Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol Weather

Considering the wide range of variability of all aerosol characteristics (especially in the near-ground layer of the atmosphere near industrial centers), when creating a realistic empirical model of optical and microphysical characteristics, the optimal dividing of the total data array according to...

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Main Authors: Mikhail V. Panchenko, Valerii S. Kozlov, Victor V. Polkin, Svetlana A. Terpugova, Vasily V. Polkin, Victor N. Uzhegov, Dmitry G. Chernov, Vladimir P. Shmargunov, Elena P. Yausheva, Polina N. Zenkova
Format: Article
Language:English
Published: MDPI AG 2019-12-01
Series:Atmosphere
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Online Access:https://www.mdpi.com/2073-4433/11/1/20
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author Mikhail V. Panchenko
Valerii S. Kozlov
Victor V. Polkin
Svetlana A. Terpugova
Vasily V. Polkin
Victor N. Uzhegov
Dmitry G. Chernov
Vladimir P. Shmargunov
Elena P. Yausheva
Polina N. Zenkova
author_facet Mikhail V. Panchenko
Valerii S. Kozlov
Victor V. Polkin
Svetlana A. Terpugova
Vasily V. Polkin
Victor N. Uzhegov
Dmitry G. Chernov
Vladimir P. Shmargunov
Elena P. Yausheva
Polina N. Zenkova
author_sort Mikhail V. Panchenko
collection DOAJ
description Considering the wide range of variability of all aerosol characteristics (especially in the near-ground layer of the atmosphere near industrial centers), when creating a realistic empirical model of optical and microphysical characteristics, the optimal dividing of the total data array according to some multifactor signs is needed. In this paper, we analyze the main states of &#8220;dry&#8221; aerosol on the basis of the results of long-term regular measurements in the near-ground layer of the atmosphere near the city of Tomsk in 2000&#8722;2017. The following parameters were considered: aerosol number concentration and size distribution function, total and angular scattering coefficients, including the small-angle range 1.2&#176; to 20&#176;, mass concentration and size distribution of absorbing substances (equivalent black carbon), characteristics of the aerosol hygroscopic properties, and spectral aerosol extinction of radiation on an open long path in the wavelength range 0.45 to 3.9 &#181;m. In our comprehensive study, we first proposed and developed an original approach (classification) to study the optical and microphysical properties of atmospheric aerosol of various physicochemical origins (background, smoke, smog, anthropogenic, etc.) based on dividing the entire data array into characteristic subarrays (types of aerosol weather), which differ from each other in a different combination of scattering and absorbing properties of particles. To divide the total data array into types of aerosol weather including &#8220;Background&#8221;, &#8220;Haze-S&#8221;, &#8220;Smog&#8221;, and &#8220;Smoke haze&#8221;, the values of the scattering coefficient of the dry aerosol matter &#963;<sub>d</sub>(&#955; = 0.51 &#956;m) = 100 Mm<sup>&#8722;1</sup> and the ratio of the mass concentration of the absorbing substance to the mass concentration of submicron aerosol <i>P</i> = 0.05. The results showed that most of the seasonal average values of the aerosol parameters analyzed in the paper are statistically significantly different when comparing various characteristic types of scattering and absorbing atmospheric aerosol. The results of the research indicate that the application of the developed classification of types of aerosol weather for the analyzed optical and microphysical parameters of aerosol particles is quite effective and reasonable.
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spelling doaj.art-c40d1361f7ad4ba5a61cfae130b632732022-12-21T17:59:04ZengMDPI AGAtmosphere2073-44332019-12-011112010.3390/atmos11010020atmos11010020Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol WeatherMikhail V. Panchenko0Valerii S. Kozlov1Victor V. Polkin2Svetlana A. Terpugova3Vasily V. Polkin4Victor N. Uzhegov5Dmitry G. Chernov6Vladimir P. Shmargunov7Elena P. Yausheva8Polina N. Zenkova9V.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaV.E. Zuev Institute of Atmospheric Optics, 1, Ak. Zuev square, Tomsk 634055, RussiaConsidering the wide range of variability of all aerosol characteristics (especially in the near-ground layer of the atmosphere near industrial centers), when creating a realistic empirical model of optical and microphysical characteristics, the optimal dividing of the total data array according to some multifactor signs is needed. In this paper, we analyze the main states of &#8220;dry&#8221; aerosol on the basis of the results of long-term regular measurements in the near-ground layer of the atmosphere near the city of Tomsk in 2000&#8722;2017. The following parameters were considered: aerosol number concentration and size distribution function, total and angular scattering coefficients, including the small-angle range 1.2&#176; to 20&#176;, mass concentration and size distribution of absorbing substances (equivalent black carbon), characteristics of the aerosol hygroscopic properties, and spectral aerosol extinction of radiation on an open long path in the wavelength range 0.45 to 3.9 &#181;m. In our comprehensive study, we first proposed and developed an original approach (classification) to study the optical and microphysical properties of atmospheric aerosol of various physicochemical origins (background, smoke, smog, anthropogenic, etc.) based on dividing the entire data array into characteristic subarrays (types of aerosol weather), which differ from each other in a different combination of scattering and absorbing properties of particles. To divide the total data array into types of aerosol weather including &#8220;Background&#8221;, &#8220;Haze-S&#8221;, &#8220;Smog&#8221;, and &#8220;Smoke haze&#8221;, the values of the scattering coefficient of the dry aerosol matter &#963;<sub>d</sub>(&#955; = 0.51 &#956;m) = 100 Mm<sup>&#8722;1</sup> and the ratio of the mass concentration of the absorbing substance to the mass concentration of submicron aerosol <i>P</i> = 0.05. The results showed that most of the seasonal average values of the aerosol parameters analyzed in the paper are statistically significantly different when comparing various characteristic types of scattering and absorbing atmospheric aerosol. The results of the research indicate that the application of the developed classification of types of aerosol weather for the analyzed optical and microphysical parameters of aerosol particles is quite effective and reasonable.https://www.mdpi.com/2073-4433/11/1/20aerosolscatteringabsorptionextinctionsize distributionhygroscopic growth
spellingShingle Mikhail V. Panchenko
Valerii S. Kozlov
Victor V. Polkin
Svetlana A. Terpugova
Vasily V. Polkin
Victor N. Uzhegov
Dmitry G. Chernov
Vladimir P. Shmargunov
Elena P. Yausheva
Polina N. Zenkova
Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol Weather
Atmosphere
aerosol
scattering
absorption
extinction
size distribution
hygroscopic growth
title Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol Weather
title_full Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol Weather
title_fullStr Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol Weather
title_full_unstemmed Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol Weather
title_short Aerosol Characteristics in the Near-Ground Layer of the Atmosphere of the City of Tomsk in Different Types of Aerosol Weather
title_sort aerosol characteristics in the near ground layer of the atmosphere of the city of tomsk in different types of aerosol weather
topic aerosol
scattering
absorption
extinction
size distribution
hygroscopic growth
url https://www.mdpi.com/2073-4433/11/1/20
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