Introduction: In recent years, Desert Dust frequency has increased in the Global system. Due to lack of vegetation in the regions prone to dust, the earth’s surface air becomes warm enough in these regions, moves upward and causes a cold downward circular air flow when it collides with upper tropospheric winds. When these winds strongly hit the earth’s surface, they create dust storms (Xuan et al, 2004). Many studies from all around the world have been conducted on the source regions of this environmental phenomenon (Kai & Gao, 2007). The studies on Asian dust storms with sea sources during 2000-2002 showed 64% of storms originate from China seas and become more severe from west to east and carry dust on the land. Wang, Stein, Draxler, Rosa & Zhang (2011) studied sand and dust storms in 2008 and defined North Africa, Middle East, Mongolia, and north-west China with high frequency of dust phenomenon, using HYSPLIT Model. Shamsipour and Safar-Rad (2012), analyzed the July 2009 dust in the west of Iran. In the chosen sample, the Zagros hillsides contain the highest amount of pollutants. Also, the results indicate that the location of Naveh, upper-level divergence of 500 and forming a thermal low-pressure system on earth’s surface play the main role in flowing the dust toward Iran...