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Multiangle photopolarimetric aerosol retrievals in the vicinity of clouds: Synthetic study based on a large eddy simulation
Author(s) -
Stap F. A.,
Hasekamp O. P.,
Emde C.,
Röckmann T.
Publication year - 2016
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2016jd024787
Subject(s) - aerosol , radiative transfer , atmospheric radiative transfer codes , environmental science , remote sensing , optical depth , atmospheric sciences , albedo (alchemy) , image resolution , meteorology , physics , geology , optics , art history , art , performance art
We investigate the effect of cloud contamination and 3‐D radiative transfer effects on aerosol retrievals from multiangle photopolarimetric measurements in the vicinity of clouds. To this end multiangle, multiwavelength photopolarimetric observations are simulated using a 3‐D radiative transfer model for scenes with realistic cloud properties, based on a large eddy simulation. Spatial resolutions of 2 × 2, 4 × 4, and 6 × 6 km 2 have been considered. It is found that a goodness‐of‐fit criterion efficiently filters out cloud contamination. However, it does not filter out all scenes that are affected by 3‐D radiative effects, resulting in small biases in the retrieved aerosol optical thickness (AOT) and single‐scattering albedo (SSA). We also found that measurements at higher spatial resolution (2 × 2 km 2 ) do not result in retrievals closer to clouds compared to measurements at coarser spatial resolutions (4 × 4 and 6 × 6 km 2 ). If cloud parameters are fitted simultaneously with aerosol parameters using a 1‐D radiative transfer model and the Independent Pixel Approximation, more successful retrievals are obtained in partially cloudy scenes and in the vicinity of clouds. This effect is most apparent at 6 × 6 km 2 and only marginal at 2 × 2 km 2 resolution. The retrieved aerosol AOT and SSA from the simultaneous aerosol and cloud retrievals still have a small bias, like the aerosol‐only retrievals. We conclude that in order to substantially improve aerosol retrievals in the vicinity of clouds, a retrieval algorithm is needed that takes into account 3‐D radiative transfer effects.