Abstract

Abstract. Delhi, India, routinely experiences some of the world's highest urban particulate matter concentrations. We established the Delhi Aerosol Supersite study to provide long-term characterization of the ambient submicron aerosol composition in Delhi. Here we report on 1.25 years of highly time-resolved speciated submicron particulate matter (PM1) data, including black carbon (BC) and nonrefractory PM1 (NR-PM1), which we combine to develop a composition-based estimate of PM1 (“C-PM1” = BC + NR-PM1) concentrations. We observed marked seasonal and diurnal variability in the concentration and composition of PM1 owing to the interactions of sources and atmospheric processes. Winter was the most polluted period of the year, with average C-PM1 mass concentrations of ∼210 µg m−3. The monsoon was hot and rainy, consequently making it the least polluted (C-PM1 ∼50 µg m−3) period. Organics constituted more than half of the C-PM1 for all seasons and times of day. While ammonium, chloride, and nitrate each were ∼10 % of the C-PM1 for the cooler months, BC and sulfate contributed ∼5 % each. For the warmer periods, the fractional contribution of BC and sulfate to C-PM1 increased, and the chloride contribution decreased to less than 2 %. The seasonal and diurnal variation in absolute mass loadings were generally consistent with changes in ventilation coefficients, with higher concentrations for periods with unfavorable meteorology – low planetary boundary layer height and low wind speeds. However, the variation in C-PM1 composition was influenced by temporally varying sources, photochemistry, and gas–particle partitioning. During cool periods when wind was from the northwest, episodic hourly averaged chloride concentrations reached 50–100 µg m−3, ranking among the highest chloride concentrations reported anywhere in the world. We estimated the contribution of primary emissions and secondary processes to Delhi's submicron aerosol. Secondary species contributed almost 50 %–70 % of Delhi's C-PM1 mass for the winter and spring months and up to 60 %–80 % for the warmer summer and monsoon months. For the cooler months that had the highest C-PM1 concentrations, the nighttime sources were skewed towards primary sources, while the daytime C-PM1 was dominated by secondary species. Overall, these findings point to the important effects of both primary emissions and more regional atmospheric chemistry on influencing the extreme particle concentrations that impact the Delhi megacity region. Future air quality strategies considering Delhi's situation in both a regional and local context will be more effective than policies targeting only local, primary air pollutants.

Highlights

  • Outdoor air pollution has detrimental health effects (Pope and Dockery, 2006) and is responsible for more than 4 million deaths every year globally (Cohen et al, 2017), resulting in substantial global and regional decrements in life expectancy (Apte et al, 2018)

  • That most of the PM1 was composed of nonrefractory material and black carbon (BC) was consistent with past literature from Delhi which observed that metals and other nonrefractory crustal materials, which we did not measure in this study, constituted less than 5 % of PM1 (Jaiprakash et al, 2017)

  • Els, by change in the VC that varied dynamically as the planetary boundary layer height (PBLH) varied by season and time of day

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Summary

Introduction

Outdoor air pollution has detrimental health effects (Pope and Dockery, 2006) and is responsible for more than 4 million deaths every year globally (Cohen et al, 2017), resulting in substantial global and regional decrements in life expectancy (Apte et al, 2018). S. Gani et al.: Submicron aerosol composition in the world’s most polluted megacity from ambient air pollution among all countries in the world (∼ 1.1 million people yr−1, ∼ 1.5 years of life lost due to air pollution) (Cohen et al, 2017; Apte et al, 2018). Delhi (population = 28 million) is the world’s most polluted megacity, with recent annual-average PM2.5 concentrations of ∼ 140 μg m−3 (World Health Organization, 2018)

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