A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during 1986-1995 at the Eastern European mid-latitude station of - Kazan (56° N, 49° E) has been used to determine the height structure of parameters of prevailing and tidal movements of the zonal and meridional circulation, their inter-annual, annual, semi-annual oscillations and several-year averages; height and seasonal structures of wave disturbances of prevailing circulation with time scales of planetary waves; investment of long-period internal gravity waves in prevailing circulation was evaluated. The influence of solar cycle activity on dynamics has also been determined. © 1999 COSPAR. Published by Elsevier Science Ltd
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
In this papers the investigation of time variations of the energy of background motions as well as t...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
In this papers the investigation of time variations of the energy of background motions as well as t...
In this papers the investigation of time variations of the energy of background motions as well as t...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
In this papers the investigation of time variations of the energy of background motions as well as t...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
In this papers the investigation of time variations of the energy of background motions as well as t...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
In this papers the investigation of time variations of the energy of background motions as well as t...
In this papers the investigation of time variations of the energy of background motions as well as t...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
In this papers the investigation of time variations of the energy of background motions as well as t...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
In this papers the investigation of time variations of the energy of background motions as well as t...