Please use this identifier to cite or link to this item: http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/10436
Title: Classification of global aerosol types and its radiative effects using Aerosol Robotic Network (AERONET) data
Authors: Mukhopadhyay, Swagata
Ningombam, Shantikumar S.
AMOGHAVARSHA, A. V.
Madhavan, B. L.
Eck, Thomas F.
Dumka, Umesh Chandra
Khatri, Pradeep
Gupta, Pawan
Dept. of Physics
Keywords: Particle linear depolarization ratio
AERONET
Inversion products
Biomass-burning aerosols
Radiative forcing
2025-SEP-WEEK5
TOC-SEP-2025
2025
Issue Date: Dec-2025
Publisher: Elsevier B.V.
Citation: Atmospheric Environment, 362, 121530.
Abstract: The present study performed classification global aerosols based on particle linear depolarization ratio (PLDR) and single scattering albedo (SSA) provided from AErosol RObotic NETwork (AERONET) Version 3.0 and Level 2.0 inversion products of 171 AERONET sites located in six continents. Current methodology could distinguish effectively between dust and non-dust aerosols using PLDR and SSA. These selected sites include dominant aerosol types such as, pure dust (PD), dust dominated mixture (DDM), pollution dominated mixture (PDM), very weakly absorbing (VWA), strongly absorbing (SA), moderately absorbing(MA), and weakly absorbing (WA). Biomass-burning aerosols which are associated with black carbon are assigned as combinations of WA, MA and SA. The key important findings show the sites in the Northern African region are predominantly influenced by PD, while south Asian sites are characterized by DDM as well as mixture of dust and pollution aerosols. Urban and industrialized regions located in Europe and North American sites are characterized by VWA, WA, and MA aerosols. Tropical regions, including South America, South-east-Asia and southern African sites which prone to forest and biomass-burning, are dominated by SA aerosols. The study further examined the impacts by radiative forcing for different aerosol types. Among the aerosol types, SA and VWA contribute with the highest (30.14 ± 8.04 Wm−2) and lowest (7.83 ± 4.12 Wm−2) atmospheric forcing, respectively. Consequently, atmospheric heating rates are found to be highest by SA (0.85 K day−1) and lowest by VWA aerosols (0.22 Kday−1). The current study provides a comprehensive report on aerosol optical, micro-physical and radiative properties for different aerosol types across six continents.
URI: https://doi.org/10.1016/j.atmosenv.2025.121530
http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/10436
ISSN: 1352-2310
1873-2844
Appears in Collections:JOURNAL ARTICLES

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