In some regions, particularly the Middle East, the dust storms occur with high frequency. Since the past decade, the occurrence of dust storms has increased in this region (Kutiel & Furman, 2003: 419).Several factors are involved in the creation of the dust storms, but the main factors are circulation of the atmosphere and earth surface. Synoptic studies have shown that low and high pressure (especially dynamic), and the vertical motion of air are the main causes of dust storms in the Middle East (Omidvar, 2006; Lashkari, et.al., 2008; Mehrshahi, 2009; Tavousi, 2010). Daily mean of dust storms in Iran, especially Khuzestan in the warm season is more than other seasons, and the highest frequency has been observed in the Zabol (Raeespour, 2010; Farajzadeh, 2011). The frequency of these storms will be increased after droughts, because the ground is dry and has less vegetation (Miri, et.al., 2009). To investigate the mechanism of dust storms in Middle East, dust storm occurrence in first days of July 2009, that is the biggest storms, has been elected, in this study interaction between atmospheric circulation and earth surface properties including soil moisture, land cover and soil type has been studied by a synoptic approach.