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  4. Assessment of lidar depolarization uncertainty by means of a polarimetric lidar simulator
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Assessment of lidar depolarization uncertainty by means of a polarimetric lidar simulator

Journal
Atmospheric Measurement Techniques
Date Issued
October 7, 2016
Author(s)
Bravo-Aranda, Juan Antonio  
Belegante, Livio  
Freudenthaler, Volker  
Alados-Arboledas, Lucas  
Nicolae, Doina Nicoleta  
Granados-Munõz, María José  
Luis Guerrero-Rascado, J. L.  
Amodeo, Aldo  
D'Amico, Giusseppe  
Engelmann, R.  
Pappalardo, Gelsomina  
Kokkalis, Panayotis  
Mamouri, Rodanthi-Elisavet  
Papayannis, Alexandros D.  
Navas-Guzmán, Francisco  
José Olmo, Francisco  
Wandinger, Ulla  
Amato, Francesco  
Haeffelin, Martial  
DOI
10.5194/amt-9-4935-2016
Abstract
Lidar depolarization measurements distinguish between spherical and non-spherical aerosol particles based on the change of the polarization state between the emitted and received signal. The particle shape information in combination with other aerosol optical properties allows the characterization of different aerosol types and the retrieval of aerosol particle microphysical properties. Regarding the microphysical inversions, the lidar depolarization technique is becoming a key method since particle shape information can be used by algorithms based on spheres and spheroids, optimizing the retrieval procedure. Thus, the identification of the depolarization error sources and the quantification of their effects are crucial. This work presents a new tool to assess the systematic error of the volume linear depolarization ratio (δ), combining the Stokes-Müller formalism and the complete sampling of the error space using the lidar model presented in Freudenthaler (2016a). This tool is applied to a synthetic lidar system and to several EARLINET lidars with depolarization capabilities at 355 or 532 nm. The lidar systems show relative errors of δ larger than 100% for δ values around molecular linear depolarization ratios (∼ 0.004 and up to ∼ 10 % for δ = 0.45). However, one system shows only relative errors of 25 and 0.22% for δ = 0.004 and δ = 0.45, respectively, and gives an example of how a proper identification and reduction of the main error sources can drastically reduce the systematic errors of δ. In this regard, we provide some indications of how to reduce the systematic errors.
Funding(s)
ACTRIS PPP - Aerosols, Clouds and Trace gases Preparatory Phase Project  
Subjects

Depolarization measur...

Spherical and non-sph...

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Mamouri.pdf

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Format

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Checksum (MD5)

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