Sandstorms share fluid dynamic properties with atmospheric gravity currents and density currents
Sandstorms and dust fronts are well-documented in meteorological and fluid dynamic literature to share properties with atmospheric gravity currents and density currents.
The retrieved literature includes papers directly linking sand and dust storm dynamics to density currents and atmospheric gravity features.
D. Kaskaoutis, D. Francis, A. Rashki, J. Chaboureau, U. C. Dumka. Atmospheric Dynamics from Synoptic to Local Scale During an Intense Frontal Dust Storm over the Sistan Basin in Winter 2019. 2019. https://doi.org/10.3390/geosciences9100453
Paper [2] discusses how dust storms and their atmospheric dynamics involve surface density currents emanating from convective clouds that cause soil erosion.
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M. Hilton, D. R. Borrie, T. Konlechner, S. Wakes, T. Lane, P. Kench, D. Kennedy, M. Aslam. A first evaluation of the contribution of aeolian sand transport to lagoon island accretion in the Maldives. 2019. https://doi.org/10.1016/J.AEOLIA.2019.04.006
Paper [6] notes that high rates of sand transport and dust movement can be forced or generated by surface-based density currents.
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