Multiwavelength fluorescence lidar observations of smoke plumes

<p>A five-channel fluorescence lidar was developed for the study of atmospheric aerosol. The fluorescence spectrum induced by 355 nm laser emission is analyzed in five spectral intervals using interference filters. Central wavelengths and the widths of these five interference filters are, resp...

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Main Authors: I. Veselovskii, N. Kasianik, M. Korenskii, Q. Hu, P. Goloub, T. Podvin, D. Liu
Format: Article
Language:English
Published: Copernicus Publications 2023-04-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/16/2055/2023/amt-16-2055-2023.pdf
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author I. Veselovskii
N. Kasianik
M. Korenskii
Q. Hu
P. Goloub
T. Podvin
D. Liu
author_facet I. Veselovskii
N. Kasianik
M. Korenskii
Q. Hu
P. Goloub
T. Podvin
D. Liu
author_sort I. Veselovskii
collection DOAJ
description <p>A five-channel fluorescence lidar was developed for the study of atmospheric aerosol. The fluorescence spectrum induced by 355 nm laser emission is analyzed in five spectral intervals using interference filters. Central wavelengths and the widths of these five interference filters are, respectively, as follows: 438 and 29, 472 and 32, 513 and 29, 560 and 40, and 614 and 54 nm. The relative calibration of these channels has been performed using a tungsten–halogen lamp with a color temperature of 2800 K. This new lidar system was operated during summer–autumn 2022, when strong forest fires occurred in the Moscow region and generated a series of smoke plumes analyzed in this study. Our results demonstrate that, for urban aerosol, the maximal fluorescence backscattering is observed in a 472 nm channel. For the smoke, the maximum is shifted toward longer wavelengths, and the fluorescence backscattering coefficients in 472, 513 and 560 nm channels have comparable values. Thus, from the analysis of the ratios of fluorescence backscattering in available channels, we show that it is possible to identify smoke layers. The particle classification based on single-channel fluorescence capacity (ratio of the fluorescence backscattering to the elastic one) has limitations at high relative humidity (RH). The fluorescence capacity indeed decreases when water uptake of particles enhances the elastic scattering. However, the spectral variation of fluorescence backscattering does not exhibit any dependence on RH and can be therefore applied to aerosol identification.</p>
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spelling doaj.art-29bdb8b1c7fb4c2fbe3dcf21185dc2422023-04-18T09:13:19ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482023-04-01162055206510.5194/amt-16-2055-2023Multiwavelength fluorescence lidar observations of smoke plumesI. Veselovskii0N. Kasianik1M. Korenskii2Q. Hu3P. Goloub4T. Podvin5D. Liu6Prokhorov General Physics Institute, Russian Academy of Sciences, Moscow, RussiaProkhorov General Physics Institute, Russian Academy of Sciences, Moscow, RussiaProkhorov General Physics Institute, Russian Academy of Sciences, Moscow, RussiaUMR 8518 – LOA – Laboratoire d'Optique Atmosphérique, Univ. Lille, CNRS, 59650 Lille, FranceUMR 8518 – LOA – Laboratoire d'Optique Atmosphérique, Univ. Lille, CNRS, 59650 Lille, FranceUMR 8518 – LOA – Laboratoire d'Optique Atmosphérique, Univ. Lille, CNRS, 59650 Lille, FranceState Key Laboratory of Modern Optical Instrumentation, College of Optical Science and Engineering: International Research Center for Advanced Photonics, Zhejiang University, Hangzhou 310027, China<p>A five-channel fluorescence lidar was developed for the study of atmospheric aerosol. The fluorescence spectrum induced by 355 nm laser emission is analyzed in five spectral intervals using interference filters. Central wavelengths and the widths of these five interference filters are, respectively, as follows: 438 and 29, 472 and 32, 513 and 29, 560 and 40, and 614 and 54 nm. The relative calibration of these channels has been performed using a tungsten–halogen lamp with a color temperature of 2800 K. This new lidar system was operated during summer–autumn 2022, when strong forest fires occurred in the Moscow region and generated a series of smoke plumes analyzed in this study. Our results demonstrate that, for urban aerosol, the maximal fluorescence backscattering is observed in a 472 nm channel. For the smoke, the maximum is shifted toward longer wavelengths, and the fluorescence backscattering coefficients in 472, 513 and 560 nm channels have comparable values. Thus, from the analysis of the ratios of fluorescence backscattering in available channels, we show that it is possible to identify smoke layers. The particle classification based on single-channel fluorescence capacity (ratio of the fluorescence backscattering to the elastic one) has limitations at high relative humidity (RH). The fluorescence capacity indeed decreases when water uptake of particles enhances the elastic scattering. However, the spectral variation of fluorescence backscattering does not exhibit any dependence on RH and can be therefore applied to aerosol identification.</p>https://amt.copernicus.org/articles/16/2055/2023/amt-16-2055-2023.pdf
spellingShingle I. Veselovskii
N. Kasianik
M. Korenskii
Q. Hu
P. Goloub
T. Podvin
D. Liu
Multiwavelength fluorescence lidar observations of smoke plumes
Atmospheric Measurement Techniques
title Multiwavelength fluorescence lidar observations of smoke plumes
title_full Multiwavelength fluorescence lidar observations of smoke plumes
title_fullStr Multiwavelength fluorescence lidar observations of smoke plumes
title_full_unstemmed Multiwavelength fluorescence lidar observations of smoke plumes
title_short Multiwavelength fluorescence lidar observations of smoke plumes
title_sort multiwavelength fluorescence lidar observations of smoke plumes
url https://amt.copernicus.org/articles/16/2055/2023/amt-16-2055-2023.pdf
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AT pgoloub multiwavelengthfluorescencelidarobservationsofsmokeplumes
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