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Global Ionospheric and Thermospheric Effects of the June 2015 Geomagnetic Disturbances: Multi‐Instrumental Observations and Modeling

机译:2015年6月地磁干扰的全球电离层和热层影响:多仪器观测和建模

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摘要

By using data from multiple instruments, we investigate ionospheric/thermospheric behavior during the period from 21 to 23 June 2015, when three interplanetary shocks (IS) of different intensities arrived at Earth. The first IS was registered at 16:45 UT on 21 June and caused ~50 nT increase in the SYM‐H index. The second IS arrived at 5:45 UT on 22 June and induced an enhancement of the auroral/substorm activity that led to rapid increase of thermospheric neutral mass density and ionospheric vertical total electron content at high latitudes. Several hours later, topside electron content and electron density increased at low latitudes on the nightside. The third and much larger IS arrived at 18:30 UT on 22 June and initiated a major geomagnetic storm that lasted for many hours. The storm provoked significant effects in the thermosphere and ionosphere on both dayside and nightside. In the thermosphere, the dayside neutral mass density exceeded the quiet time levels by 300–500%, with stronger effects in the summer hemisphere. In the ionosphere, both positive and negative storm effects were observed on both dayside and nightside. We compared the ionospheric observations with simulations by the coupled Sami3 is Also a Model of the Ionosphere/Rice Convection Model (SAMI3/RCM) model. We find rather good agreement between the data and the model for the first phase of the storm, when the prompt penetration electric field (PPEF) was the principal driver. At the end of the storm main phase, when the ionospheric effects were, most likely, driven by a combination of PPEF and thermospheric winds, the modeling results agree less with the observations.
机译:通过使用多种仪器的数据,我们研究了2015年6月21日至23日期间电离层/热层的行为,当时三种强度不同的行星际激波(IS)到达地球。第一个IS于6月21日世界标准时间16:45注册,并导致SYM‐H指数增加了约50 nT。第二次IS于6月22日5:45 UT到达,并引起了极光/亚暴活动的增强,从而导致高纬度地区的热层中性质量密度和电离层垂直总电子含量迅速增加。几个小时后,夜空低纬度时,顶侧电子含量和电子密度增加。第三个更大的IS于6月22日到达世界标准时间18:30,引发了持续数小时的重大地磁风暴。风暴在白天和夜晚对热层和电离层产生了重大影响。在热层中,白天的中性质量密度超过了安静时间的水平300-500%,在夏季半球中的影响更大。在电离层中,白天和黑夜都观察到正面和负面的风暴影响。我们将电离层的观测结果与耦合的Sami3的模拟进行了比较,这也是电离层/水稻对流模型(SAMI3 / RCM)的模型。当快速穿透电场(PPEF)是主要驱动因素时,我们发现风暴第一阶段的数据与模型之间的一致性很好。在风暴主阶段结束时,当电离层效应最有可能是由PPEF和热层风共同驱动时,模拟结果与观测值的吻合度较低。

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