Method of studying infrasound waves from thunderstorms

A. Sorokin, V. Dobrynin
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Abstract

The paper provides an overview of studies of infrasound signals from thunderstorms over a period of more than 30 years. We deal with several types of infrasound signals from thunderstorms detected at the ISTP SB RAS infrasound station Badary in Buryatia. Special attention is paid to signals arising during the rarefaction phase. A mechanism for generating signals of this type by converting the energy of the electrostatic field into fluctuations in the pressure field was proposed by Dessler in 1973. We propose a method for identifying thunderstorm infrasound signals of various types: 1 — signals from an expanding thermal lightning channel; 2 — signals with an electrostatic generation mechanism. Using infrasound signals recorded earlier at the station in Buryatia as an example, we discuss the validity of the thunderstorm cloud model and assess some parameters of the thunderstorm source of infrasound.
研究雷暴中次声波的方法
本文概述了30多年来雷暴次声信号的研究概况。我们处理在布里亚特巴德里的isp SB RAS次声站探测到的雷暴的几种类型的次声信号。特别注意在稀薄阶段产生的信号。Dessler于1973年提出了一种将静电场的能量转化为压力场的波动来产生这种类型信号的机制。我们提出了一种识别各种雷暴次声信号的方法:1 -来自扩展的热闪电通道的信号;2 -信号与静电产生机制。以布里亚特站早期记录的次声信号为例,讨论了雷暴云模型的有效性,并对次声雷暴源的一些参数进行了评估。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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