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Low-latitude ionosphere response to super geomagnetic storm of 17/18 March 2015: Results from a chain of ground-based observations over Indian sector

机译:低纬度电离层响应超级17/18 2015年3月:结果的磁暴从地面观测的链印度的部门

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In this paper, we present unique results of equatorial and low-latitude ionosphere response to one of the major geomagnetic storms of the current solar cycle that occurred during 17–18 March 2015, where Dst reached its minimum of -228 nT. Here we utilized data from magnetometers, chain of ionosondes located at Tirunelveli (8.73°N, 77.70°E; geometry: 0.32°N), Hyderabad (17.36°N, 78.47°E; geometry 8.76°N), and Allahabad (25.45°N, 81.85°E; geometry 16.5°N) along with multistation GPS receivers over Indian sector. The observations showed a remarkable increase of h′F to as high as ~560 km over Tirunelveli (magnetic equator) with vertical drift of ~70m/s at 13:30 UT due to direct penetration of storm time eastward electric fields which exactly coincided with the local time of pre-reversal enhancement (PRE) and caused intense equatorial spread F irregularities in ionosondes and scintillations in GPS receivers at wide latitudes. Plasma irregularities are so intense that their signatures are seen in Allahabad/Lucknow. Storm time thermospheric meridional winds as estimated using two ionosondes suggest the equatorward surge of gravity waves with period of ~2 h. Suppression of anomaly crest on the subsequent day of the storm suggests the complex role of disturbance dynamo electric fields and disturbance wind effects. Our results also show an interesting feature of traveling ionospheric disturbances possibly associated with disturbance meridional wind surge during recovery phase. In addition, noteworthy observations are nighttime westward zonal drifts and PRE-related total electron content enhancements at anomaly crests during main phase and counter electrojet signatures during recovery phase.
机译:在本文中,我们目前唯一的结果赤道和低纬度电离层响应的一个主要的地磁风暴当前太阳周期发生在17 - 182015年3月,Dst达到最低-228从磁力计nT。在这里我们利用数据,ionosondes位于Tirunelveli链(8.73°N, 77.70°E;(17.36°N, 78.47°E;阿拉哈巴德(25.45°N, 81.85°E;随着多站在印度的GPS接收器部门。增加h 'F高达~ 560公里与垂直Tirunelveli(磁赤道)漂移13:30 ~ 70 m / s的UT直接造成的东电风暴的渗透时间字段,恰逢当地pre-reversal增强(前)和引起的强烈的赤道扩展F中的违规行为ionosondes和闪烁在GPS接收器广泛的纬度。是强烈的,他们的签名阿拉哈巴德勒克瑙。经向风估计使用两个ionosondes建议朝赤道方向的重力波~ 2 h。抑制期异常峰值在随后一天的风暴显示的复杂作用干扰发电机电场和扰动风效果。结果还显示一个有趣的特性旅行电离层扰动可能与扰动经向风在复苏阶段。观测是夜间西纬向漂移和PRE-related总电子含量增强在异常波峰的主要阶段在复苏和计数器电喷流签名阶段。

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