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Seasonal characteristics of gravity waves in the middle atmosphere over Gadanki using Rayleigh lidar observations

机译:利用瑞利激光雷达观测,Gadanki上层中层大气重力波的季节特征

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摘要

Extensive study of middle atmospheric gravity waves (GWs) has been carried out to characterize seasonal variability of wave associated potential energy and vertical component of horizontal momentum flux with long term database (1998-2008) over Gadanki (13.5°N, 79.2°E), India. GWs are observed to transport significant energy and momentum flux with considerable variability throughout the seasons. Wave dissipation is found to be quite large (>30%) at upper mesospheric altitude. Dominant annual oscillation (AO) is observed in the energy and momentum flux pattern in the middle atmosphere. Power spectral density of the vertical wavenumber spectra of normalized temperature derived for the upper stratosphere and mesosphere exhibit resemblance in the saturated region. Logarithmic slope of vertical wavenumber spectra reveals more negative value and near to the model estimation in the upper stratosphere (~-2.83) than the mesosphere (~-2.43), which implies linear wave theory can explain stratospheric wave characteristics in a better way than mesospheric characteristics.
机译:借助Gadanki(13.5°N,79.2°E)的长期数据库(1998-2008),已对中层大气重力波(GWs)进行了广泛的研究,以表征波浪相关势能和水平动量通量的垂直分量的季节性变化。 ,印度。在整个季节中,观测到的GWs传输的能量和动量通量都具有很大的变化性。发现在较高的中层高度,波消散非常大(> 30%)。在中层大气的能量和动量通量模式中观察到了显着的年振荡(AO)。高层平流层和中层大气的归一化温度垂直波数谱的功率谱密度在饱和区域表现出相似性。垂直波数谱的对数斜率比平流层(〜-2.43)在平流层上层(〜-2.83)处显示出更多的负值并且更接近模型估计,这意味着线性波理论比平流层可以更好地解释平流层的波特征特征。

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