Anthropogenic Emissions in Coastal India Strongly Influence New Particle Formation and Cloud Condensation Nuclei Activity

Aishwarya Singh, Basudev Swain, Mathew Sebastian, S. N. Tripathi, Mira Pöhlker, James Allan, Gordon McFiggans, Ulrich Pöschl, Hang Su, Scot T. Martin, Meinrat O. Andreae, R. Ravikrishna, Yafang Cheng, Hugh Coe, Pengfei Liu* and Sachin S. Gunthe*, 
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Abstract

Aerosols influence Earth’s energy balance and hydrological cycle as cloud condensation nuclei (CCN), yet uncertainties persist in how anthropogenic emissions alter their abundance and climate-relevant properties. Abrupt, large-scale reductions in human activities provided a natural experiment to quantify anthropogenic impact on aerosol-cloud-climate interactions in coastal India. Combining chemical and microphysical measurements under drastically reduced and subsequently reintroduced emission scenarios, we reveal that CCN concentrations increased by 80–250% postlockdown. This surge coincided with increased new particle formation (NPF) event frequency and enhanced particle growth rates. Postlockdown air masses shifted from marine to continental sources, revealing that anthropogenic organic matter (OM), despite lower hygroscopicity, dominated particle growth to CCN-active sizes, offsetting hygroscopicity limitations. These findings demonstrate how shifts in anthropogenic activity can strongly impact aerosol–cloud interaction potential, even under varying air mass influences, and provide a reference for understanding the atmospheric effects of future air quality interventions.

Organic-rich aerosols in coastal India show strong sensitivity to changes in anthropogenic emissions and wind patterns, enhancing new particle formation and cloud-forming potential, highlighting implications for air quality interventions.

印度沿海人为排放强烈影响新粒子形成和云凝结核活动
气溶胶作为云凝结核(CCN)影响地球的能量平衡和水文循环,但在人为排放如何改变其丰度和与气候相关的特性方面仍然存在不确定性。人类活动的突然大规模减少为量化人为对印度沿海气溶胶-云-气候相互作用的影响提供了一个自然实验。结合化学和微物理测量,在大幅减少和随后重新引入排放的情况下,我们发现CCN浓度在封锁后增加了80-250%。这种激增与增加的新粒子形成(NPF)事件频率和增强的粒子生长速率一致。封湖后气团从海洋气团转移到大陆气团,这表明尽管吸湿性较低,但人为有机质(OM)主导了颗粒生长到ccn活性大小,抵消了吸湿性的限制。这些发现表明,即使在不同气团的影响下,人为活动的变化如何强烈影响气溶胶-云相互作用的潜力,并为了解未来空气质量干预措施的大气影响提供参考。印度沿海地区富含有机物的气溶胶对人为排放和风型的变化表现出强烈的敏感性,增强了新粒子的形成和云形成的潜力,突出了对空气质量干预的影响。
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