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Airglow measurements of mesospheric wave structures and thermal gradient variability over a low-latitude Indian station

机译:低纬印度台站中层波结构的气辉测量和热梯度变化

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Simultaneous mesospheric OH and O-2 temperature estimates are used in the present study to characterize the wave perturbations over Gadanki (13.5 degrees N, 79.2 degrees E), a low-latitude station in India. The 65 degrees 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 O-2 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 short-period gravity waves.
机译:在本研究中,同时使用了中层大气OH和O-2温度估算值来表征印度低纬度站Gadanki(北纬13.5度,东经79.2度)上的波扰动。 65度天顶角扫描测量结果显示,一个方向到另一个方向的变化很大。发现观察到的波扰动的纬向和垂直波长在740至4500 km和26至38 km之间变化。已计算出OH和O-2层之间的温度梯度,这显示出明显的短期变化。温度梯度测量显示从一个方向到另一方向的较大变化。在400 km内如此大的温度梯度的出现表明上部中层空间的热态是高度动态的,这可能严重影响短周期重力波的向上传播。

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