Diurnal observation of the deep convective precipitation system and the associated gravity wave signatures using 206.5 MHz VHF radar over the central Himalayas

A. Jaiswal, M. Naja, S. Bhattacharjee
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Abstract

With the aim to explore the dynamical behavior of the lower atmosphere during precipitation in monsoon season over Himalayan region, diurnal observation with ARIES Stratosphere Troposphere radar were conducted from September 23 to 24, 2020. Development and evolution of the precipitation system was studied through the derived high resolution wind profiles from radar as well as from radar backscattered power and spectral width. A burst of gravity wave of 8 −10 minutes in period was detected before the precipitation in the mid-troposphere. Similarly gravity waves signatures of 25 minute period were detected among the updraft and downdraft couplet in the upper troposphere and lower stratosphere region during convective precipitation. Overall depletion of turbulent echo power is detected and significant reduction of about 6 dB in radar SNR in noticed around tropopause height during convection. Significant enhancement of horizontal momentum flux noticed during convection period at all height levels.
206.5 MHz VHF雷达对喜马拉雅中部地区深对流降水系统及其重力波特征的日观测
为了探讨喜马拉雅地区季风季节降水过程中低层大气的动力特征,于2020年9月23日至24日利用ARIES平流层对流层雷达进行了逐日观测。利用雷达反演的高分辨率风廓线以及雷达后向散射功率和谱宽对降水系统的发展演变进行了研究。在对流层中降水发生前,探测到一个周期为8 ~ 10分钟的重力波爆发。在对流降水过程中,对流层上层和平流层下层的上升气流和下降气流对偶中也检测到25分钟周期的重力波特征。在对流过程中,在对流层顶高度附近探测到湍流回波功率的总体损耗,雷达信噪比显著降低约6 dB。对流期各高度水平动量通量显著增强。
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