Sulfur Dioxide Point Sources Remain Important for Daytime Plume-Scale New Particle Formation in the United States: Case Study for Gary, Indiana During the Summer 2023 AEROMMA Aircraft Campaign

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
En Li, Samuel E. O’Donnell, Adam T. Ahern, Kelvin H. Bates, Charles A. Brock, Wyndom S. Chace, Matthew M. Coggon, Emily V. Fischer, Jessica B. Gilman, Georgios I. Gkatzelis, Han N. Huynh, Emily R. Lill, Ming Lyu, Ann M. Middlebrook, Alison M. Piasecki, Jeff Peischl, Ilana B. Pollack, Andrew W. Rollins, Nell B. Schafer, Chelsea E. Stockwell, Victoria Treadaway, Carsten Warneke, Eleanor M. Waxman, Lu Xu, Kristen Zuraski, Robin G. Stevens, Shantanu H. Jathar, Jeffrey R. Pierce
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Abstract

Plumes from sulfur dioxide (SO2) point sources have been shown to be significant contributors to new particle formation (NPF), but SO2 emissions in the United States (US) have decreased drastically by ∼10× since the early 2000s. We present observations of plume-scale NPF from SO2 point sources over the industrial hub in Gary, Indiana and assess the importance of SO2 plumes to NPF using the P6 subgrid NPF parameterization and model the subsequent aerosol growth using the Statistical Oxidation Model-TwO Moment Aerosol Sectional (SOM-TOMAS) kinetic gas/aerosol model. We identify 29 SO2-rich NPF plumes downwind of SO2 point sources in our observations. Across eight separate flight passes over Gary, the total plume-scale particle production rate via NPF is estimated to be in the range of 8.5 × 1013–3.5 × 1018 # s−1 and is typically comparable to or greater than primary particle number emissions from traffic in nearby Chicago. On a single case day, subsequent growth of newly formed particles is mainly driven by regional condensation of organics and coagulation. These results demonstrate the continued importance of SO2 point sources for plume-scale NPF and regional aerosol number concentrations, including those of climate-relevant sizes (<50–100 nm diameter), despite more than a factor-of-10 reduction in SO2 emissions in recent decades. Further, organics are critical in sustaining the growth of these newly formed particles, and organics may be more important for this growth compared to past decades due to reduced sulfuric acid (H2SO4).

二氧化硫点源对美国白天羽状尺度新颗粒形成仍然很重要:2023年夏季AEROMMA飞机运动期间印第安纳州加里的案例研究
来自二氧化硫(SO2)点源的羽流已被证明是新粒子形成(NPF)的重要贡献者,但自21世纪初以来,美国的SO2排放量急剧减少了约10倍。我们提供了来自印第安纳州Gary工业中心的SO2点源的羽状尺度NPF的观测结果,并使用P6子网格NPF参数化评估了SO2羽状对NPF的重要性,并使用统计氧化模型-二时刻气溶胶截面(SOM-TOMAS)动力学气体/气溶胶模型模拟了随后的气溶胶增长。在我们的观测中,我们确定了29个富含SO2的NPF羽流在SO2点源的下风。在加里上空的8个独立飞行通道中,通过NPF产生的总羽状尺度颗粒产生率估计在8.5 × 1013-3.5 × 1018 # s−1的范围内,通常与附近芝加哥交通产生的主要颗粒数量相当或更大。在单一情况下,新形成的颗粒的后续生长主要是由有机物的区域凝结和混凝驱动的。这些结果表明,尽管近几十年来SO2排放量减少了10倍以上,但SO2点源对羽状尺度NPF和区域气溶胶数量浓度(包括与气候相关的尺寸(<; 50-100 nm直径))仍然具有重要意义。此外,有机物对维持这些新形成的颗粒的生长至关重要,与过去几十年相比,由于硫酸(H2SO4)的减少,有机物对这种生长可能更重要。
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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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