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Airglow Measurements of Mesospheric Wave Structures and Thermal Gradient Variability over a Low-Latitude Indian Station


Affiliations
1 National Atmospheric Research Laboratory, Pakala Mandal, Gadanki 517 112, India
 

Simultaneous mesospheric OH and O2 temperature estimates are used in the present study to characterize the wave perturbations over Gadanki (13.5°N, 79.2°E), a low-latitude station in India. The 65° zenith angle scanning measurements show large variations from one direction to another. The zonal and vertical wavelengths of the observed wave perturbation are found to vary from 740 to 4500 km and 26 to 38 km. The temperature gradient between OH and O2 layers has been calculated, which shows significant short-period variability. The temperature gradient measurements show large changes from one direction to another. The occurrence of such large temperature gradients within 400 km suggests thermal state of the upper mesosphere to be highly dynamic, which can severely impact the upward propagation of shortperiod gravity waves.

Keywords

Airglow Measurements, Mesosphere, Temperature, Thermal Gradient, Wave Perturbations.
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  • Airglow Measurements of Mesospheric Wave Structures and Thermal Gradient Variability over a Low-Latitude Indian Station

Abstract Views: 301  |  PDF Views: 100

Authors

A. Taori
National Atmospheric Research Laboratory, Pakala Mandal, Gadanki 517 112, India

Abstract


Simultaneous mesospheric OH and O2 temperature estimates are used in the present study to characterize the wave perturbations over Gadanki (13.5°N, 79.2°E), a low-latitude station in India. The 65° zenith angle scanning measurements show large variations from one direction to another. The zonal and vertical wavelengths of the observed wave perturbation are found to vary from 740 to 4500 km and 26 to 38 km. The temperature gradient between OH and O2 layers has been calculated, which shows significant short-period variability. The temperature gradient measurements show large changes from one direction to another. The occurrence of such large temperature gradients within 400 km suggests thermal state of the upper mesosphere to be highly dynamic, which can severely impact the upward propagation of shortperiod gravity waves.

Keywords


Airglow Measurements, Mesosphere, Temperature, Thermal Gradient, Wave Perturbations.



DOI: https://doi.org/10.18520/cs%2Fv106%2Fi4%2F542-551