西伯利亚西部气候站雷暴活动年变率监测

S. I. Pryakhina, A. Kotova
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摘要

本文介绍了1971 - 2020年50年间西伯利亚西部9个气象站雷暴活动年变率的研究结果。研究表明,雷暴活动具有复杂的准周期结构,森林-冻土带雷暴活动具有7 ~ 8年的显著周期,针叶林带和森林-草原雷暴活动具有2 ~ 4年的显著周期。揭示了西伯利亚西部各气象站的雷暴频率在每几十年的增减周期中具有同步过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Monitoring of annual variability of thunderstorm activity for climatic stations of Western Siberia
The article presents the study results of the annual variability of thunderstorm activity at nine climatic stations in Western Siberia over a fifty-year period from 1971 to 2020. The study revealed a complex quasi-periodic structure of thunderstorm activity series with the most pronounced amplitude of 7–8-year cycles for the forest-tundra and a 2–4-year cycle for the taiga zone, as well as forest-steppes. A synchronous course of increase and decrease periods in the frequency of thunderstorms for individual decades at the studied climatic stations in Western Siberia was revealed.
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