Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica

The variability in the atmospheric electric field is modulated by a combination of solar activities, meteorological activities, and geological conditions. A foundational dataset of the daily variations in the fair-weather atmospheric electric field is established in this study, and several examinati...

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Published in:Applied Sciences
Main Authors: Lei Li, Tao Chen, Shuo Ti, Shi-Han Wang, Jia-Jun Song, Chun-Lin Cai, Yong-Hua Liu, Wen Li, Jing Luo
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/app12189248
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author Lei Li
Tao Chen
Shuo Ti
Shi-Han Wang
Jia-Jun Song
Chun-Lin Cai
Yong-Hua Liu
Wen Li
Jing Luo
author_facet Lei Li
Tao Chen
Shuo Ti
Shi-Han Wang
Jia-Jun Song
Chun-Lin Cai
Yong-Hua Liu
Wen Li
Jing Luo
author_sort Lei Li
collection MDPI Open Access Publishing
container_issue 18
container_start_page 9248
container_title Applied Sciences
container_volume 12
description The variability in the atmospheric electric field is modulated by a combination of solar activities, meteorological activities, and geological conditions. A foundational dataset of the daily variations in the fair-weather atmospheric electric field is established in this study, and several examinations are conducted into the details of these variations in particular regions. This paper is organized as follows. First, the researchers count the datasets of daily variations to the atmospheric electric field on fair-weather days from 1 March–1 August 2022 at Zhongshan Chinese Station in Antarctica and Changping Station in Beijing. Then, the average daily variation in the atmospheric electric field on 40 fair-weather days in Antarctica is shown and the variations are compared with the average curve of 37 fair-weather days in Beijing during the same time period. Finally, the three main differences between these variations, their possible reasons, and a reasonable error analysis are clarified and discussed at the end of this paper.
format Text
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
geographic Antarctic
Zhongshan
geographic_facet Antarctic
Zhongshan
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institution Open Polar
language English
long_lat ENVELOPE(76.371,76.371,-69.373,-69.373)
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op_doi https://doi.org/10.3390/app12189248
op_relation Earth Sciences and Geography
https://dx.doi.org/10.3390/app12189248
op_rights https://creativecommons.org/licenses/by/4.0/
op_source Applied Sciences; Volume 12; Issue 18; Pages: 9248
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spelling ftmdpi:oai:mdpi.com:/2076-3417/12/18/9248/ 2025-01-16T19:19:49+00:00 Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica Lei Li Tao Chen Shuo Ti Shi-Han Wang Jia-Jun Song Chun-Lin Cai Yong-Hua Liu Wen Li Jing Luo agris 2022-09-15 application/pdf https://doi.org/10.3390/app12189248 EN eng Multidisciplinary Digital Publishing Institute Earth Sciences and Geography https://dx.doi.org/10.3390/app12189248 https://creativecommons.org/licenses/by/4.0/ Applied Sciences; Volume 12; Issue 18; Pages: 9248 atmospheric electric field Zhongshan Chinese Antarctic station fair weather Text 2022 ftmdpi https://doi.org/10.3390/app12189248 2023-08-01T06:28:59Z The variability in the atmospheric electric field is modulated by a combination of solar activities, meteorological activities, and geological conditions. A foundational dataset of the daily variations in the fair-weather atmospheric electric field is established in this study, and several examinations are conducted into the details of these variations in particular regions. This paper is organized as follows. First, the researchers count the datasets of daily variations to the atmospheric electric field on fair-weather days from 1 March–1 August 2022 at Zhongshan Chinese Station in Antarctica and Changping Station in Beijing. Then, the average daily variation in the atmospheric electric field on 40 fair-weather days in Antarctica is shown and the variations are compared with the average curve of 37 fair-weather days in Beijing during the same time period. Finally, the three main differences between these variations, their possible reasons, and a reasonable error analysis are clarified and discussed at the end of this paper. Text Antarc* Antarctic Antarctica MDPI Open Access Publishing Antarctic Zhongshan ENVELOPE(76.371,76.371,-69.373,-69.373) Applied Sciences 12 18 9248
spellingShingle atmospheric electric field
Zhongshan Chinese Antarctic station
fair weather
Lei Li
Tao Chen
Shuo Ti
Shi-Han Wang
Jia-Jun Song
Chun-Lin Cai
Yong-Hua Liu
Wen Li
Jing Luo
Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica
title Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica
title_full Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica
title_fullStr Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica
title_full_unstemmed Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica
title_short Fair-Weather Near-Surface Atmospheric Electric Field Measurements at the Zhongshan Chinese Station in Antarctica
title_sort fair-weather near-surface atmospheric electric field measurements at the zhongshan chinese station in antarctica
topic atmospheric electric field
Zhongshan Chinese Antarctic station
fair weather
topic_facet atmospheric electric field
Zhongshan Chinese Antarctic station
fair weather
url https://doi.org/10.3390/app12189248