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太阳活动周期24下降阶段太阳风高速流对巴西低纬度电离层的影响

Influence of Solar Wind High-Speed Streams on the Brazilian Low-Latitude Ionosphere During the Descending Phase of Solar Cycle 24.

作者信息

Moraes-Santos S P, Cândido C M N, Becker-Guedes F, Nava B, Klausner V, Borries C, Chingarandi F S, Osanyin T O

机构信息

National Institute for Space Research São José dos Campos Brazil.

University of the Vale of Paraíba UNIVAP São José dos Campos Brazil.

出版信息

Space Weather. 2024 Dec;22(12):e2024SW003873. doi: 10.1029/2024SW003873. Epub 2024 Nov 28.

DOI:10.1029/2024SW003873
PMID:39620208
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11604352/
Abstract

This study investigates the Brazilian low-latitude ionospheric response to CIR/HSS-driven geomagnetic storms during the declining phase of solar cycle 24, from 2016 to 2017. In this period the geomagnetic storms were mostly moderate, SymH ≈ -72 nT, AE ≈ 1580 nT, Vsw ≈ 690 km/s and lasted, on average, for 6 days. We analyze the variations in Vertical Total Electron Content (VTEC) at three representative regions: bele, over the equatorial region; boav and cuib, at the northern and southern crests of the Equatorial Ionization Anomaly. Our findings reveal the role of High-Speed Solar Wind Streams and Corotating Interaction Region-driven geomagnetic storms. The VTEC intensifications were up to 30 TECu, during the daytime and nighttime. Additionally, three categories of nighttime enhancements were observed and analyzed with distinct characteristics and levels of pre-reversal strengthening; Depletions up to 20 TECu also occurred during the day and nighttime. The delay between the storm commencement and the positive and negative variations were, on average, 7 and 20 hours, respectively. We discuss the Prompt Penetration Electric Fields and Disturbance Dynamo Electric Fields following the magnetic reconnection between Earth's and interplanetary magnetic field, using observational data and modeling. Furthermore, this study presents catalogs of low-latitude ionospheric storms, providing detailed information for space weather applications and ionospheric modeling.

摘要

本研究调查了2016年至2017年太阳活动周期24下降阶段巴西低纬度电离层对共转相互作用区/高速太阳风驱动的地磁暴的响应。在此期间,地磁暴大多为中等强度,SymH≈ -72 nT,AE≈ 1580 nT,Vsw≈ 690 km/s,平均持续6天。我们分析了三个代表性区域垂直总电子含量(VTEC)的变化:赤道地区的贝莱;赤道电离异常南北峰处的博阿夫和库伊布。我们的研究结果揭示了高速太阳风流和共转相互作用区驱动的地磁暴的作用。白天和夜间,VTEC增强高达30 TECu。此外,还观测并分析了三类夜间增强现象,它们具有不同的特征和反转前增强水平;白天和夜间也出现了高达20 TECu的损耗。地磁暴开始与正负变化之间的延迟平均分别为7小时和20小时。我们利用观测数据和模型,讨论了地球磁场与行星际磁场磁重联后的迅速穿透电场和扰动发电机电场。此外,本研究还给出了低纬度电离层暴的目录,为空间天气应用和电离层建模提供了详细信息。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5a7c/11604352/17a93ea3705b/SWE-22-0-g004.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5a7c/11604352/535343d0b331/SWE-22-0-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5a7c/11604352/17a93ea3705b/SWE-22-0-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5a7c/11604352/934f8ccfe803/SWE-22-0-g005.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5a7c/11604352/535343d0b331/SWE-22-0-g001.jpg
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本文引用的文献

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Solar wind stream interaction regions throughout the heliosphere.贯穿整个日球层的太阳风气流相互作用区域。
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Ionospheric redistribution during geomagnetic storms.地磁暴期间的电离层重新分布。
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