首页> 外文期刊>Annales Geophysicae >Outer Van Allen belt trapped and precipitating electron flux responses to two interplanetary magnetic clouds of opposite polarity
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Outer Van Allen belt trapped and precipitating electron flux responses to two interplanetary magnetic clouds of opposite polarity

机译:外文艾伦带捕获和沉淀电子通量对两个相反极性的两际磁云响应

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Recently, it has been established that interplanetary coronal mass ejections (ICMEs) can dramatically affect both trapped electron fluxes in the outer radiation belt and precipitating electron fluxes lost from the belt into the atmosphere. Precipitating electron fluxes and energies can vary over a range of timescales during these events. These variations depend on the initial energy and location of the electron population and the ICME characteristics and structures. One important factor controlling electron dynamics is the magnetic field orientation within the ejecta that is an integral part of the ICME. In this study, we examine Van Allen Probes (RBSPs) and Polar Orbiting Environmental Satellites (POESs) data to explore trapped and precipitating electron fluxes during two ICMEs. The ejecta in the selected ICMEs have magnetic cloud characteristics that exhibit the opposite sense of the rotation of the north–south magnetic field component (BZ). RBSP data are used to study trapped electron fluxes in situ, while POES data are used for electron fluxes precipitating into the upper atmosphere. The trapped and precipitating electron fluxes are qualitatively analysed to understand their variation in relation to each other and to the magnetic cloud rotation during these events. Inner magnetospheric wave activity was also estimated using RBSP and Geostationary Operational Environmental Satellite (GOES) data. In each event, the largest changes in the location and magnitude of both the trapped and precipitating electron fluxes occurred during the southward portion of the magnetic cloud. Significant changes also occurred during the end of the sheath and at the sheath–ejecta boundary for the cloud with south to north magnetic field rotation, while the ICME with north to south rotation had significant changes at the end boundary of the cloud. The sense of rotation of BZ and its profile also clearly affects the coherence of the trapped and/or precipitating flux changes, timing of variations with respect to the ICME structures, and flux magnitude of different electron populations. The differing electron responses could therefore imply partly different dominant acceleration mechanisms acting on the outer radiation belt electron populations as a result of opposite magnetic cloud rotation.
机译:最近,已经确定了截然冠状物质射出(ICMES)可以显着影响外辐射带中的被捕获的电子助熔剂,并沉淀从带中损失的电子势孔进入大气中。在这些事件期间,沉淀的电子助焊剂和能量可以在一系列时间尺寸变化。这些变化取决于电子群的初始能量和位置和ICME特性和结构。控制电子动力学的一个重要因素是喷射内的磁场取向,其是ICME的一个组成部分。在这项研究中,我们检查范艾伦探针(RBSPS)和极性轨道环境卫星(POOS)数据,以在两个ICMES期间探索被困和沉淀的电子助熔剂。所选ICME中的喷射物具有磁性云特性,其表现出南北磁场分量(BZ)旋转的相反感。 RBSP数据用于研究捕获的电子通量,而PoES数据用于沉淀到高大气中的电子助熔剂。定性地分析捕获和沉淀的电子助熔剂以在这些事件期间了解它们相对于彼此的变化以及磁云旋转。使用RBSP和地球静止操作环境卫星(GOUSE)数据也估计内磁体波活性。在每个事件中,在磁性云的向南部分期间发生截图和沉淀电子磁通量的位置和幅度的最大变化。在鞘的末端和南部云覆盖到北磁场旋转时也发生了显着变化,而北方的ICME在云的最终边界处具有显着的变化。 BZ的旋转感及其轮廓也清楚地影响了捕获和/或沉淀的通量变化的相干性,相对于ICME结构的变化的时间和不同电子群体的通量大小。因此,不同的电子响应可能意味着由于相反的磁云旋转而构成作用在外辐射带电子群的主要显性加速机制。

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