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Ionospheric disturbances at low and mid-low latitudes of the South American sector during the March 2015 great storm

机译:2015年3月大风暴期间,南美地区低纬度和中低纬度的电离层扰动

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This paper analyzes the response of the near equatorial and low latitude ionosphere of the South American sector to the geomagnetic storm occurred on 17 March 2015. lonosonde data from Ramey (18.5 degrees N, 292.9 degrees E), Jicamarca (12.0 degrees S, 283.2 degrees E), Boa Vista (2.8 degrees N, 299.3 degrees E), Sao Luis (2.6 degrees S, 315.8 degrees E), Fortaleza (3.9 degrees S, 321.6 degrees E) and Cachoeira Paulista (22.7 degrees S, 315.0 degrees E) are used for the study. The results show negative disturbances in foF2 at low latitudes during the main phase of the storm, which were attributed to prompt penetration electric fields. Thus, the Equatorial Anomaly (EA) started to reduce their structure in this sector since on 17 March. During the recovery phase (on 18 March), positive disturbances were observed at low, mid-low latitudes (in the post-midnight - predawn hours), which can be mainly attributed to enhanced storm-time neutral winds and composition changes (i.e., increase in the O/N2 ratio). Disturbance dynamo electric fields would also contribute in modulating the electron density of the EA during this storm period. (C) 2019 COSPAR. Published by Elsevier Ltd. All rights reserved.
机译:本文分析了南美地区近赤道和低纬度电离层对2015年3月17日发生的地磁风暴的响应。来自拉米(北纬18.5度,东经292.9度),贾卡马卡(南经12.0度,283.2度)的探空仪数据E),博阿维斯塔(北纬2.8度,东经299.3度),圣路易斯(南纬2.6度,东经315.8度),福塔莱萨(南纬3.9度,东经321.6度)和卡乔埃拉保利斯塔(南纬22.7度,东经315.0度)是用于研究。结果表明,在风暴的主要阶段,低纬度地区foF2产生了负面干扰,这归因于快速穿透电场。因此,自3月17日以来,赤道异常(EA)开始缩小该部门的结构。在恢复阶段(3月18日),在低,中低纬度(午夜后到黎明前)观测到了积极干扰,这主要归因于风暴时中风和成分变化的增加(即, O / N2比增加)。在此风暴期间,干扰发电机电场也将有助于调节EA的电子密度。 (C)2019 COSPAR。由Elsevier Ltd.出版。保留所有权利。

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