Please use this identifier to cite or link to this item: http://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/10436
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dc.contributor.authorMukhopadhyay, Swagataen_US
dc.contributor.authorNingombam, Shantikumar S.en_US
dc.contributor.authorAMOGHAVARSHA, A. V.en_US
dc.contributor.authorMadhavan, B. L.en_US
dc.contributor.authorEck, Thomas F.en_US
dc.contributor.authorDumka, Umesh Chandraen_US
dc.contributor.authorKhatri, Pradeepen_US
dc.contributor.authorGupta, Pawanen_US
dc.date.accessioned2025-09-29T06:33:24Z
dc.date.available2025-09-29T06:33:24Z
dc.date.issued2025-12en_US
dc.identifier.citationAtmospheric Environment, 362, 121530.en_US
dc.identifier.issn1352-2310en_US
dc.identifier.issn1873-2844en_US
dc.identifier.urihttps://doi.org/10.1016/j.atmosenv.2025.121530en_US
dc.identifier.urihttp://dr.iiserpune.ac.in:8080/xmlui/handle/123456789/10436
dc.description.abstractThe 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.en_US
dc.language.isoenen_US
dc.publisherElsevier B.V.en_US
dc.subjectParticle linear depolarization ratioen_US
dc.subjectAERONETen_US
dc.subjectInversion productsen_US
dc.subjectBiomass-burning aerosolsen_US
dc.subjectRadiative forcingen_US
dc.subject2025-SEP-WEEK5en_US
dc.subjectTOC-SEP-2025en_US
dc.subject2025en_US
dc.titleClassification of global aerosol types and its radiative effects using Aerosol Robotic Network (AERONET) dataen_US
dc.typeArticleen_US
dc.contributor.departmentDept. of Physicsen_US
dc.identifier.sourcetitleAtmospheric Environmenten_US
dc.publication.originofpublisherForeignen_US
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