The use of topographic scale models in predicting eolian dust erosion in hilly areas: field verification of a wind tunnel experiment
Eolian erosion of natural dust in an area of 53 ha, situated in the northern Negev Desert, is investigated both in the wind tunnel (erosion simulations on a topographic scale model) and in the field. The wind tunnel results and the field results
The spatial pattern of short-term aeolian dust deposition on and around cone-shaped hills is investigated via the simulation, in a wind tunnel, of dust storms over a topographic scale model of a conical hill in the Negev desert, Israel. The results