36-40An experiment was conducted with the Indian MST radar (in ST mode) at Gadanki (13.47°N, 79.18°E) in March 1992 to study the diurnal non-migrating tidal variation in the lower troposphere. The results obtained are presented in this paper and they do not indicate any evidence for the presence of the diurnal non-migrating tides in the lower troposphere over Gadanki
Wind observations made at Gadanki (13.5°N) by using Indian MST Radar for few days in September, Oct...
Doppler SODAR Sound Detection and Ranging is used to measure vertical velocity in order to investiga...
21-29The Indian Mesosphere-Stratosphere-Troposphere (MST) radar, installed at Gadanki (13.47°N, 79.1...
210-221A study of seasonal differences of diurnal tidal oscillations in zonal and merid ional winds...
Diurnal tidal components in horizontal winds measured by MST radar in the troposphere and lower ...
International audienceDiurnal tidal components in horizontal winds measured by MST radar in the trop...
30-35The Indian MST radar located at Gadanki (13.47°N, 79.18°E) near Tirupati, Andhra Pradesh, was o...
Significant attention is being paid in recent times by several observational and modeling studies to...
Low-latitude mesospheric winds are investigated using data collected from 1995 to 2006 (11 years) by...
52-58Results of the ST mode experiments using the Indian MST radar for a 24-h period during 21-22 Ma...
Mean winds and tidal signatures in the mesosphere and lower thermosphere (MLT) region are derived fr...
Mean winds and tidal signatures in the mesosphere and lower thermosphere (MLT) region are derived fr...
41-51Clear-air radars are widely used for measuring atmospheric windfield with good height and time ...
Comparisons are made between horizontal wind measurements carried out using Indian mesosphere-strato...
The vertical velocity in the troposphere-lower stratosphere region measured using MST radar has be...
Wind observations made at Gadanki (13.5°N) by using Indian MST Radar for few days in September, Oct...
Doppler SODAR Sound Detection and Ranging is used to measure vertical velocity in order to investiga...
21-29The Indian Mesosphere-Stratosphere-Troposphere (MST) radar, installed at Gadanki (13.47°N, 79.1...
210-221A study of seasonal differences of diurnal tidal oscillations in zonal and merid ional winds...
Diurnal tidal components in horizontal winds measured by MST radar in the troposphere and lower ...
International audienceDiurnal tidal components in horizontal winds measured by MST radar in the trop...
30-35The Indian MST radar located at Gadanki (13.47°N, 79.18°E) near Tirupati, Andhra Pradesh, was o...
Significant attention is being paid in recent times by several observational and modeling studies to...
Low-latitude mesospheric winds are investigated using data collected from 1995 to 2006 (11 years) by...
52-58Results of the ST mode experiments using the Indian MST radar for a 24-h period during 21-22 Ma...
Mean winds and tidal signatures in the mesosphere and lower thermosphere (MLT) region are derived fr...
Mean winds and tidal signatures in the mesosphere and lower thermosphere (MLT) region are derived fr...
41-51Clear-air radars are widely used for measuring atmospheric windfield with good height and time ...
Comparisons are made between horizontal wind measurements carried out using Indian mesosphere-strato...
The vertical velocity in the troposphere-lower stratosphere region measured using MST radar has be...
Wind observations made at Gadanki (13.5°N) by using Indian MST Radar for few days in September, Oct...
Doppler SODAR Sound Detection and Ranging is used to measure vertical velocity in order to investiga...
21-29The Indian Mesosphere-Stratosphere-Troposphere (MST) radar, installed at Gadanki (13.47°N, 79.1...
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