Mineral dust is lofted from the surface to the atmosphere by strong winds, with the most dramatic and dangerous instance of this occurring in convective dust storms, whereby visibility can be reduced to near zero in a matter of seconds (Chen & Fryrear, 2002;Leys et al., 2011;Zhang & Wang, 1997). Convective dust storms result from dust lofting in and at the outflow boundary of a convective cold pool, a specific type of atmospheric density current which forms as precipitation evaporates and ice melts below the cloud base of a mature convective cell or convective system. The air, now cooler and denser than its surroundings, is negatively buoyant and sinks until it hits the ground, spreading out as a distinct air mass. Convective downdrafts can produce intense surface winds and depending on the soil type and moisture content, they can loft loose soils into the air (