An Investigation of the Third Harmonic Power Line Emission in the Topside Ionosphere During the Recent Solar Minimum Period

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Li Liao, Shufan Zhao, Zhenhui Ma, Xuhui Shen, Huaiyun Peng, HengXin Lu
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Abstract

Power line harmonic radiation (PLHR) events are radiated by electric power systems on the ground at harmonics of the base power system frequency (50 or 60 Hz, depending on the region). We analyze the global third harmonics PLHR at 150 and 180 Hz using electric field data collected by China Seismo-Electromagnetic Satellite during the recent solar minimum between January 2019 and December 2022. The average frequency spectrum over industrialized areas shows that the third harmonic has a high occurrence rate in the U.S. region, as well as in western China and northern India, but is very low in the European region. In particular, in the China region and the U.S. region, more than 11,000 and 24,000 dayside and nightside third harmonic PLHR events have been detected from 2019 to 2022, respectively. Compared to the 150 Hz PLHR occurrence rate detected above the China region, the 180 Hz PLHR occurrence rate above the U.S. region is higher, which reveals a significant regional difference. In addition, both at nighttime and daytime, the PLHR electric field intensities at 180 Hz are higher than that at 60 Hz above the U.S. region, which is also different from the result above the China region.

近期太阳极小期顶层电离层三次谐波电力线发射研究
电力线谐波辐射(PLHR)事件是电力系统在地面上以基本电力系统频率(50 或 60 赫兹,视地区而定)的谐波进行辐射的。我们利用中国地震电磁卫星在 2019 年 1 月至 2022 年 12 月最近一次太阳极小期期间收集的电场数据,分析了 150 和 180 Hz 的全球三次谐波 PLHR。工业化地区的平均频谱显示,三次谐波在美国地区、中国西部和印度北部出现率很高,但在欧洲地区出现率很低。特别是在中国地区和美国地区,从 2019 年到 2022 年,分别探测到超过 11,000 次和 24,000 次日侧和夜侧三次谐波 PLHR 事件。与中国地区上空检测到的 150 赫兹 PLHR 发生率相比,美国地区上空的 180 赫兹 PLHR 发生率更高,显示出显著的地区差异。此外,无论是夜间还是白天,美国地区上空 180 Hz 的 PLHR 电场强度均高于 60 Hz,这也与中国地区上空的结果不同。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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