首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Reply to comment by U. Villante and M. Piersanti on 'Statistical analysis of geosynchronous magnetic field perturbations near midnight during sudden commencements'
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Reply to comment by U. Villante and M. Piersanti on 'Statistical analysis of geosynchronous magnetic field perturbations near midnight during sudden commencements'

机译:由美国Villante和m . Piersanti回复置评在“同步的统计分析午夜在附近的磁场扰动一开始"

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We thank Villante and Piersanti [2015 hereinafter referred to as VP] for their comments on our recent paper Park et al. [2014, hereinafter referred to as P14]. The main comment in VP is that geosynchronous magnetic field perturbations near midnight during sudden commencement (SC) can be explained by different combinations of the hinging point distance and current sheet thickness. We basically agree with VP. However, we have question as to whether all SC-associated magnetic field perturbations observed at geosynchronous orbit near midnight can be explained by empirical models developed by Tsyganenko [2002a, 2002b, referred to as T01] in VP and developed by Tsyganenko and Sitnov [2005, referred to as TS05] in P14. It should be noted that T01 and TS05 are not time-dependent models. This indicates that the magnetic field strength and magnetic field vectors of strongly disturbed magnetic field perturbations, which is caused by the passage of interplanetary shock over the Earth's magnetosphere, during a typical SC interval less than ~15 min cannot be easily estimated from both T01 and TS05 models. The models do not provide the distance of the hinging point from Earth and current sheet thickness in the magnetotail as a function of the solar wind dynamic pressure during the SC interval. In particular, the location where the SC-associated current establishes has not been provided from the models. This is a reason that we do not make a quantitative examination whether the SC observation at geosynchronous orbit is consistent with the model field variation (see Figures 7 and 8 in P14).
机译:我们感谢Villante Piersanti[2015以下称为评论我们的副总裁)最近的一篇论文公园et al。(2014年,以下称为好)。同步轨道磁场扰动接近午夜时突然开始(SC)用不同的组合加以解释要点距离和当前表厚度。我们所有SC-associated是否有问题磁场扰动观察到地球同步轨道接近午夜用经验来解释模型开发的Tsyganenko [2002 a, 2002 b,称为T01]副总裁和由Tsyganenko Sitnov [2005,称为TS05]好。T01及TS05不是时间模型。这表明,磁场强度和磁场矢量的强烈干扰磁场扰动,引起的段落的行星际激波地球的磁气圈,在一个典型的SC间隔不到~ 15分钟不容易估计T01和TS05模型。模型没有提供明确的距离点从地球和当前薄板厚度磁尾的太阳风的函数动压在SC区间。SC-associated的位置当前建立尚未提供的模型。定量检查是否SC观察在地球同步轨道是一致的与模型领域的变化(见图7和图在好8)。

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