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Thunderstorm induced stratosphere-troposphere exchange during pre-monsoon over Kochi

机译:在高知前季风期间,雷暴引起的平流层-对流层交换

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The processes in Stratosphere and Troposphere are strongly correlated with each other and exchange of water vapor, momentum and energy between these two layers have much significance on climate. Recent studies indicate that stratospheric water vapor and its variability play an important role in changing climate. High-resolution data, even though available only at few locations, are highly useful for the analysis of stratosphere troposphere exchange. A stratosphere-troposphere (ST) radar (205 MHz) is operational at the Advanced Centre for Atmospheric Radar Research (10.04N; 76.33E), Cochin University of Science and Technology, India. This radar provides accurate measurements of upper troposphere-lower stratosphere (UTLS) region. Observations made during May 16 – 19, 2017, few days prior to the onset of Indian summer monsoon show that strong convection reached the tropopause height and disturbed the tropopause.
机译:平流层和对流层的过程之间密切相关,这两层之间的水蒸气,动量和能量的交换对气候具有重要意义。最近的研究表明,平流层水汽及其变化在气候变化中起着重要作用。高分辨率数据,即使仅在少数几个位置可用,对于分析平流层对流层交换也非常有用。印度科钦科技大学的平流层-对流层(ST)雷达(205 MHz)在大气雷达研究高级中心(10.04N; 76.33E)运行。该雷达提供对流层低平流层上方(UTLS)区域的准确测量。在2017年5月16日至19日(印度夏季风爆发前几天)进行的观测显示,强对流到达对流层顶高度并扰乱了对流层顶。

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