Atmospheric aerosols have a wide range of impacts on the climate system. This includes interactions with the incoming solar radiation and clouds (Forkel et al., 2012), serving as a medium for transporting various organisms through vast distances (Azua-Bustos et al., 2019), and causing or enhancing respiratory, infectious, cardiovascular, and allergic diseases (Boersma et al., 2008). However, quantifying the effects of aerosols on the climate on both global and regional scales has never been a trivial problem, primarily due to their sporadic nature and large spatiotemporal variability (B. Liu et al., 2018). Hence, a considerable uncertainty of their net effect on the climate remains (Boucher et al., 2013).Atmospheric aerosols originate from different sources, namely biogenic (nature) and anthropogenic (human-related activities). Mineral dust aerosols are the dominant species in the atmosphere by virtue of their large contribution to the global aerosol loading (Tegen et al., 2002). These natural aerosols originate mostly from the Arabian, the Asian, and the Sahara deserts (Prospero, 2002). Dust mixed with biomass burning and urban pollution, frequently labeled as "polluted dust," is also an important contributor to atmospheric aerosols and is regularly observed in the Middle East, West Africa, and Central Asia (Kim et al., 2018).The cycle of atmospheric aerosols, from emission to transport and deposition, is strongly controlled by the atmospheric dynamics and thermodynamics (Kok et al., 2012). In the Arabian Gulf and surrounding region, the prevailing near-surface wind is from the northwest, locally known as Shamal winds (Bou Karam Francis et al., 2017;Yu et al., 2016). This large-scale wind interacts with local land-sea breeze circulations (Eager et al., 2008), which are stronger in the summer season when the land-sea temperature gradient is larger. As a result of the strong heating of the surface by the Sun, a thermal low develops in the region,