Research in dynamic processes in the lower thermosphere has been carried out in Kazan using the meteor radar facilities of the Kazan State University under the MAP-GLOBMET international program. Presented is experimental data on seasonal dependences of the wind for anomalous winter circulation periods, spring and autumn reconstructions and stable summer circulation from observations conducted in 1978 to 1984. Prevailing wind parameters are shown: zonal and meridional component amplitudes and A sub 0 and azimuth of the prevailing wind vector. The values are also presented for semidiurnal zonal and meridional tidal components, their correlation coefficient and zonal component amplitude maximum time
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
The lower thermosphere occupies the intermediate position between the overlying thermospheric layers...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
Temporal variations of prevailing winds at 90 to 100 km obtained from measurements carried out in wi...
Meteor wind results obtained at 93-95 km altitude at seven sites, six in the Soviet Union and one in...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
The determination of climatic norms of wind regime parameters in the lower thermosphere requires som...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
The dynamics of the mesosphere and lower thermosphere (80-110 km) are investigated using data for 19...
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...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
The lower thermosphere occupies the intermediate position between the overlying thermospheric layers...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
Temporal variations of prevailing winds at 90 to 100 km obtained from measurements carried out in wi...
Meteor wind results obtained at 93-95 km altitude at seven sites, six in the Soviet Union and one in...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
Using long-term radio meteoric observations of wind at Kazan (52°N, 49°E) from 1978 to 1988, the hei...
The determination of climatic norms of wind regime parameters in the lower thermosphere requires som...
A homogeneous series of radiometeor observations in the height interval of 80-110 km obtained during...
The dynamics of the mesosphere and lower thermosphere (80-110 km) are investigated using data for 19...
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...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
This paper presents the experimental results for the circulation in the 80-110 km height region obta...
Nowadays investigations of the wind regime of the mesosphere - lower thermosphere (80-100 km) using ...
The lower thermosphere occupies the intermediate position between the overlying thermospheric layers...