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Numerical modeling of inhomogeneous orographic wave influence on planetary waves in the middle atmosphere. / Gavrilov, Nikolai M.; Koval, Andrey V.; Pogoreltsev, Alexander I.; Savenkova, Elena N.

In: Advances in Space Research, Vol. 51, No. 11, 2013, p. 2145-2154.

Research output: Contribution to journal › Article › peer-review

Harvard

Gavrilov, NM, Koval, AV, Pogoreltsev, AI & Savenkova, EN 2013, 'Numerical modeling of inhomogeneous orographic wave influence on planetary waves in the middle atmosphere', Advances in Space Research, vol. 51, no. 11, pp. 2145-2154. https://doi.org/doi 10.1016/j.asr.2012.12.024, https://doi.org/10.1016/j.asr.2012.12.024

APA

Gavrilov, N. M., Koval, A. V., Pogoreltsev, A. I., & Savenkova, E. N. (2013). Numerical modeling of inhomogeneous orographic wave influence on planetary waves in the middle atmosphere. Advances in Space Research, 51(11), 2145-2154. https://doi.org/doi 10.1016/j.asr.2012.12.024, https://doi.org/10.1016/j.asr.2012.12.024

Vancouver

Gavrilov NM, Koval AV, Pogoreltsev AI, Savenkova EN. Numerical modeling of inhomogeneous orographic wave influence on planetary waves in the middle atmosphere. Advances in Space Research. 2013;51(11):2145-2154. https://doi.org/doi 10.1016/j.asr.2012.12.024, https://doi.org/10.1016/j.asr.2012.12.024

Author

Gavrilov, Nikolai M. ; Koval, Andrey V. ; Pogoreltsev, Alexander I. ; Savenkova, Elena N. / Numerical modeling of inhomogeneous orographic wave influence on planetary waves in the middle atmosphere. In: Advances in Space Research. 2013 ; Vol. 51, No. 11. pp. 2145-2154.

BibTeX

@article{fa2f1177c1ef4b2087217ed1d2240d59,
title = "Numerical modeling of inhomogeneous orographic wave influence on planetary waves in the middle atmosphere",
abstract = "Parameterization of dynamical and thermal effects of stationary orographic gravity waves (OGWs) generated by the Earth's surface topography is incorporated into a numerical model of general circulation of the middle and upper atmosphere. Responses of atmospheric general circulation and characteristics of planetary waves at altitudes from the troposphere up to the thermosphere to the effects of OGWs propagating from the earth surface are studied. Changes in atmospheric circulation and amplitudes of planetary waves due to variations of OGW generation and propagation in different seasons are considered. It is shown that during solstices the main OGW dynamical and heat effects occur in the middle atmosphere of winter hemispheres, where changes in planetary wave amplitudes due to OGWs may reach up to 50%. During equinoxes OGW effects are distributed more homogeneously between northern and southern hemispheres. {\textcopyright} 2012 COSPAR. Published by Elsevier Ltd.",
keywords = "Middle and upper atmosphere, circulation, planetary waves, orographic waves, wave heating, parameterization",
author = "Gavrilov, {Nikolai M.} and Koval, {Andrey V.} and Pogoreltsev, {Alexander I.} and Savenkova, {Elena N.}",
year = "2013",
doi = "doi 10.1016/j.asr.2012.12.024",
language = "English",
volume = "51",
pages = "2145--2154",
journal = "Advances in Space Research",
issn = "0273-1177",
publisher = "Elsevier",
number = "11",

}

RIS

TY - JOUR

T1 - Numerical modeling of inhomogeneous orographic wave influence on planetary waves in the middle atmosphere

AU - Gavrilov, Nikolai M.

AU - Koval, Andrey V.

AU - Pogoreltsev, Alexander I.

AU - Savenkova, Elena N.

PY - 2013

Y1 - 2013

N2 - Parameterization of dynamical and thermal effects of stationary orographic gravity waves (OGWs) generated by the Earth's surface topography is incorporated into a numerical model of general circulation of the middle and upper atmosphere. Responses of atmospheric general circulation and characteristics of planetary waves at altitudes from the troposphere up to the thermosphere to the effects of OGWs propagating from the earth surface are studied. Changes in atmospheric circulation and amplitudes of planetary waves due to variations of OGW generation and propagation in different seasons are considered. It is shown that during solstices the main OGW dynamical and heat effects occur in the middle atmosphere of winter hemispheres, where changes in planetary wave amplitudes due to OGWs may reach up to 50%. During equinoxes OGW effects are distributed more homogeneously between northern and southern hemispheres. © 2012 COSPAR. Published by Elsevier Ltd.

AB - Parameterization of dynamical and thermal effects of stationary orographic gravity waves (OGWs) generated by the Earth's surface topography is incorporated into a numerical model of general circulation of the middle and upper atmosphere. Responses of atmospheric general circulation and characteristics of planetary waves at altitudes from the troposphere up to the thermosphere to the effects of OGWs propagating from the earth surface are studied. Changes in atmospheric circulation and amplitudes of planetary waves due to variations of OGW generation and propagation in different seasons are considered. It is shown that during solstices the main OGW dynamical and heat effects occur in the middle atmosphere of winter hemispheres, where changes in planetary wave amplitudes due to OGWs may reach up to 50%. During equinoxes OGW effects are distributed more homogeneously between northern and southern hemispheres. © 2012 COSPAR. Published by Elsevier Ltd.

KW - Middle and upper atmosphere

KW - circulation

KW - planetary waves

KW - orographic waves

KW - wave heating

KW - parameterization

U2 - doi 10.1016/j.asr.2012.12.024

DO - doi 10.1016/j.asr.2012.12.024

M3 - Article

VL - 51

SP - 2145

EP - 2154

JO - Advances in Space Research

JF - Advances in Space Research

SN - 0273-1177

IS - 11

ER -

ID: 5626039