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Transport of stratospheric aerosols in the field of averaged vertical wind: book chapter. / Gryazin, V. I.; Beresnev, S. A.
AAAS08: 2ND ADVANCED ATMOSPHERIC AEROSOL SYMPOSIUM: book. ed. / E. Ranzi. Vol. 16 MILANO: AIDIC-Italian Association of Chemical Engineering, 2008. p. 329-335 (Chemical Engineering Transactions).

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

Harvard

Gryazin, VI & Beresnev, SA 2008, Transport of stratospheric aerosols in the field of averaged vertical wind: book chapter. in E Ranzi (ed.), AAAS08: 2ND ADVANCED ATMOSPHERIC AEROSOL SYMPOSIUM: book. vol. 16, Chemical Engineering Transactions, AIDIC-Italian Association of Chemical Engineering, MILANO, pp. 329-335.

APA

Gryazin, V. I., & Beresnev, S. A. (2008). Transport of stratospheric aerosols in the field of averaged vertical wind: book chapter. In E. Ranzi (Ed.), AAAS08: 2ND ADVANCED ATMOSPHERIC AEROSOL SYMPOSIUM: book (Vol. 16, pp. 329-335). (Chemical Engineering Transactions). AIDIC-Italian Association of Chemical Engineering.

Vancouver

Gryazin VI, Beresnev SA. Transport of stratospheric aerosols in the field of averaged vertical wind: book chapter. In Ranzi E, editor, AAAS08: 2ND ADVANCED ATMOSPHERIC AEROSOL SYMPOSIUM: book. Vol. 16. MILANO: AIDIC-Italian Association of Chemical Engineering. 2008. p. 329-335. (Chemical Engineering Transactions).

Author

Gryazin, V. I. ; Beresnev, S. A. / Transport of stratospheric aerosols in the field of averaged vertical wind : book chapter. AAAS08: 2ND ADVANCED ATMOSPHERIC AEROSOL SYMPOSIUM: book. editor / E. Ranzi. Vol. 16 MILANO : AIDIC-Italian Association of Chemical Engineering, 2008. pp. 329-335 (Chemical Engineering Transactions).

BibTeX

@inproceedings{dc9d3adf7c8d4373b5466fb33b5453e9,
title = "Transport of stratospheric aerosols in the field of averaged vertical wind: book chapter",
abstract = "The latitudinal and seasonal dependences of vertical profiles of the averaged vertical wind for different time intervals from 1992 to 2006 based on the data of the UKMO atmosphere general circulation model are analyzed. It is shown that monthly average amplitudes of the vertical wind are approximately +/- 5 mm/s, while annual average ones are +/- 1 mm/s. The upward wind can provide the vertical lifting against gravity for sufficiently large (up to 3-5 mu m) aerosol particles with a density up to 1.0-1.5 g/cm(3) at stratospheric and mesospheric altitudes. The vertical wind probably is a substantial factor of particle motion up to altitudes of 30-40 km and can change essentially the sedimentation rate and the residence time of stratospheric aerosols. The structure of the averaged fields of vertical wind supposes the opportunity of formation of dynamically stable aerosol layers in the middle stratosphere.",
author = "Gryazin, {V. I.} and Beresnev, {S. A.}",
year = "2008",
language = "English",
isbn = "978-88-95608-03-7",
volume = "16",
series = "Chemical Engineering Transactions",
publisher = "AIDIC-Italian Association of Chemical Engineering",
pages = "329--335",
editor = "E. Ranzi",
booktitle = "AAAS08: 2ND ADVANCED ATMOSPHERIC AEROSOL SYMPOSIUM",
address = "Italy",

}

RIS

TY - GEN

T1 - Transport of stratospheric aerosols in the field of averaged vertical wind

T2 - book chapter

AU - Gryazin, V. I.

AU - Beresnev, S. A.

PY - 2008

Y1 - 2008

N2 - The latitudinal and seasonal dependences of vertical profiles of the averaged vertical wind for different time intervals from 1992 to 2006 based on the data of the UKMO atmosphere general circulation model are analyzed. It is shown that monthly average amplitudes of the vertical wind are approximately +/- 5 mm/s, while annual average ones are +/- 1 mm/s. The upward wind can provide the vertical lifting against gravity for sufficiently large (up to 3-5 mu m) aerosol particles with a density up to 1.0-1.5 g/cm(3) at stratospheric and mesospheric altitudes. The vertical wind probably is a substantial factor of particle motion up to altitudes of 30-40 km and can change essentially the sedimentation rate and the residence time of stratospheric aerosols. The structure of the averaged fields of vertical wind supposes the opportunity of formation of dynamically stable aerosol layers in the middle stratosphere.

AB - The latitudinal and seasonal dependences of vertical profiles of the averaged vertical wind for different time intervals from 1992 to 2006 based on the data of the UKMO atmosphere general circulation model are analyzed. It is shown that monthly average amplitudes of the vertical wind are approximately +/- 5 mm/s, while annual average ones are +/- 1 mm/s. The upward wind can provide the vertical lifting against gravity for sufficiently large (up to 3-5 mu m) aerosol particles with a density up to 1.0-1.5 g/cm(3) at stratospheric and mesospheric altitudes. The vertical wind probably is a substantial factor of particle motion up to altitudes of 30-40 km and can change essentially the sedimentation rate and the residence time of stratospheric aerosols. The structure of the averaged fields of vertical wind supposes the opportunity of formation of dynamically stable aerosol layers in the middle stratosphere.

UR - https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=tsmetrics&SrcApp=tsm_test&DestApp=WOS_CPL&DestLinkType=FullRecord&KeyUT=000270892200043

M3 - Conference contribution

SN - 978-88-95608-03-7

VL - 16

T3 - Chemical Engineering Transactions

SP - 329

EP - 335

BT - AAAS08: 2ND ADVANCED ATMOSPHERIC AEROSOL SYMPOSIUM

A2 - Ranzi, E.

PB - AIDIC-Italian Association of Chemical Engineering

CY - MILANO

ER -

ID: 38655027