首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Polar cap size during 14–16 July 2000 (Bastille Day) solar coronal mass ejection event: MHD modeling and satellite imager observations
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Polar cap size during 14–16 July 2000 (Bastille Day) solar coronal mass ejection event: MHD modeling and satellite imager observations

机译:2000年7月14日至16日(巴士底日)太阳日冕大规模抛射事件中的极帽尺寸:MHD建模和卫星成像仪观测

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This study investigates the development of the polar cap area as simulated by global magnetohydrodynamic models of the Earth's magnetosphere during the 14–16 July 2000 (Bastille Day) event. Around 1440 UT on 15 July, a magnetic cloud hit the magnetosphere and in the following hours high levels of activity in the magnetosphere and ionosphere were driven by the frequent changes in solar wind conditions. We compare the size of the polar cap (region of open magnetic field lines) as computed with two MHD models (UCLA-GGCM and BATSRUS) with observation data obtained from the IMAGE and Polar satellites. The two models in general reproduce the changes of the polar cap size that are seen by the satellite imagers. The range of modeled polar cap sizes, however, is limited to about 50–80% of the size range seen by the imagers and the shapes of the polar caps sometimes differ considerably among the models and compared to the observations. We found that a smoothing of solar wind parameters occurs, suggesting that solar wind inputs are stored in the magnetospheric system over a certain “memory” timescale. Cross-correlations are computed between smoothed solar wind input and the time history of the resulting polar cap size. Modeled magnetospheric “memory” timescales are estimated to be less than 12 min, whereas the satellite image data suggest a timescale of more than 20 min.
机译:这项研究调查了在2000年7月14日至16日(巴士底日)事件中,地球磁层的整体磁流体动力学模型所模拟的极帽区域的发展。在7月15日左右UT 1440左右,磁云击中了磁层,在随后的几个小时中,由于太阳风条件的频繁变化,磁层和电离层中的高水平活动被驱使。我们将两个MHD模型(UCLA-GGCM和BATSRUS)计算出的极帽(开放磁场线区域)的大小与从IMAGE和Polar卫星获得的观测数据进行比较。通常,这两个模型再现了卫星成像仪看到的极帽尺寸的变化。但是,建模的极帽尺寸范围被限制在成像仪看到的尺寸范围的50-80%左右,极帽的形状有时在模型之间也存在很大差异,并且与观测结果相比有很大差异。我们发现对太阳风参数进行了平滑处理,这表明太阳风输入在一定的“内存”时间范围内存储在磁层系统中。互相关是在平滑的太阳风输入和所得极帽尺寸的时间历程之间计算的。建模的磁层“记忆”时标估计少于12分钟,而卫星图像数据表明时标超过20分钟。

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