Monitoring of Climatic Factors Affecting on Dust & Sand Storm in Tehran Province
Engineering, Climatic
DOI:
https://doi.org/10.55672/hij2022pp26-35Keywords:
Dust, Climatic Factors, Drought Indices, Dust and Sand Storm, Tehran ProvinceAbstract
In this study, according to the objectives and implementation method, climatic factors affecting the dust phenomenon in active meteorological stations in Tehran province for a period of 30 years were studied and analyzed. The results showed that in Mehrabad meteorological station, temperature, humidity, rainfall, evaporation factors were directly related to DSI indices, wind trend and dust storm changes, Lancaster, wind and storm diagrams, SPEI and the increase of drought indices in the statistical period increased with temperature, evaporation and decrease. Rainfall and humidity are proportional. DSI dust storm indexes were compared to 1 and Lancaster drought index was compared to 50 and SPEI index was compared positively and negatively in different years of the statistical period in the region and was classified in terms of drought and wet season. The results of monthly and annual changes in wind trend and dust storms showed that the region has no wind in all months and seasons with a speed of more than 20 meters per second. In terms of wind speed and frequency percentage, the highest wind speed was related to late May and early June, and the lowest wind speed was related to late December and early January. In addition, according to the changes in the wind trend and the documents of the winds and thunderstorms, the prevailing wind direction in the region was from the west.
Downloads
References
REFERENCES
[1] R. Poor.M, "Dust storms assessment as an environmental crisis and its impact on human health," presented at the The 1st National Conference on Environment, Energy, and Biodefense, 2010.
[2] J. M. Prospero, E. Blades, G. Mathison, and R. J. A. Naidu, "Interhemispheric transport of viable fungi and bacteria from Africa to the Caribbean with soil dust," vol. 21, no. 1, pp. 1-19, 2005.
[3] L. Natsagdorj, D. Jugder, and Y. J. A. E. Chung, "Analysis of dust storms observed in Mongolia during 1937–1999," vol. 37, no. 9-10, pp. 1401-1411, 2003.
[4] J.-T. Liu, X.-G. Jiang, X.-J. Zheng, L. Kang, and F.-Y. J. T. Qi, "An intensive Mongolian cyclone genesis induced severe dust storm," vol. 15, no. 5, pp. 1019-1033, 2004.
[5] Esmaeili.O, "Preliminary mapping of the main center's dust generation by GIS, ," Sharif University of Technology, 2005.
[6] H. Lashkari and G. Keykhosravi, "Statistical synoptic analysis of dust storm in khorasan razavi province (1993-2005)," 2008.
[7] H. K. H. J. I. Furman and B. Environment, "Dust storms in the Middle East: sources of origin and their temporal characteristics," vol. 12, no. 6, pp. 419-426, 2003.
[8] Rezaeei.M, "The effects of dust storms on human life and the environment,," presented at The Environmental Magazine, 2014.
[9] M. R. Sweeney, E. V. McDonald, and V. J. G. Etyemezian, "Quantifying dust emissions from desert landforms, eastern Mojave Desert, USA," vol. 135, no. 1-2, pp. 21-34, 2011.
[10] N. Lancaster, "13.9 Climate Change and Aeolian Processes," 2013.
[11] Y.-S. Chen, P.-C. Sheen, E.-R. Chen, Y.-K. Liu, T.-N. Wu, and C.-Y. J. E. r. Yang, "Effects of Asian dust storm events on daily mortality in Taipei, Taiwan," vol. 95, no. 2, pp. 151-155, 2004.
Published
How to Cite
Issue
Section
License
Copyright (c) 2022 Hyperscience International Journal
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.