Dust is the dominant aerosol species by mass in the Earth's atmosphere, and emissions from the deserts and arid regions across the globe range between 1,000 and 4,000 Tg yr −1 annually (e.g., Huneeus et al., 2011; Urban et al., 2018). Dust aerosols play an important role in the Earth's climate dynamics (e.g., Kok et al., 2018; Sokolik et al., 2001), affecting the Earth's radiative balance, and also rainfall (Shepherd et al., 2016). Dust also enriches oceanic biological productivity by supplying micronutrients, which in turn helps the oceans to act as carbon sinks by reducing atmospheric carbon dioxide concentrations (e.g.,