Synoptic and remote sensing analysis of dust events in southwestern Iran

• Published in: Natural hazards (Dordrecht) 2012-11, Vol.64 (2), p.1625-1638
• Main Authors: Ghasem, Azizi, Shamsipour, AliAkbar, Miri, Morteza, Safarrad, Taher
• Format: Article
• Language: English
• Subjects: Air pollution; Anthropogenic factors; Civil Engineering; Climatic conditions; Dam construction; Drought; Droughts; Drying; Dust; Dust storms; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Environmental conditions; Environmental Management; Environmental policy; Exact sciences and technology; Geophysics/Geodesy; Geotechnical Engineering & Applied Earth Sciences; Hydrogeology; Instability; Iran; Meteorology; Mountains; Natural Hazards; Natural hazards: prediction, damages, etc; Original Paper; Rainfall; Remote sensing; Satellites; Southwest; Stability; Storms; War; Weather
• ISSN: 0921-030X; 1573-0840
• DOI: 10.1007/s11069-012-0328-9

Southwest regions of Iran, due to dry environmental and climatic conditions, have been identified as one of the five major regions in the world. In recent years, large parts of Iran have been affected by suspended particles from the dust storms. The studied area is located in foothills of the Zagros Mountain Range just north of Persian Gulf in southwest of Iran. Dust and other meteorological data were prepared in 3-hour intervals from 12 synoptic weather stations. For tracking dust storms, satellite images of MODIS were used. Atmospheric conditions during the occurrence of dust storms were determined using NCEP reanalysis data. According to the statistical calculations, most storms occurred in the spring and summer. The lowest number of dust events occurred in the fall and winter particularly in December and January, when there are high possibilities of rainfall occurrence and dynamical instability conditions in the north and west of the region. The results illustrated that the highest amounts of hourly dust occurred in the afternoon and the lowest amounts occurred at 00UTC (3.30 am local times). It seems that it is closely related to the heating surface and the occurrence of local dry instabilities. Analyses of data showed that dust amounts (or volumes) in all the stations have two climactic peaks, first between 1982 and 1990 and second between 2005 and 2008 periods. These peaks can be related to a variety of factors including anthropogenic factors such as war, agricultural activities, dam construction, and widespread droughts.