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The strength and hemispheric asymmetry of Equatorial Ionization Anomaly during two geomagnetic storms in 2013 from Global Ionosphere Map and SAMI2

机译:全球电离层图和SAMI2在2013年的两次地磁风暴中赤道电离异常的强度和半球不对称性

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The variations of the strength and the hemispheric asymmetry of EIA were studied by Global Ionosphere Map (GIM) and SAMI2 during two geomagnetic storm periods in March and June 2013. Compared with the 30-days median TEC, the TEC at the two crests of EIA had small variations while the TEC at the trough had a more remarkable variation for the two storms after the SSC. The TEC difference between the two EIA peaks had an increase or decrease several hours after the SSC, the asymmetry between the two crests of EIA represented by the defined asymmetry index has no obvious variations except several hours after the SSC, and EIA strength represented by the Crest-to-Trough Ratio (CTR) had a remarkable increase one day after the SSC day for March storm and decrease several hours after the SSC for June storm. The variations last several hours, with more than 40% variations compared with the value during the quiet period. The EIA peaks were also found to move toward the equator after the SSC during the two storms. The simulation from SAMI2 and HWM07 also shows that EIA crests would move toward the equator during storm time and EIA strength would decrease, which suggests that the disturbed neutral wind and disturbed electric field may be important factors affecting the EIA during the storm periods. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在2013年3月和2013年6月的两个地磁风暴期间,通过全球电离层图(GIM)和SAMI2研究了EIA的强度和半球不对称性的变化。与30天中值TEC相比,EIA的两个波峰处的TEC均值SSC之后的两次风暴,波谷的TEC变化很小,而波谷的TEC变化更明显。在SSC几个小时后,两个EIA峰之间的TEC差异增加或减小,除SSC几个小时后,由定义的不对称指数表示的EIA的两个波峰之间的不对称性没有明显变化,而EIA强度由SSC表示了几个小时。波峰与波谷之比(CTR)在3月风暴的SSC一天后的第一天显着增加,而在6月风暴的SSC几小时后的峰值却降低了。变化持续几个小时,与安静期间的变化相比,变化超过40%。在两次风暴中,SSC之后,EIA峰也向赤道移动。 SAMI2和HWM07的模拟还表明,在风暴期间,EIA波峰会移向赤道,EIA强度会降低,这表明受干扰的中性风和电场可能是影响风暴期间EIA的重要因素。 (C)2016 Elsevier Ltd.保留所有权利。

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