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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • atmospheric aerosol
  • MAX-DOAS
  • inverse modeling

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Radiation: transmission and scattering
  • Atmospheric Composition and Structure: Instruments and techniques
Abstract
Cited By (10)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, D14203, 20 PP., 2006
doi:10.1029/2005JD006618

MAX-DOAS O4 measurements: A new technique to derive information on atmospheric aerosols: 2. Modeling studies

U. Frieß

Institute for Environmental Physics, University of Heidelberg, Heidelberg, Germany

P. S. Monks

Space Research Centre, University of Leicester, Leicester, UK

J. J. Remedios

Space Research Centre, University of Leicester, Leicester, UK

A. Rozanov

Institute of Environmental Physics, University of Bremen, Bremen, Germany

R. Sinreich

Institute for Environmental Physics, University of Heidelberg, Heidelberg, Germany

T. Wagner

Institute for Environmental Physics, University of Heidelberg, Heidelberg, Germany

U. Platt

Institute for Environmental Physics, University of Heidelberg, Heidelberg, Germany

A new retrieval algorithm for the determination of aerosol properties using Multi-AXis Differential Optical Absorption Spectroscopy (MAX-DOAS) measurements based on nonlinear optimal estimation is presented. Using simulated MAX-DOAS measurements of the optical depth of the collision complex of oxygen (O4) as well as the variation of the intensity of diffuse skylight measured at different viewing directions and wavelengths, the capability of this measurement technique to derive the aerosol extinction profile as well as information on the phase function and single scattering albedo is demonstrated. The information content, vertical resolution and retrieval errors under various atmospheric conditions are discussed. Furthermore, it is demonstrated that the assumption of a smooth variation of the aerosol properties between successive measurements can be used to improve the quality of the retrieval by applying a Kalman smoother. The results of these model studies suggest that the achievable precision of MAX-DOAS measurements of the aerosol total optical depth is better than 0.01 and thus comparable with established methods of aerosol detection by Sun photometers (e.g., within the AERONET network) over a wide range of atmospheric conditions. Moreover, MAX-DOAS measurements contain information on the vertical profile of the aerosol extinction, and can be performed with relatively simple, robust and self-calibrating instruments.

Received 24 August 2005; accepted 7 April 2006; published 19 July 2006.

Citation: Frieß, U., P. S. Monks, J. J. Remedios, A. Rozanov, R. Sinreich, T. Wagner, and U. Platt (2006), MAX-DOAS O4 measurements: A new technique to derive information on atmospheric aerosols: 2. Modeling studies, J. Geophys. Res., 111, D14203, doi:10.1029/2005JD006618.

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