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Changing optical properties of black carbon and brown carbon aerosols during long-range transport from the Indo-Gangetic Plain to the equatorial Indian Ocean

Atmospheric aerosols strongly influence the global climate through their light absorption properties (e.g., black carbon (BC) and brown carbon (BrC)) and scattering properties (e.g., sulfate). This study presents simultaneous measurements of ambient-aerosol light absorption properties and chemical c...

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Published in:Atmospheric chemistry and physics 2024-10, Vol.24 (20), p.11911-11925
Main Authors: Budhavant, Krishnakant, Manoj, Mohanan Remani, Nair, Hari Ram Chandrika Rajendran, Gaita, Samuel Mwaniki, Holmstrand, Henry, Salam, Abdus, Muslim, Ahmed, Satheesh, Sreedharan Krishnakumari, Gustafsson, Örjan
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container_end_page 11925
container_issue 20
container_start_page 11911
container_title Atmospheric chemistry and physics
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creator Budhavant, Krishnakant
Manoj, Mohanan Remani
Nair, Hari Ram Chandrika Rajendran
Gaita, Samuel Mwaniki
Holmstrand, Henry
Salam, Abdus
Muslim, Ahmed
Satheesh, Sreedharan Krishnakumari
Gustafsson, Örjan
description Atmospheric aerosols strongly influence the global climate through their light absorption properties (e.g., black carbon (BC) and brown carbon (BrC)) and scattering properties (e.g., sulfate). This study presents simultaneous measurements of ambient-aerosol light absorption properties and chemical composition obtained at three large-footprint southern Asian receptor sites during the South Asian Pollution Experiment (SAPOEX) from December 2017 to March 2018. The BC mass absorption cross section (BC-MAC678) values increased from 3.5 ± 1.3 at the Bangladesh Climate Observatory at Bhola (BCOB), located at the exit outflow of the Indo-Gangetic Plain, to 6.4 ± 1.3 at two regional receptor observatories, the Maldives Climate Observatory at Hanimaadhoo (MCOH) and the Maldives Climate Observatory at Gan (MCOG), representing an increase of 80 %. This likely reflects a scavenging fractionation, resulting in a population of finer BC with higher MAC678 that has greater longevity. At the same time, BrC-MAC365 decreased by a factor of 3 from the Indo-Gangetic Plain (IGP) exit to the equatorial Indian Ocean, likely due to photochemical bleaching of organic chromophores. The high chlorine-to-sodium ratio at the BCOB, located near the source region, suggests a significant contribution of chorine from anthropogenic activities. Particulate Cl− has the potential to be converted into Cl radicals, which can affect the oxidation capacity of polluted air. Moreover, Cl− is shown to be nearly fully consumed during long-range transport. The results of this synoptic study, conducted on a large southern Asian scale, provide rare observational constraints on the optical properties of ambient BC (and BrC) aerosols over regional scales, away from emission sources. They also contribute significantly to understanding the aging effect of the optical and chemical properties of aerosols as pollution from the Indo-Gangetic Plain disperses over the tropical ocean.
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This study presents simultaneous measurements of ambient-aerosol light absorption properties and chemical composition obtained at three large-footprint southern Asian receptor sites during the South Asian Pollution Experiment (SAPOEX) from December 2017 to March 2018. The BC mass absorption cross section (BC-MAC678) values increased from 3.5 ± 1.3 at the Bangladesh Climate Observatory at Bhola (BCOB), located at the exit outflow of the Indo-Gangetic Plain, to 6.4 ± 1.3 at two regional receptor observatories, the Maldives Climate Observatory at Hanimaadhoo (MCOH) and the Maldives Climate Observatory at Gan (MCOG), representing an increase of 80 %. This likely reflects a scavenging fractionation, resulting in a population of finer BC with higher MAC678 that has greater longevity. At the same time, BrC-MAC365 decreased by a factor of 3 from the Indo-Gangetic Plain (IGP) exit to the equatorial Indian Ocean, likely due to photochemical bleaching of organic chromophores. The high chlorine-to-sodium ratio at the BCOB, located near the source region, suggests a significant contribution of chorine from anthropogenic activities. Particulate Cl− has the potential to be converted into Cl radicals, which can affect the oxidation capacity of polluted air. Moreover, Cl− is shown to be nearly fully consumed during long-range transport. The results of this synoptic study, conducted on a large southern Asian scale, provide rare observational constraints on the optical properties of ambient BC (and BrC) aerosols over regional scales, away from emission sources. 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ispartof Atmospheric chemistry and physics, 2024-10, Vol.24 (20), p.11911-11925
issn 1680-7324
1680-7316
1680-7324
language eng
recordid cdi_doaj_primary_oai_doaj_org_article_b4981d8d16c048b3ab259d51a2b2e69a
source Publicly Available Content Database; DOAJ Directory of Open Access Journals; Alma/SFX Local Collection
subjects Absorption
Absorption cross sections
Aerosol absorption
Aerosol light absorption
Aerosols
Air pollution
Analysis
Anthropogenic factors
Atmospheric aerosols
Atmospheric physics
Biomass
Black carbon
Bleaching
Carbon
Carbon aerosols
Chemical composition
Chemical properties
Chemicophysical properties
Chlorine
Chromophores
Climate
Electromagnetic absorption
Equatorial regions
Fractionation
Global climate
Human influences
Light absorption
Long-range transport
Observatories
Ocean
Oceans
Optical properties
Outdoor air quality
Oxidation
Photochemicals
Photochemistry
Pollution
Pollution sources
Receptors
Scavenging
Sodium
Sulfates
VOCs
Volatile organic compounds
Wind
title Changing optical properties of black carbon and brown carbon aerosols during long-range transport from the Indo-Gangetic Plain to the equatorial Indian Ocean
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