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A new dust observation site was built in Tsogt-Ovoo, which is located in the northern Gobi Desert in Mongolia, to clarify wind erosion processes. Ten dust events were detected from March 24 to May 4, 2012. Strong winds (greater than 20 m s −1 at an altitude of 3 m) blew predominantly from the west. Clear relationships among wind speed, saltation and particulate matter concentrations less than 10 μm (PM 10 ) were detected. A transition in the wind speed threshold for saltation was observed atdoi:10.2151/sola.2012-032 fatcat:ah6lmtkiefe75desrvp7dgyopa