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Determining the source of dust storms with use of coupling WRF and HYSPLIT models: A case study of Yazd province in central desert of Iran
Institution:1. Department of Physics, Yazd University, Yazd, Iran;2. Department of Geography, Yazd University, Yazd, Iran;1. Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environmental Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, 210044, China;2. Joint Innovation Center for Modern Forestry Studies, College of Biology and Environment, Nanjing Forestry University, Nanjing, 210037, China;3. Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York, Albany, NY, 12222, USA;1. CNR – Institute of Atmospheric Sciences and Climate, Via Gobetti 101, 40129 Bologna, Italy;2. Univ. Grenoble Alpes, CNRS, LGGE, F-38041 Grenoble, France;3. Ev-K2-CNR, Via San Bernardino 145, 24126 Bergamo, Italy;1. Amirkabir University of Technology, Department of Energy Engineering and Physics, Tehran, Iran;2. Shahid Beheshti University, Radiation Application Department, Tehran, Iran;3. Iran Radioactive Waste Management Co. (IRWA), Atomic Energy Organization of Iran (AEOI), Tehran, Iran;1. National Pollen and Aerobiology Research Unit, University of Worcester, Henwick Grove, Worcester, Worcestershire, WR2 6AJ, UK;2. University of Worcester and Rothamsted Research, UK
Abstract:Dust storm, which has a significant impact on regional air quality, is one of the most hazardous meteorological phenomena in the arid areas. Yazd province is one of the arid areas in Iran that is exposed to dust storms. In this study, two cases of dust storms of Yazd province are studied with the use of coupling numerical models and aerosol optical depth (AOD) from MODIS data. We investigated synoptic condition of such dust storms that were formed downstream of upper level through in the area by focusing on two storms, on May 24 and 25, 2014. For this purpose, a dynamic coupling of this case is done using WRF output the HYSPLIT model. This model was implemented to investigate the sources of the dust storms by calculating the back trajectories from the receptor sites. The trajectories indicated that the first and the second case storms occurred in the northeast and the south of Yazd respectively. These results also showed a good agreement with MODIS aerosol optical depth data and HYSPLIT back trajectories paths.
Keywords:Dust storm  Yazd  WRF  HYSPLIT  Source  MODIS
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