Mathematical Modeling of Formation of Transparency Regions in Supercooled Stratiform Clouds and Fogs
Abstract
We developed models of active influence on clouds using crystallization reagents to ensure transparency of the atmosphere. Numerical modeling of various versions of influence on stratiform clouds at aviation seeding was performed. Variation of characteristics of supercooled fogs when bringing man-made crystals was studied. The determination of reagents application rates, estimating impact effect and some other issues were solved using the results of modelling of clouds evolution (both natural and under active influence). Based on generalization of the results of numerical simulation of cloud evolution, the proposals for improvement of cloud seeding technology under different weather conditions are developed.
References
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*** Methodical instructions for conducting work on the artificial regulation of precipitation from convective clouds by means of aircraft. 1988. Available at: http://www.gostrf.com/normadata/1/4293848/4293848975.htm
(accessed: 15.12.2017)
*** Methodological instructions. 1999. Planning and carrying out of works on artificial increase of atmospheric precipitation by aircraft methods. Moscow: CAO. (in Russian)
[2] Bakhanov, V.P., Kolezhuk, V.G. 1980. Numerical simulation of the formation of the clear zone in the fog under the influence of a hygroscopic reagent using the airplane method. Proceedings of Ukr.NIIGI, 178: 26-40.
[3] Bakhanov, V.P., Kolezhuk, V.T., Manzhara, A.A. 1990. Numerical simulation of the effect on mixed and crystalline stratiform clouds for the purpose of controlling precipitation. Proceedings ofUkrNIGMI, 237: 13-36.
[4] Bekryaev, V.I. 1991. Workshop on the physical basis of the impact on atmospheric processes. Saint Petersburg: Gidrometeoizdat. (in Russian)
[5] Beryulev, G.P., Danelyan, B.G., Nevzorov, A.N. 1996. On measurements of crystal spectra in the bands of artificial influences on stratiform clouds. Trudy CAO, 162: 42-48.
[6] Chernikov, A.A., Bankova, N.Yu., Krasnovskaya, L.I., Khizhnyak, A.N., Sergeev, B.N. et al. 1999. Using Russian supercooled fog dispersal technology at the beginning of northern Italy, 7th WMO Sci. Conf. on Weath. Mod, in Thailand.
[7] Denis, A. 1983. Change in the weather by the seeding of clouds. Moscow: Mir. (in Russian)
[8] Hindman, E.E., Johnson, D.B. 1972. Numerical simulation of ice particle growth in a cloud of supercooled water droplets. J.Atm.Sci, 29(7): 1313-1321.
[9] Kachurin, L.G. 1990. Physical bases of influence on atmospheric processes. Saint Petersburg: Gidrometeoizdat. (in Russian)
[10] Khvorostyanov, V.I. 1986. Modeling and schemes of the clearance zones in terrestrial scattering of supercooled fogs. Meteorology and Hydrology, 3: 30-37.
[11] Khvorostyanov, V.I. 1988. Modeling of artificial crystallization and scattering of supercooled fogs and low clouds. Materials of the All-Union Seminar “Numerical modeling of layered clouds and artificial impact on them”, Moscow: Gidrometeoizdat.
[12] Kogan, E.L., Mazin, I.P., Sergeev, B.N., Khvorostyanov, V.I. 1984. Numerical modeling of clouds. Moscow: Gidrometeoizdat. (in Russian)
[13] Krasnogorskaya, N.V. 1965. The effect of electrical forces on the coagulation of particles of comparable dimensions. IAN USSR, FAO, 1: 339-345.
[14] Krasnovskaya, L.I., Seregin, Yu.A., Khvorostyanov, V.I. 1987. The current state of research on the artificial effect on supercooled clouds and fogs with the use of ice-forming reagent, Problems of the Physics of clouds. Saint Petersburg: Gidrometeoizdat.
[15] Mazin, I.P., Shmeeter, S.M. 1983. Clouds. The structure and physics of education, Saint Petersburg: Gidrometeoizdat. (in Russian)
[16] Pirnach, A.M. 1990. Numerical simulation of the evolution of clouds and precipitation bands on cold fronts under different conditions of temperature and pressure fields, Tr. UkrNIIGMI, 237: 117-138.
[17] Polovina, I.P. 1980. Scattering of supercooled stratiform clouds and fogs. Saint Petersburg: Gidrometeoizdat.
[18] Stefanov, S., Calovski, C. 2003. Experiments of supercooled fog dispersal in urban areas, 8th WMO Sci. Conf. on Weather Modif, in Marocco.
*** Methodical instructions for conducting work on the artificial regulation of precipitation from convective clouds by means of aircraft. 1988. Available at: http://www.gostrf.com/normadata/1/4293848/4293848975.htm
(accessed: 15.12.2017)
*** Methodological instructions. 1999. Planning and carrying out of works on artificial increase of atmospheric precipitation by aircraft methods. Moscow: CAO. (in Russian)
Published
2018-06-19
How to Cite
SHAPOVALOV, Vitaly A. et al.
Mathematical Modeling of Formation of Transparency Regions in Supercooled Stratiform Clouds and Fogs.
Journal of Environmental Management and Tourism, [S.l.], v. 9, n. 1, p. 17-27, june 2018.
ISSN 2068-7729.
Available at: <https://journals.aserspublishing.eu/jemt/article/view/2051>. Date accessed: 25 apr. 2024.
doi: https://doi.org/10.14505//jemt.v9.1(25).03.
Section
Article
Copyright© 2023 The Author(s). Published by ASERS Publishing 2023. This is an open access article distributed under the terms of CC-BY 4.0 license.