Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R.

Meteor wind results obtained at 93-95 km altitude at seven sites, six in the Soviet Union and one in Antarctica, between 1965 and 1985 are reported. Attention is focussed on the amplitudes and phases of the semi-diurnal tide, showing a 22-yr oscillation, and of the generally weaker diurnal tide. The...

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Bibliographic Details
Main Authors: Lysenko I., Makarov N., Portnyagin Y., Kashcheev B., Lizogub V., Sidorov V., Fahrutdinova A.
Format: Article in Journal/Newspaper
Language:unknown
Published: 1992
Subjects:
Antarc*
Antarctica
Online Access:https://openrepository.ru/article?id=172212
id ftneicon:oai:rour.neicon.ru:rour/172212
record_format openpolar
spelling ftneicon:oai:rour.neicon.ru:rour/172212 2023-05-15T13:58:23+02:00 Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R. Lysenko I. Makarov N. Portnyagin Y. Kashcheev B. Lizogub V. Sidorov V. Fahrutdinova A. 1992 https://openrepository.ru/article?id=172212 unknown Journal of Atmospheric and Terrestrial Physics 7-8 54 915 http://rour.neicon.ru:80/xmlui/bitstream/rour/172212/1/nora.pdf 0021-9169 https://openrepository.ru/article?id=172212 SCOPUS00219169-1992-54-78-SID38249011419 Article 1992 ftneicon 2020-07-21T11:58:42Z Meteor wind results obtained at 93-95 km altitude at seven sites, six in the Soviet Union and one in Antarctica, between 1965 and 1985 are reported. Attention is focussed on the amplitudes and phases of the semi-diurnal tide, showing a 22-yr oscillation, and of the generally weaker diurnal tide. The measurement results are compared with the results of theoretical models. © 1992. Article in Journal/Newspaper Antarc* Antarctica NORA (National aggregator of open repositories of Russian universities)
institution Open Polar
collection NORA (National aggregator of open repositories of Russian universities)
op_collection_id ftneicon
language unknown
description Meteor wind results obtained at 93-95 km altitude at seven sites, six in the Soviet Union and one in Antarctica, between 1965 and 1985 are reported. Attention is focussed on the amplitudes and phases of the semi-diurnal tide, showing a 22-yr oscillation, and of the generally weaker diurnal tide. The measurement results are compared with the results of theoretical models. © 1992.
format Article in Journal/Newspaper
author Lysenko I.
Makarov N.
Portnyagin Y.
Kashcheev B.
Lizogub V.
Sidorov V.
Fahrutdinova A.
spellingShingle Lysenko I.
Makarov N.
Portnyagin Y.
Kashcheev B.
Lizogub V.
Sidorov V.
Fahrutdinova A.
Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R.
author_facet Lysenko I.
Makarov N.
Portnyagin Y.
Kashcheev B.
Lizogub V.
Sidorov V.
Fahrutdinova A.
author_sort Lysenko I.
title Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R.
title_short Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R.
title_full Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R.
title_fullStr Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R.
title_full_unstemmed Seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the U.S.S.R.
title_sort seasonal and latitudinal variations of the lower thermospheric tidal winds from meteor radar measurements in the u.s.s.r.
publishDate 1992
url https://openrepository.ru/article?id=172212
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source SCOPUS00219169-1992-54-78-SID38249011419
op_relation Journal of Atmospheric and Terrestrial Physics
7-8
54
915
http://rour.neicon.ru:80/xmlui/bitstream/rour/172212/1/nora.pdf
0021-9169
https://openrepository.ru/article?id=172212
_version_ 1766266639279456256

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