One of the issues that has been observed especially in recent years in the West Asian region is the simultaneous occurrence of snow or rain along with dust storm. On May 5-10, 2024, the presence of atmospheric fronts associated with low-pressure systems over the West Asia region caused heavy rainfall in some areas and dust storms in other areas at the same time. The aim of this study is to comprehensively investigate these simultaneous atmospheric events. For this purpose, a set of satellite data and products and reanalysis data were used. Since it is difficult to forecast these phenomena, the output of the WRF-Chem model was examined in order to qualitatively evaluate the dust and rain forecast in the region. On May 5, 2024, the Occluded front, associated with the low-pressure system, covered Turkey from the east to the center of the country. On this day, from the east of the Black Sea to the north of the Red Sea, cold and warm fronts followed each other. The warm front extended from the east of the Black Sea to the north of the Caspian Sea. There was a cold front in the northwest of Iran and cold and warm fronts in the north of Saudi Arabia and the border areas of this country with Iraq and Syria. Further, with the movement of low-pressure systems to the east and northeast, their fronts were also moved. During this period, on the one hand, strong winds caused by cold fronts over Iraq, Syria, Northern Saudi Arabia, Turkmenistan and southwest and center of Iran and on the other hand, the presence of thermal low-pressure systems over Saudi Arabia and the southern half of Pakistan caused dust emission in the region. The relative humidity (RH) and streamlines maps at 700hPa level show the transfer of moisture from the east of the Mediterranean Sea, the Black Sea and the Caspian Sea at higher latitudes and from the Red Sea, the Arabian Sea, the Persian Gulf, the Oman Sea and the northern Indian Ocean at lower latitudes in the presence of atmospheric fronts and ascending movements due to instability, caused rain over parts of the region. The severe gradient of RH over the region caused simultaneous occurrence of rain along with dust during this time interval. The output of the WRF-Chem model showed that this model was able to forecast the simultaneous occurrence of dust and precipitation in its 48-hour forecast. The pattern of precipitation and dust in the output of the WRF-Chem model is very similar to the satellite products.
Awad, A.M., Mashat, A.W.S., Alamoudi, A.O. and Assiri, M.E., 2016. Synoptic study of the seasonal variability of dust cases observed by the TOMS satellite over northern Saudi Arabia. Theoretical and Applied Climatology, 124, pp.1099-1117.
AlNasser, F. and Entekhabi, D., 2023, July. Tracking dust storms and identifying source areas using MSG Seviri. In IGARSS 2023-2023 IEEE International Geoscience and Remote Sensing Symposium (pp. 3905-3908). IEEE.
Bergametti, G., Rajot, J.L., Marticorena, B., Féron, A., Gaimoz, C., Chatenet, B., Coulibaly, M., Koné, I., Maman, A. and Zakou, A., 2022. Rain, wind, and dust connections in the Sahel. Journal of Geophysical Research: Atmospheres, 127(3), p.e2021JD035802.
Broomandi, P., Davletov, K., Kim, J.R. and Karaca, F., 2023. Dust Storm and Infant Health. In Dust and Health: Challenges and Solutions (pp. 113-136). Cham: Springer International Publishing.
Cao, H., Amiraslani, F., Liu, J. and Zhou, N., 2015. Identification of dust storm source areas in West Asia using multiple environmental datasets. Science of the Total Environment, 502, pp.224-235.
Cerro, J.C., Cerdà, V., Caballero, S., Bujosa, C., Alastuey, A., Querol, X. and Pey, J., 2020. Chemistry of dry and wet atmospheric deposition over the Balearic Islands, NW Mediterranean: Source apportionment and African dust areas. Science of The Total Environment, 747, p.141187.
Dayan, U., Nissen, K. and Ulbrich, U., 2015. Atmospheric conditions inducing extreme precipitation over the eastern and western Mediterranean. Natural Hazards and Earth System Sciences, 15(11), pp.2525-2544.
Dayeh, M.A., Farahat, A., Ismail-Aldayeh, H. and Abuelgasim, A., 2021. Effects of aerosols on lightning activity over the Arabian Peninsula. Atmospheric Research, 261, p.105723.
Desboeufs, K., Fu, F., Bressac, M., Tovar-Sánchez, A., Triquet, S., Doussin, J.F., Giorio, C., Chazette, P., Disnaquet, J., Feron, A. and Formenti, P., 2022. Wet deposition in the remote western and central Mediterranean as a source of trace metals to surface seawater. Atmospheric Chemistry and Physics, 22(4), pp.2309-2332.
Francis, D., Chaboureau, J.P., Nelli, N., Cuesta, J., Alshamsi, N., Temimi, M., Pauluis, O. and Xue, L., 2021. Summertime dust storms over the Arabian Peninsula and impacts on radiation, circulation, cloud development and rain. Atmospheric Research, 250, p.105364.
Goudie, A.S., 2020. Dust storms and human health. Extreme weather events and human health: International case studies, pp.13-24.
Hamzeh, N.H., Karami, S., Kaskaoutis, D.G., Tegen, I., Moradi, M. and Opp, C., 2021. Atmospheric dynamics and numerical simulations of six frontal dust storms in the Middle East region. Atmosphere, 12(1), p.125.
Karami, S., Hamzeh, N.H., Alam, K. and Ranjbar, A., 2020. The study of a rare frontal dust storm with snow and rain fall: Model results and ground measurements. Journal of Atmospheric and Solar-Terrestrial Physics, 197, p.105149.
Karami, S., Hamzeh, N.H., Kaskaoutis, D.G., Rashki, A., Alam, K. and Ranjbar, A., 2021a. Numerical simulations of dust storms originated from dried lakes in central and southwest Asia: The case of Aral Sea and Sistan Basin. Aeolian Research, 50, p.100679.
Karami, S., Kaskaoutis, D.G., Ghassabi, Z. and Khansalari, S., 2023. Investigation and model simulation of dry and moist (haboob) convective dust storms in Yazd Province, central Iranian plateau. Arabian Journal of Geosciences, 16(4), p.241.
Karami, S., Kaskaoutis, D.G., Kashani, S.S., Rahnama, M. and Rashki, A., 2021b. Evaluation of nine operational models in forecasting different types of synoptic dust events in the Middle East. Geosciences, 11(11), p.458.
Karami, S., Ranjbar, A., Mohebalhojeh, A.R. and Moradi, M., 2017. A rare case of haboob in Tehran: observational and numerical study. Atmospheric Research, 185, pp.169-185.
Kawai, K., Kai, K., Jin, Y., Sugimoto, N. and Batdorj, D., 2015. Dust event in the Gobi Desert on 22-23 May 2013: Transport of dust from the atmospheric boundary layer to the free troposphere by a cold front. Sola, 11, pp.156-159.
Knippertz, P., 2014. Meteorological aspects of dust storms. Mineral dust: A key player in the earth system, pp.121-147.
Middleton, N., Kashani, S.S., Attarchi, S., Rahnama, M. and Mosalman, S.T., 2021. Synoptic causes and socio-economic consequences of a severe dust storm in the Middle East. Atmosphere, 12(11), p.1435.
Miller, S.D., Kuciauskas, A.P., Liu, M., Ji, Q., Reid, J.S., Breed, D.W., Walker, A.L. and Mandoos, A.A., 2008. Haboob dust storms of the southern Arabian Peninsula. Journal of Geophysical Research: Atmospheres, 113(D1).
Miri, A. and Middleton, N., 2022. Long-term impacts of dust storms on transport systems in south-eastern Iran. Natural Hazards, 114(1), pp.291-312.
Rabbani, F. and Sharifikia, M., 2023. Prediction of sand and dust storms in West Asia under climate change scenario (RCPs). Theoretical and Applied Climatology, 151(1), pp.553-566.
Rostási, Á., Topa, B.A., Gresina, F., Weiszburg, T.G., Gelencsér, A. and Varga, G., 2022. Saharan dust deposition in central Europe in 2016—a representative year of the increased North African dust removal over the last decade. Frontiers in Earth Science, 10, p.869902.
Safaierad, R., Mohtadi, M., Zolitschka, B., Yokoyama, Y., Vogt, C. and Schefuß, E., 2020. Elevated dust depositions in West Asia linked to ocean–atmosphere shifts during North Atlantic cold events. Proceedings of the National Academy of Sciences, 117(31), pp.18272-18277.
Spiridonov, V., Ćurić, M., Spiridonov, V. and Ćurić, M., 2021. Air Masses and Fronts. Fundamentals of Meteorology, pp.253-261.
Wei, W., Zou, S., Duan, W., Chen, Y., Li, S. and Zhou, Y., 2023. Spatiotemporal variability in extreme precipitation and associated large-scale climate mechanisms in Central Asia from 1950 to 2019. Journal of Hydrology, 620, p.129417.
Williams, C.G. and Samara, F., 2023. Changing particle content of the modern desert dust storm: a climate× health problem. Environmental Monitoring and Assessment, 195(6), p.706.
Yao, J., Chen, Y., Chen, J., Zhao, Y., Tuoliewubieke, D., Li, J., Yang, L. and Mao, W., 2021. Intensification of extreme precipitation in arid Central Asia. Journal of Hydrology, 598, p.125760.
Yuan, T., Huang, J., Cao, J., Zhang, G. and Ma, X., 2021. Indian dust-rain storm: Possible influences of dust ice nuclei on deep convective clouds. Science of The Total Environment, 779, p.146439.
Zhao, X., Zhao, C., Yang, Y., Sun, Y., Xia, Y., Yang, X. and Fan, T., 2022. Distinct changes of cloud microphysical properties and height development by dust aerosols from a case study over Inner-Mongolia region. Atmospheric Research, 273, p.106175.
Karami,S. , Ghassabi,Z. and Moradi,M. (2024). Analysis of Systems Affecting the Simultaneous Events of Precipitation and Dust Over West Asia (May 5-10, 2024). Nivar, 48(126-127), 151-168. doi: 10.30467/nivar.2024.461752.1294
MLA
Karami,S. , , Ghassabi,Z. , and Moradi,M. . "Analysis of Systems Affecting the Simultaneous Events of Precipitation and Dust Over West Asia (May 5-10, 2024)", Nivar, 48, 126-127, 2024, 151-168. doi: 10.30467/nivar.2024.461752.1294
HARVARD
Karami S., Ghassabi Z., Moradi M. (2024). 'Analysis of Systems Affecting the Simultaneous Events of Precipitation and Dust Over West Asia (May 5-10, 2024)', Nivar, 48(126-127), pp. 151-168. doi: 10.30467/nivar.2024.461752.1294
CHICAGO
S. Karami, Z. Ghassabi and M. Moradi, "Analysis of Systems Affecting the Simultaneous Events of Precipitation and Dust Over West Asia (May 5-10, 2024)," Nivar, 48 126-127 (2024): 151-168, doi: 10.30467/nivar.2024.461752.1294
VANCOUVER
Karami S., Ghassabi Z., Moradi M. Analysis of Systems Affecting the Simultaneous Events of Precipitation and Dust Over West Asia (May 5-10, 2024). Nivar, 2024; 48(126-127): 151-168. doi: 10.30467/nivar.2024.461752.1294