Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-Shan

Features of the manifestations of various sources of disturbances in the atmospheric electric field at the Tien-Shan high-mountain station have been studied, and the statistical relationship between solar and thunderstorm activity has been established. Air currents arising over the ocean, having ove...

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Main Authors: Valentina Antonova, Vadim Lutsenko, Galina Gordiyenko, Sergey Kryukov
Format: Article
Language:English
Published: MDPI AG 2023-01-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/14/1/164
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author Valentina Antonova
Vadim Lutsenko
Galina Gordiyenko
Sergey Kryukov
author_facet Valentina Antonova
Vadim Lutsenko
Galina Gordiyenko
Sergey Kryukov
author_sort Valentina Antonova
collection DOAJ
description Features of the manifestations of various sources of disturbances in the atmospheric electric field at the Tien-Shan high-mountain station have been studied, and the statistical relationship between solar and thunderstorm activity has been established. Air currents arising over the ocean, having overcome the mountain gorges of the Himalayas, carry moisture to the Northern Tien-Shan and determine the weather features and thunderstorm activity at the Tien-Shan high-mountain station. It was established that the maximum and minimum thunderstorm activity at the Tien-Shan high-mountain station corresponds to the distribution curve of daily thunderstorm activity for the Asia–Australia region. The investigation showed that coronal mass ejections (CMEs) affect the atmospheric electric field by increasing or decreasing its level or causing its fluctuations, depending on the features of manifestations in the near-Earth space and in the Earth’s magnetosphere. In at least 70% of cases, thunderstorm activity was observed with a 1–2-day delay after impact on the Earth’s magnetosphere by CMEs and HSSs. A number of cases were studied when thunderstorm activity was observed in a quiet geomagnetic field. In these cases, an increase in the values of fmin (the minimum frequency of reflection from the ionosphere) and foEs (the critical frequency of the sporadic E layer) was observed, which indicated an increase in the level of radio wave absorption in the ionospheric D-region and the level of electron density at altitudes of 100–120 km.
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spelling doaj.art-8bf78556a4434d6d8cc62a85e5f900622023-11-30T21:10:19ZengMDPI AGAtmosphere2073-44332023-01-0114116410.3390/atmos14010164Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-ShanValentina Antonova0Vadim Lutsenko1Galina Gordiyenko2Sergey Kryukov3Institute of the Ionosphere, JSC National Center for Space Research and Technology, Almaty 050010, KazakhstanInstitute of the Ionosphere, JSC National Center for Space Research and Technology, Almaty 050010, KazakhstanInstitute of the Ionosphere, JSC National Center for Space Research and Technology, Almaty 050010, KazakhstanInstitute of the Ionosphere, JSC National Center for Space Research and Technology, Almaty 050010, KazakhstanFeatures of the manifestations of various sources of disturbances in the atmospheric electric field at the Tien-Shan high-mountain station have been studied, and the statistical relationship between solar and thunderstorm activity has been established. Air currents arising over the ocean, having overcome the mountain gorges of the Himalayas, carry moisture to the Northern Tien-Shan and determine the weather features and thunderstorm activity at the Tien-Shan high-mountain station. It was established that the maximum and minimum thunderstorm activity at the Tien-Shan high-mountain station corresponds to the distribution curve of daily thunderstorm activity for the Asia–Australia region. The investigation showed that coronal mass ejections (CMEs) affect the atmospheric electric field by increasing or decreasing its level or causing its fluctuations, depending on the features of manifestations in the near-Earth space and in the Earth’s magnetosphere. In at least 70% of cases, thunderstorm activity was observed with a 1–2-day delay after impact on the Earth’s magnetosphere by CMEs and HSSs. A number of cases were studied when thunderstorm activity was observed in a quiet geomagnetic field. In these cases, an increase in the values of fmin (the minimum frequency of reflection from the ionosphere) and foEs (the critical frequency of the sporadic E layer) was observed, which indicated an increase in the level of radio wave absorption in the ionospheric D-region and the level of electron density at altitudes of 100–120 km.https://www.mdpi.com/2073-4433/14/1/164thunderstorm activityatmospheric electric fieldearthquakeseffects in the ionosphere
spellingShingle Valentina Antonova
Vadim Lutsenko
Galina Gordiyenko
Sergey Kryukov
Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-Shan
Atmosphere
thunderstorm activity
atmospheric electric field
earthquakes
effects in the ionosphere
title Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-Shan
title_full Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-Shan
title_fullStr Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-Shan
title_full_unstemmed Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-Shan
title_short Impact of Various Disturbance Sources on the Atmospheric Electric Field and Thunderstorm Activity of the Northern Tien-Shan
title_sort impact of various disturbance sources on the atmospheric electric field and thunderstorm activity of the northern tien shan
topic thunderstorm activity
atmospheric electric field
earthquakes
effects in the ionosphere
url https://www.mdpi.com/2073-4433/14/1/164
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