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

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Comparison of box-air-mass-factors and radiances for Multiple-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) geometries calculated from different UV/visible radiative transfer models (2006, background): “The inﬂuence of additional aerosol scattering not only affects the dependence of the radiance and box-AMFs on the elevation angle but also on the relative azimuth angle (Wagner et al., 2004; Frieß et al., 2006).”
First retrieval of tropospheric aerosol profiles using MAX-DOAS and comparison with lidar and sky radiometer measurements (2008, methodology): “These agreements may indicate that the vertical resolution at altitudes below 2 km was roughly 1 km, corresponding to the vertical spacing chosen in the parameterization ofk, consistent with the simulation done by Frieβ et al. (2006).”
Radiative transfer corrections for accurate spectroscopic measurements of volcanic gas emissions (2010, methodology): “measuring oxygen dimer absorption (Wagner et al. 2004; Fries et al. 2006 ).”
The Monte Carlo atmospheric radiative transfer model McArtim: Introduction and validation of Jacobians and 3D features (2011, background): “[30–32]) for aerosol property retrievals, or for interpreting spectroscopic measurements with respect to ice and liquid water paths.”