 1. Actinic flux and the effects of ground reflections and clouds , 1987 .

[2]  S. Madronich,et al.  Visible‐ultraviolet absorption cross sections for NO2 as a function of temperature , 1988 .

[3]  Arve Kylling,et al.  Efficient yet accurate solution of the linear transport equation in the presence of internal sources - The exponential-linear-in-depth approximation , 1992 .

[4]  M. Molina,et al.  Absolute absorption cross sections of ozone in the 185- to 350-nm wavelength range , 1986 .

[5]  M. Nicolet,et al.  Radiation field in the troposphere and stratosphere—II. Numerical analysis , 1982 .

[6]  A. Ravishankara,et al.  Reconsideration of the rate constant for the reaction of hydroxyl radicals with nitric acid , 1999 .

[7]  Ulrich Platt,et al.  A photoelectric detector for the measurement of photolysis frequencies of ozone and other atmospheric molecules , 1989 .

[8]  Martyn P. Chipperfield,et al.  Multiannual simulations with a three‐dimensional chemical transport model , 1999 .

[9]  A sensitivity study of photolysis rate coefficients during POLARIS , 1999 .

[10]  M. Nicolet,et al.  On the molecular scattering in the terrestrial atmosphere : An empirical formula for its calculation in the homosphere , 1984 .

[11]  Ulrich Schmidt,et al.  Ultraviolet actinic flux in the stratosphere: An overview of balloon‐borne measurements during EASOE, 1991/92 , 1994 .

[12]  M. Molina,et al.  Chemical kinetics and photochemical data for use in stratospheric modeling , 1985 .

[13]  D. Weisenstein,et al.  A comparison of observations and model simulations of NOx/NOy in the lower stratosphere , 1999 .

[14]  David John Lary,et al.  Diffuse radiation, twilight, and photochemistry — I , 1991 .

[15]  D. K. Prinz,et al.  Validation of the UARS solar ultraviolet irradiances: Comparison with the ATLAS 1 and 2 measurements , 1996 .

[16]  E. Shettle Models of aerosols, clouds, and precipitation for atmospheric propagation studies , 1990 .

[17]  H. Oelhaf,et al.  Ozone loss rates in the Arctic stratosphere in the winter 1994/1995 : Model simulations underestimate results of the Match analysis , 2000 .

[18]  Charles Thomas McElroy,et al.  Comparison of modeled and observed values of NO2 and JNO2 during the Photochemistry of Ozone Loss in the Arctic Region in Summer (POLARIS) mission , 1999 .

[19]  M. Nicolet,et al.  Radiation field in the troposphere and stratosphere from 240-1000 NM. I - General analysis. II - Numerical analysis , 1982 .

[20]  John J. Orlando,et al.  Temperature Dependence of the Quantum Yields for the Photolysis of NO2 Near the Dissociation Limit , 1994 .