Standard

On the consideration of the averaged vertical wind in problems of stratospheric aerosol transport. / Gryazin, V. I.; Beresnev, S. A.
в: Atmospheric and Oceanic Optics, Том 23, № 3, 2010, стр. 174-180.

Результаты исследований: Вклад в журнал › Статья › Рецензирование

Harvard

Gryazin, VI & Beresnev, SA 2010, 'On the consideration of the averaged vertical wind in problems of stratospheric aerosol transport', Atmospheric and Oceanic Optics, Том. 23, № 3, стр. 174-180. https://doi.org/10.1134/S1024856010030036

APA

Gryazin, V. I., & Beresnev, S. A. (2010). On the consideration of the averaged vertical wind in problems of stratospheric aerosol transport. Atmospheric and Oceanic Optics, 23(3), 174-180. https://doi.org/10.1134/S1024856010030036

Vancouver

Gryazin VI, Beresnev SA. On the consideration of the averaged vertical wind in problems of stratospheric aerosol transport. Atmospheric and Oceanic Optics. 2010;23(3):174-180. doi: 10.1134/S1024856010030036

Author

Gryazin, V. I. ; Beresnev, S. A. / On the consideration of the averaged vertical wind in problems of stratospheric aerosol transport. в: Atmospheric and Oceanic Optics. 2010 ; Том 23, № 3. стр. 174-180.

BibTeX

@article{11ab53ab8d784b3ebaf6d88f4309e6df,
title = "On the consideration of the averaged vertical wind in problems of stratospheric aerosol transport",
abstract = "The influence of the averaged vertical wind on the transport of stratospheric aerosol has been analyzed with the use of the database of the GCM UKMO assimilated model for 1993–2006. With the problem regarding the action of a permanent source of particles near the stratopause taken as an example, it is shown that if the action of the averaged vertical component is taken into account along with the gravitational sedimentation and turbulent diffusion, the standard vertical profiles of the relative concentration of particles change cardinally. The results are presented for the levitation heights of particles of different densities and sizes in the stratosphere under the action of gravity and wind pressure. {\textcopyright} 2010, Pleiades Publishing, Ltd.",
author = "Gryazin, {V. I.} and Beresnev, {S. A.}",
note = "This work was supported in part by the Russian Foundation for Basic Research (project no. 09 01 00649) and the Ministry of Education and Science of the Russian Federation (Program “Development of the Scientific Potential of the Higher School (2009– 2010),” registration number 2.1.1/6019).",
year = "2010",
doi = "10.1134/S1024856010030036",
language = "English",
volume = "23",
pages = "174--180",
journal = "Atmospheric and Oceanic Optics",
issn = "1024-8560",
publisher = "Pleiades Publishing",
number = "3",

}

RIS

TY - JOUR

T1 - On the consideration of the averaged vertical wind in problems of stratospheric aerosol transport

AU - Gryazin, V. I.

AU - Beresnev, S. A.

N1 - This work was supported in part by the Russian Foundation for Basic Research (project no. 09 01 00649) and the Ministry of Education and Science of the Russian Federation (Program “Development of the Scientific Potential of the Higher School (2009– 2010),” registration number 2.1.1/6019).

PY - 2010

Y1 - 2010

N2 - The influence of the averaged vertical wind on the transport of stratospheric aerosol has been analyzed with the use of the database of the GCM UKMO assimilated model for 1993–2006. With the problem regarding the action of a permanent source of particles near the stratopause taken as an example, it is shown that if the action of the averaged vertical component is taken into account along with the gravitational sedimentation and turbulent diffusion, the standard vertical profiles of the relative concentration of particles change cardinally. The results are presented for the levitation heights of particles of different densities and sizes in the stratosphere under the action of gravity and wind pressure. © 2010, Pleiades Publishing, Ltd.

AB - The influence of the averaged vertical wind on the transport of stratospheric aerosol has been analyzed with the use of the database of the GCM UKMO assimilated model for 1993–2006. With the problem regarding the action of a permanent source of particles near the stratopause taken as an example, it is shown that if the action of the averaged vertical component is taken into account along with the gravitational sedimentation and turbulent diffusion, the standard vertical profiles of the relative concentration of particles change cardinally. The results are presented for the levitation heights of particles of different densities and sizes in the stratosphere under the action of gravity and wind pressure. © 2010, Pleiades Publishing, Ltd.

UR - http://www.scopus.com/inward/record.url?partnerID=8YFLogxK&scp=84950277776

U2 - 10.1134/S1024856010030036

DO - 10.1134/S1024856010030036

M3 - Article

VL - 23

SP - 174

EP - 180

JO - Atmospheric and Oceanic Optics

JF - Atmospheric and Oceanic Optics

SN - 1024-8560

IS - 3

ER -

ID: 37956431