Standard

Numerical simulation of convective clouds developing in the atmosphere in emergency situations (explosions, fires). / Veremei, N. E.; Dovgalyuk, Yu A.; Stankova, E. N.

в: Izvestiya - Atmospheric and Ocean Physics, Том 43, № 6, 01.12.2007, стр. 731-744.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Veremei, NE, Dovgalyuk, YA & Stankova, EN 2007, 'Numerical simulation of convective clouds developing in the atmosphere in emergency situations (explosions, fires)', Izvestiya - Atmospheric and Ocean Physics, Том. 43, № 6, стр. 731-744. https://doi.org/10.1134/S0001433807060072

APA

Veremei, N. E., Dovgalyuk, Y. A., & Stankova, E. N. (2007). Numerical simulation of convective clouds developing in the atmosphere in emergency situations (explosions, fires). Izvestiya - Atmospheric and Ocean Physics, 43(6), 731-744. https://doi.org/10.1134/S0001433807060072

Vancouver

Veremei NE, Dovgalyuk YA, Stankova EN. Numerical simulation of convective clouds developing in the atmosphere in emergency situations (explosions, fires). Izvestiya - Atmospheric and Ocean Physics. 2007 Дек. 1;43(6):731-744. https://doi.org/10.1134/S0001433807060072

Author

Veremei, N. E. ; Dovgalyuk, Yu A. ; Stankova, E. N. / Numerical simulation of convective clouds developing in the atmosphere in emergency situations (explosions, fires). в: Izvestiya - Atmospheric and Ocean Physics. 2007 ; Том 43, № 6. стр. 731-744.

BibTeX

@article{8683f51258da44f284be9daec28905c8,
title = "Numerical simulation of convective clouds developing in the atmosphere in emergency situations (explosions, fires)",
abstract = "A numerical model is presented that allows an adequate description of the evolution of a liquiddroplet convective cloud developing under extreme conditions in the presence of high-power thermal sources on the land surface or in the atmosphere. The features of the life cycle and stages of clouds are studied on the basis of this model in relation to the distribution of environmental humidity and the time of action of a thermal source and its temperature and radius. It is shown that, owing to the action of an instantaneous energy source (an explosion), a convection flow develops in the form of a thermal, whereas a convection flow in the form of a jet develops above a long-acting energy source (fire). The features of the evolution and formation of precipitation in the clouds formed under the development of both convection forms are studied in detail.",
author = "Veremei, {N. E.} and Dovgalyuk, {Yu A.} and Stankova, {E. N.}",
year = "2007",
month = dec,
day = "1",
doi = "10.1134/S0001433807060072",
language = "English",
volume = "43",
pages = "731--744",
journal = "Izvestiya - Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Numerical simulation of convective clouds developing in the atmosphere in emergency situations (explosions, fires)

AU - Veremei, N. E.

AU - Dovgalyuk, Yu A.

AU - Stankova, E. N.

PY - 2007/12/1

Y1 - 2007/12/1

N2 - A numerical model is presented that allows an adequate description of the evolution of a liquiddroplet convective cloud developing under extreme conditions in the presence of high-power thermal sources on the land surface or in the atmosphere. The features of the life cycle and stages of clouds are studied on the basis of this model in relation to the distribution of environmental humidity and the time of action of a thermal source and its temperature and radius. It is shown that, owing to the action of an instantaneous energy source (an explosion), a convection flow develops in the form of a thermal, whereas a convection flow in the form of a jet develops above a long-acting energy source (fire). The features of the evolution and formation of precipitation in the clouds formed under the development of both convection forms are studied in detail.

AB - A numerical model is presented that allows an adequate description of the evolution of a liquiddroplet convective cloud developing under extreme conditions in the presence of high-power thermal sources on the land surface or in the atmosphere. The features of the life cycle and stages of clouds are studied on the basis of this model in relation to the distribution of environmental humidity and the time of action of a thermal source and its temperature and radius. It is shown that, owing to the action of an instantaneous energy source (an explosion), a convection flow develops in the form of a thermal, whereas a convection flow in the form of a jet develops above a long-acting energy source (fire). The features of the evolution and formation of precipitation in the clouds formed under the development of both convection forms are studied in detail.

UR - http://www.scopus.com/inward/record.url?scp=37749025087&partnerID=8YFLogxK

U2 - 10.1134/S0001433807060072

DO - 10.1134/S0001433807060072

M3 - Article

AN - SCOPUS:37749025087

VL - 43

SP - 731

EP - 744

JO - Izvestiya - Atmospheric and Oceanic Physics

JF - Izvestiya - Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 6

ER -

ID: 43545652