Seasonal contrast in size distributions and mixing state of black carbon and its association with PM_1.0 chemical composition from the eastern coast of India

• Main Authors: S. K. Kompalli, S. N. Suresh Babu, S. K. Satheesh, K. Krishna Moorthy, T. Das, R. Boopathy, D. Liu, E. Darbyshire, J. D. Allan, J. Brooks, M. J. Flynn, H. Coe
• Format: Article
• Language: English
• Published: Copernicus Publications 2020-04-01
• Series: Atmospheric Chemistry and Physics
• Online Access: https://www.atmos-chem-phys.net/20/3965/2020/acp-20-3965-2020.pdf

<p><span id="page3966"/>Over the Indian region, aerosol absorption is considered to have a potential impact on the regional climate, monsoon and hydrological cycle. Black carbon (BC) is the dominant absorbing aerosol, whose absorption potential is determined mainly by its microphysical properties, including its concentration, size and mixing state with other aerosol components. The Indo-Gangetic Plain (IGP) is one of the regional aerosol hot spots with diverse sources, both natural and anthropogenic, but still the information on the mixing state of the IGP aerosols, especially BC, is limited and a significant source of uncertainty in understanding their climatic implications. In this context, we present the results from intensive measurements of refractory BC (<span class="inline-formula"><i>r</i>_BC</span>) carried out over Bhubaneswar, an urban site in the eastern coast of India, which experiences contrasting air masses (the IGP outflow or coastal/marine air masses) in different seasons. This study helps to elucidate the microphysical characteristics of BC over this region and delineates the IGP outflow from the other air masses. The observations were carried out as part of South West Asian Aerosol Monsoon Interactions (SWAAMI) collaborative field experiment during July 2016–May 2017, using a single-particle soot photometer (SP2) that uses a laser-induced incandescence technique to measure the mass and mixing state of individual BC particles and an aerosol chemical speciation monitor (ACSM) to infer the possible coating material. Results highlighted the distinctiveness in aerosol microphysical properties in the IGP air masses. BC mass concentration was highest during winter (December–February) (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">1.94</mn><mo>±</mo><mn mathvariant="normal">1.58</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="66pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="d05d0a131b7330f12bd2049f56cff7af"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-3965-2020-ie00001.svg" width="66pt" height="10pt" src="acp-20-3965-2020-ie00001.png"/></svg:svg></span></span>&thinsp;<span class="inline-formula">µ</span>g&thinsp;m<span class="inline-formula">⁻³</span>), when the prevailing air masses were mostly of IGP origin, followed by post-monsoon (October–November) (mean <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">1.34</mn><mo>±</mo><mn mathvariant="normal">1.40</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="66pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="bb337c0054b1e0325853f2f8fe6d05bc"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-3965-2020-ie00002.svg" width="66pt" height="10pt" src="acp-20-3965-2020-ie00002.png"/></svg:svg></span></span>&thinsp;<span class="inline-formula">µ</span>g&thinsp;m<span class="inline-formula">⁻³</span>). The mass median diameter (MMD) of the BC mass size distributions was in the range 0.190–0.195&thinsp;<span class="inline-formula">µ</span>m, suggesting mixed sources of BC, and, further, higher values (<span class="inline-formula">∼</span>&thinsp;1.3–1.8) of bulk relative coating thickness (RCT) (ratio of optical and core diameters) were seen, indicating a significant fraction of highly coated BC aerosols in the IGP outflow. During the pre-monsoon (March–May), when marine/coastal air masses prevailed, BC mass concentration was lowest (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M11" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">0.82</mn><mo>±</mo><mn mathvariant="normal">0.84</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="66pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="cbe8b26a729e315fd128e192f1e7f5a1"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-20-3965-2020-ie00003.svg" width="66pt" height="10pt" src="acp-20-3965-2020-ie00003.png"/></svg:svg></span></span>&thinsp;<span class="inline-formula">µ</span>g&thinsp;m<span class="inline-formula">⁻³</span>), and larger BC cores (MMD&thinsp;<span class="inline-formula">&gt;</span>&thinsp;0.210&thinsp;<span class="inline-formula">µ</span>m) were seen, suggesting distinct source processes, while RCT was <span class="inline-formula">∼</span>&thinsp;1.2–1.3, which may translate into higher extent of absolute coating on BC cores, which may have crucial regional climate implications. During the summer monsoon (July–September), BC size distributions were dominated by smaller cores (MMD&thinsp;<span class="inline-formula">≤</span>&thinsp;0.185&thinsp;<span class="inline-formula">µ</span>m), with the lowest coating indicating fresher BC, likely from fossil fuel sources. A clear diurnal variation pattern of BC and RCT was noticed in all the seasons, and daytime peak in RCT suggested enhanced coating on BC due to the condensable coating material originating from photochemistry. Examination of submicrometre aerosol chemical composition highlighted that the IGP outflow was dominated by organics (47&thinsp;%–49&thinsp;%), and marine/coastal air masses contained higher amounts of sulfate (41&thinsp;%–47&thinsp;%), while ammonium and nitrate were seen in minor amounts, with significant concentrations only during the IGP air mass periods. The diurnal pattern of sulfate resembled that of the RCT of <span class="inline-formula"><i>r</i>_BC</span> particles, whereas organic mass showed a pattern similar to that of the <span class="inline-formula"><i>r</i>_BC</span> mass concentration. Seasonally, the coating on BC showed a negative association with the mass concentration of sulfate during the pre-monsoon season and with organics during the post-monsoon season. These are the first experimental data on the mixing state of BC from a long time series over the Indian region and include new information on black carbon in the IGP outflow region. These data help in improving the understanding of regional BC microphysical characteristics and their climate implications.</p>