Aerosols have far-reaching impacts including adverse health effects, reduction in visibility, modification of clouds, and alteration of the Earth's climate. Aerosols affect climate by absorbing or scattering solar radiation, regulating condensation and evaporation of atmospheric trace gases including water, and affecting cloud properties by serving as cloud condensation nuclei (CCN). The substantial role of aerosols in the hydrological cycle is a significant source of uncertainty in climate projections (Forster et al., 2021).Nucleation and growth of new particles is the major contributor to both particle number and CCN-active particles in the atmosphere (H. Gordon et al., 2017;Kulmala et al., 2004;Pierce et al., 2011). The role of organic molecules in the nucleation mechanism is not precisely known . Nucleation occurs when a nascent molecular cluster achieves a diameter exceeding ∼0.7-1.7 nm and condensation of additional molecules becomes energetically favorable (Sipilä et al., 2010). New particle formation has been observed in various environments and occurs through different chemical pathways (Kerminen et al., 2018;Kulmala et al., 2004). Although nucleation is driven by the condensation of low-volatility inorganic species such as sulfuric acid, amines, iodic acid, and nitric acid (