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Expected in Situ Velocities from a Hierarchical Model for Expanding Interplanetary Coronal Mass Ejections

机译:扩展行星际冠状物质抛射的分层模型的预期原位速度

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In situ data provide only a one-dimensional sample of the plasma velocity along the spacecraft trajectory crossing an interplanetary coronal mass ejection (ICME). Then, to understand the dynamics of ICMEs it is necessary to consider some models to describe it. We derive a series of equations in a hierarchical order, from more general to more specific cases, to provide a general theoretical basis for the interpretation of in situ observations, extending and generalizing previous studies. The main hypothesis is a self-similar expansion, but with the freedom of possible different expansion rates in three orthogonal directions. The most detailed application of the equations is though for a subset of ICMEs, magnetic clouds (MCs), where a magnetic flux rope can be identified. The main conclusions are the following ones. First, we obtain theoretical expressions showing that the observed velocity gradient within an ICME is not a direct characteristic of its expansion, but that it depends also on other physical quantities such as its global velocity and acceleration. The derived equations quantify these dependencies for the three components of the velocity. Second, using three different types of data we show that the global acceleration of ICMEs has, at most, a small contribution to the in situ measurements of the velocity. This eliminates practically one contribution to the observed velocity gradient within ICMEs. Third, we provide a method to quantify the expansion rate from velocity data. We apply it to a set of 26 MCs observed by Wind or ACE spacecrafts. They are typical MCs, and their main physical parameters cover the typical range observed in MCs in previous statistical studies. Though the velocity difference between their front and back includes a broad range of values, we find a narrow range for the determined dimensionless expansion rate. This implies that MCs are expanding at a comparable rate, independently of their size or field strength, despite very different magnitudes in their velocity profiles. Furthermore, the equations derived provide a base to further analyze the dynamics of MCs/ICMEs.
机译:原位数据仅提供沿穿越行星际冠状物质抛射(ICME)的航天器轨迹的等离子体速度的一维样本。然后,要了解ICME的动态,有必要考虑一些模型来描述它。我们从更一般的情况到更具体的情况,按等级顺序导出一系列方程式,从而为解释原位观测,扩展和概括以前的研究提供了一般的理论基础。主要假设是自相似展开,但在三个正交方向上具有可能不同的展开速率的自由。该方程式的最详细的应用不过是ICME的子集,即磁云(MC),可以在其中识别出磁通量绳。主要结论如下。首先,我们获得理论表达式,表明在ICME内观察到的速度梯度不是其扩展的直接特征,而是还取决于其他物理量,例如其整体速度和加速度。导出的方程式对速度的三个分量量化了这些依赖性。其次,使用三种不同类型的数据,我们表明ICME的整体加速度最多对速度的原位测量贡献很小。这实际上消除了对ICME中观测到的速度梯度的一种贡献。第三,我们提供了一种从速度数据中量化膨胀率的方法。我们将其应用于由Wind或ACE航天器观测到的26个MC。它们是典型的MC,其主要物理参数涵盖了先前统计研究中在MC中观察到的典型范围。尽管它们的前后速度差包括较大范围的值,但对于确定的无因次膨胀率,我们发现范围较小。这表明,尽管速度分布的大小差异很大,MC仍以可比的速度扩展,而与它们的大小或场强无关。此外,推导的方程式为进一步分析MC / ICME的动力学提供了基础。

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