A007-0011
The Dynamics of an Orographically Forced Dust Storm in a Closed Basin
Abstract:
The synoptic forcing for this dust outbreak is characterized by cold frontal passage in the early morning hours, and strong westerly flow across the area of interest. The interaction of this flow with the north-south oriented Peninsular Range resulted in trapped lee waves and rotor clouds throughout the morning hours, as well as highly variable yet moderate dust concentrations in the well-mixed boundary layer. Later in the day, spillover precipitation from a cyclonic eddy embedded in the post frontal flow, and a subsequent convective downdraft in the lee of the Peninsular range initiated a shallow density current, with wind speeds greater than 15 m/s in the lower 500 m of the atmosphere. This density current propagated westward and over the desert surface, lofting dust throughout the boundary layer with the highest concentrations confined within the body of the cold jet. Following the passage of the density current, trapped lee waves and surface rotors were again apparent throughout the remainder of the day.