大气放电现象和带电尘埃粒子相互作用的实验建模

Mohamad E. Abdelaal, Igor. V. Dokuchaev, Elena A. Malinovskaya, Stanislav I. Klimov, Genady G. Dolnikov, Alexander V. Zakharov
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引用次数: 0

摘要

高层大气包括中间层和热层,受到各种大气层和磁层撞击的复杂影响。对流层中激发的各种大气波能传播到中间层-热层(M-T)区域,改变其动态。此外,中间层大气中的大规模扰动,如太阳活动引起的平流层突然变暖和地磁扰动,也会影响高层大气。为了更好地了解这些复杂的过程,有必要利用多种平台和仪器进行观测,并开展建模研究。本研究介绍了对大气放电条件产生的电磁特征的实验研究,包括带电尘埃粒子的击穿事件和相互作用。使用真空室模拟高层大气条件。电磁信号分析仪(EMA)记录了大气放电产生的信号和带电尘埃粒子的电磁特征。实验研究的结果揭示了地球大气层内击穿事件和带电粒子相互作用期间发生的独特电磁过程。电磁信号分析仪记录的信号为了解大气放电条件的特征和带电尘埃粒子的行为提供了宝贵的信息。这些发现有助于我们了解高层大气中复杂的相互作用。对结果的进一步分析凸显了大气放电、电磁过程和尘埃粒子相互作用在塑造该区域动态方面的重要性。本研究提出的实验方法为研究大气过程及其对空间天气动力学的影响提供了宝贵的工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Experimental modeling of atmospheric discharge phenomena and charged dust particle interactions
The upper atmosphere, comprising the mesosphere and thermosphere, is intricately influenced by various atmospheric and magnetospheric impacts. Various atmospheric waves excited in the troposphere can propagate into the mesosphere-thermosphere (M-T) region, altering its dynamics. Additionally, large-scale disturbances in the middle atmosphere, such as sudden stratospheric warming and geomagnetic disturbances induced by solar activity, affect the upper atmosphere. To better understand these complex processes, observations from multiple platforms and instruments, along with modeling studies, are necessary. This study presents experimental investigations into the electromagnetic signatures generated by atmospheric discharge conditions, including breakdown events and interactions of charged dust particles. A vacuum chamber was used to simulate upper atmospheric conditions. An electromagnetic signal analyzer (EMA) registered signals generated from the atmospheric discharge and the electromagnetic signature of charged dust particles. The results of the experimental investigations revealed distinctive electromagnetic processes occurring during breakdown events and charged particle interactions within Earth’s atmosphere. Signals recorded by the electromagnetic signal analyzer provided valuable insights into the characteristics of atmospheric discharge conditions and the behavior of charged dust particles. The findings contribute to our understanding of the complex interactions in the upper atmosphere. Further analysis of the results highlights the significance of the atmospheric discharge, electromagnetic processes, and dust particle interactions in shaping the dynamics of this region. The experimental approach presented in this study offers a valuable tool for studying atmospheric processes and their implications for space weather dynamics.
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