A novel laboratory methodology to evaluate the particle extinction-to-backscatter ratio or particle lidar ratio of aerosols

While atmospheric particles are ubiquitous in nature and contribute to the Earth’s radiative budget, their backscattering and extinction remain insufficiently quantified due to their complexity in size, shape and chemical composition. In this paper, a novel laboratory methodology is proposed to evaluate the particle extinction-to-backscatter ratio or lidar ratio of aerosols. This methodology, called LR-lab, is based on a robust light backscatter experiment at 180.0° angle, enhanced with a cavity ring down experiment to evaluate the particle extinction. No assumption is required on the particle size, shape, nor complex refractive index. Our methodology is validated on homogeneous spherical water droplets, which follow the analytical Mie theory, for different water droplets sizes and number concentrations. The particle extinction-to-backscatter ratio of mineral dust, a heterogeneous mixture of non-spherical particles, is then evaluated at 532 nm wavelength in laboratory. The dust lidar ratio is found to be equal to (47 ± 2) sr while the dust depolarization ratio is equal to (33.6 ± 0.4) %. By proposing a combined laboratory evaluation of the particle lidar and depolarization ratios, we believe our methodology can meet the growing need for lidar-based aerosol typing and for validation of light scattering numerical models on complex-shaped particles.

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Publication Details

Journal
Scientific Reports
Published
2026-07-23
DOI
https://doi.org/10.1038/s41598-026-61997-3
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
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article

A novel laboratory methodology to evaluate the particle extinction-to-backscatter ratio or particle lidar ratio of aerosols

Alain Miffre, Adrien P. Genoud, Clément PACORET-BERENGER, Patrick Rairoux
Scientific Reports
Atmospheric aerosols and clouds
article

A novel laboratory methodology to evaluate the particle extinction-to-backscatter ratio or particle lidar ratio of aerosols

Alain Miffre, Adrien P. Genoud, Clément PACORET-BERENGER, Patrick Rairoux
article en

Abstract

While atmospheric particles are ubiquitous in nature and contribute to the Earth’s radiative budget, their backscattering and extinction remain insufficiently quantified due to their complexity in size, shape and chemical composition. In this paper, a novel laboratory methodology is proposed to evaluate the particle extinction-to-backscatter ratio or lidar ratio of aerosols. This methodology, called LR-lab, is based on a robust light backscatter experiment at 180.0° angle, enhanced with a cavity ring down experiment to evaluate the particle extinction. No assumption is required on the particle size, shape, nor complex refractive index. Our methodology is validated on homogeneous spherical water droplets, which follow the analytical Mie theory, for different water droplets sizes and number concentrations. The particle extinction-to-backscatter ratio of mineral dust, a heterogeneous mixture of non-spherical particles, is then evaluated at 532 nm wavelength in laboratory. The dust lidar ratio is found to be equal to (47 ± 2) sr while the dust depolarization ratio is equal to (33.6 ± 0.4) %. By proposing a combined laboratory evaluation of the particle lidar and depolarization ratios, we believe our methodology can meet the growing need for lidar-based aerosol typing and for validation of light scattering numerical models on complex-shaped particles.

Scientific Reports
Université Claude Bernard Lyon 1 (FR), Centre National de la Recherche Scientifique (FR)
Openalex Percentile: Top 11%
Atmospheric aerosols and clouds
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