Title:
Assessment of equivalent black carbon variations and its source apportionment over Varanasi, Indo-Gangetic Basin

dc.contributor.authorPrashant Kumar Chauhan
dc.contributor.authorShani Tiwari
dc.contributor.authorDileep Kumar Gupta
dc.contributor.authorAkhilesh Kumar
dc.contributor.authorVineet Pratap
dc.contributor.authorAbhay Kumar Singh
dc.date.accessioned2026-02-09T04:31:51Z
dc.date.issued2024
dc.description.abstractIn this study, the temporal variation of Equivalent Black Carbon (eBC) and its source apportionment is studied using a yearlong (Dec. 2020–Nov. 2021) multiwavelength Aethalometer (AE-33 model) measurements over Varanasi, located in the central Indo-Gangetic Basin (IGB). Results suggest that mean mass concentrations of eBC vary in the range between 0.46 ± 0.13 to 11.22 ± 5.09 μg m−3 with an annual mean value of ∼3.57 ± 2.39 μg m−3 during the study period. A strong temporal variation in eBC and its components i.e., eBCff (eBC from fossil fuel), and eBCbb (eBC from biomass burning) are found which shows a large variation on different temporal scales with an average value during winter (6.21 ± 3.56 μg m−3), summer (5.09 ± 3.61 μg m−3), monsoon season (1.52 ± 1.03 μg m−3), and post-monsoon (3.75 ± 2.68 μg m−3). The diurnal variation of eBC shows two different maxima between 07:00–08:00 a.m. and 08:00–10:00 p.m. An inverse relationship between eBC concentration and all meteorological parameters (temperature, wind speed, and boundary layer height) is found except relative humidity. The concentration of eBC increases with respect to RH (up to 70 %) suggesting hygroscopic growth while for higher RH (>70 %) value, eBC concentration decreases and indicates the possible wet scavenging processes in the atmosphere. Source apportionment of eBC using the “Aethalometer Model” reveals that eBCff is dominant over eBCbb in total eBC loading during the study period. Cluster analysis of HYSPLIT (Hybrid Single Particle Lagrangian Integrated Trajectory) model computed five days airmass back-trajectory suggests that airmass reached at Varanasi passes through a highly dense fire count region over the northwestern IGB and surrounding which could be the most responsible for the black carbon loading over the study region. © 2024 Turkish National Committee for Air Pollution Research and Control
dc.identifier.doi10.1016/j.apr.2024.102061
dc.identifier.issn13091042
dc.identifier.urihttps://doi.org/10.1016/j.apr.2024.102061
dc.identifier.urihttps://dl.bhu.ac.in/bhuir/handle/123456789/48198
dc.publisherElsevier B.V.
dc.subjectBiomass burning
dc.subjectBlack carbon (BC)
dc.subjectFire counts
dc.subjectFossil fuel
dc.subjectIndo-Gangetic Basin
dc.subjectLong range transport
dc.titleAssessment of equivalent black carbon variations and its source apportionment over Varanasi, Indo-Gangetic Basin
dc.typePublication
dspace.entity.typeArticle

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