Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength Relationship

Aerosols are composed of suspended solid or liquid particles and interact with solar radiation through absorption, refraction, and scattering, influencing climate variability. The Ångström exponent (α) is commonly used to differentiate particle sizes, but its relationship with aerosol optical depth...

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Main Author: Dyi-Huey Chang
Format: Article
Language:English
Published: MDPI AG 2025-04-01
Series:Engineering Proceedings
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Online Access:https://www.mdpi.com/2673-4591/91/1/1
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author Dyi-Huey Chang
author_facet Dyi-Huey Chang
author_sort Dyi-Huey Chang
collection DOAJ
description Aerosols are composed of suspended solid or liquid particles and interact with solar radiation through absorption, refraction, and scattering, influencing climate variability. The Ångström exponent (α) is commonly used to differentiate particle sizes, but its relationship with aerosol optical depth (AOD) and wavelength (λ) is non-linear. This relationship is modeled using higher-order polynomial expressions in this study based on the AOD data from the AErosol RObotic NETwork (AERONET). In the model, polynomial coefficients are used to effectively classify aerosol types, such as dust and biomass-burning aerosols, with a strong correlation among coefficients of the same order. Such a close correlation among the coefficients of the same polynomial order is attributed to a large variability. The coefficients of the same order exhibit a scaled relationship, where scaling factors are expressed as a function of wavelength.
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spelling doaj-art-f4f6a658ff9841b781c32c746089bbdf2025-08-20T03:24:35ZengMDPI AGEngineering Proceedings2673-45912025-04-01911110.3390/engproc2025091001Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength RelationshipDyi-Huey Chang0Department of Environmental Engineering and Management, Chaoyang University of Technology, Taichung 413310, TaiwanAerosols are composed of suspended solid or liquid particles and interact with solar radiation through absorption, refraction, and scattering, influencing climate variability. The Ångström exponent (α) is commonly used to differentiate particle sizes, but its relationship with aerosol optical depth (AOD) and wavelength (λ) is non-linear. This relationship is modeled using higher-order polynomial expressions in this study based on the AOD data from the AErosol RObotic NETwork (AERONET). In the model, polynomial coefficients are used to effectively classify aerosol types, such as dust and biomass-burning aerosols, with a strong correlation among coefficients of the same order. Such a close correlation among the coefficients of the same polynomial order is attributed to a large variability. The coefficients of the same order exhibit a scaled relationship, where scaling factors are expressed as a function of wavelength.https://www.mdpi.com/2673-4591/91/1/1AERONETÅngström exponentaerosol optical depth
spellingShingle Dyi-Huey Chang
Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength Relationship
Engineering Proceedings
AERONET
Ångström exponent
aerosol optical depth
title Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength Relationship
title_full Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength Relationship
title_fullStr Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength Relationship
title_full_unstemmed Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength Relationship
title_short Classifying Aerosol Particle Size Using Polynomial Coefficient of Aerosol Optical Depth–Wavelength Relationship
title_sort classifying aerosol particle size using polynomial coefficient of aerosol optical depth wavelength relationship
topic AERONET
Ångström exponent
aerosol optical depth
url https://www.mdpi.com/2673-4591/91/1/1
work_keys_str_mv AT dyihueychang classifyingaerosolparticlesizeusingpolynomialcoefficientofaerosolopticaldepthwavelengthrelationship