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ISSLEDOVANIE VNUTRENNIKH GRAVITATSIONNYKH VOLN V NIZHNEI ATMOSFERE PO IZOFOTAM SVECHENIYA NOCHNOGO NEBA. / Gavrilov, N. M.; Shved, G. M.

In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, Vol. 18, No. 1, 1982, p. 8-18.

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

Harvard

Gavrilov, NM & Shved, GM 1982, 'ISSLEDOVANIE VNUTRENNIKH GRAVITATSIONNYKH VOLN V NIZHNEI ATMOSFERE PO IZOFOTAM SVECHENIYA NOCHNOGO NEBA.', Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, vol. 18, no. 1, pp. 8-18.

APA

Gavrilov, N. M., & Shved, G. M. (1982). ISSLEDOVANIE VNUTRENNIKH GRAVITATSIONNYKH VOLN V NIZHNEI ATMOSFERE PO IZOFOTAM SVECHENIYA NOCHNOGO NEBA. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, 18(1), 8-18.

Vancouver

Gavrilov NM, Shved GM. ISSLEDOVANIE VNUTRENNIKH GRAVITATSIONNYKH VOLN V NIZHNEI ATMOSFERE PO IZOFOTAM SVECHENIYA NOCHNOGO NEBA. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1982;18(1):8-18.

Author

Gavrilov, N. M. ; Shved, G. M. / ISSLEDOVANIE VNUTRENNIKH GRAVITATSIONNYKH VOLN V NIZHNEI ATMOSFERE PO IZOFOTAM SVECHENIYA NOCHNOGO NEBA. In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1982 ; Vol. 18, No. 1. pp. 8-18.

BibTeX

@article{02c65c6417b94df7bea6e221d1ba17bf,
title = "ISSLEDOVANIE VNUTRENNIKH GRAVITATSIONNYKH VOLN V NIZHNEI ATMOSFERE PO IZOFOTAM SVECHENIYA NOCHNOGO NEBA.",
abstract = "Using a multipoint method of detecting internal gravity waves (IGW), an analysis is made of 92 sessions of observations of the variations in the intensity of the left bracket 01 right bracket 5577 A night airglow in Ashkhabad. Criteria for selecting frequency harmonics caused by IGW are established, and the seasonal variations of IGW parameters are studied. It is found that the directions of propagation of IGW vary especially greatly from winter to summer. The seasonal-azimuthal distribution of the chosen indices of dynamic activity of the lower atmosphere, together with the seasonal variation of the filter effect of the upper stratosphere - lower mesosphere jetstream, can explain the seasonal variation of the dominant directions of propagation of IGW observed over Ashkabad at heights of the left bracket OI right bracket 5577 A night airglow.",
author = "Gavrilov, {N. M.} and Shved, {G. M.}",
year = "1982",
language = "русский",
volume = "18",
pages = "8--18",
journal = "Izvestiya - Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - ISSLEDOVANIE VNUTRENNIKH GRAVITATSIONNYKH VOLN V NIZHNEI ATMOSFERE PO IZOFOTAM SVECHENIYA NOCHNOGO NEBA.

AU - Gavrilov, N. M.

AU - Shved, G. M.

PY - 1982

Y1 - 1982

N2 - Using a multipoint method of detecting internal gravity waves (IGW), an analysis is made of 92 sessions of observations of the variations in the intensity of the left bracket 01 right bracket 5577 A night airglow in Ashkhabad. Criteria for selecting frequency harmonics caused by IGW are established, and the seasonal variations of IGW parameters are studied. It is found that the directions of propagation of IGW vary especially greatly from winter to summer. The seasonal-azimuthal distribution of the chosen indices of dynamic activity of the lower atmosphere, together with the seasonal variation of the filter effect of the upper stratosphere - lower mesosphere jetstream, can explain the seasonal variation of the dominant directions of propagation of IGW observed over Ashkabad at heights of the left bracket OI right bracket 5577 A night airglow.

AB - Using a multipoint method of detecting internal gravity waves (IGW), an analysis is made of 92 sessions of observations of the variations in the intensity of the left bracket 01 right bracket 5577 A night airglow in Ashkhabad. Criteria for selecting frequency harmonics caused by IGW are established, and the seasonal variations of IGW parameters are studied. It is found that the directions of propagation of IGW vary especially greatly from winter to summer. The seasonal-azimuthal distribution of the chosen indices of dynamic activity of the lower atmosphere, together with the seasonal variation of the filter effect of the upper stratosphere - lower mesosphere jetstream, can explain the seasonal variation of the dominant directions of propagation of IGW observed over Ashkabad at heights of the left bracket OI right bracket 5577 A night airglow.

UR - http://www.scopus.com/inward/record.url?scp=0019913757&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0019913757

VL - 18

SP - 8

EP - 18

JO - Izvestiya - Atmospheric and Oceanic Physics

JF - Izvestiya - Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 1

ER -

ID: 87735609