首页> 美国政府科技报告 >Ground-Based Radar Detection of the Inner Boundary of the Ion Plasma Sheet and its Response to the Changes in the Interplanetary Magnetic Field.
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Ground-Based Radar Detection of the Inner Boundary of the Ion Plasma Sheet and its Response to the Changes in the Interplanetary Magnetic Field.

机译:离子等离子体片内边界的地基雷达检测及其对行星际磁场变化的响应。

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SuperDARN is an array of HF radars, which covers most of the northern and southern high-latitude regions. The primary goal of this array is to study the dynamics of the large-scale convection pattern in order to understand the Solar wind - Magnetosphere - Ionosphere coupling (SW-M-I). Wide area coverage made it possible to detect some of the proxies for the magnetospheric land marks and boundaries on a global scale and shed some light on the on the some of the fundamental problems in the SW-M-I coupling process. One discovery is that SuperDARN radar E region backscatter boundary in the dusk- midnight sector can be used as a proxy for the inner boundary of the ion plasma sheet. This made it possible to study the boundary dynamics on a more global scale. The boundary undergoes seasonal, diurnal, and substorm associated variations. One question in the SW-M-I coupling research is how fast Magnetosphere-Ionosphere system reacts to the changes in the Interplanetary Magnetic Field (IMF). There are two schools of thoughts on changes in ionospheric convection one being instantaneous and the other being delayed response. We present a study of the response of the equatorward boundary of the ion auroral oval on a global scale to the changes in the IMF. We have used the wide area coverage of the SuperDARN radar to investigate the response of the boundary to the changes in the upstream IMF. Estimation of the delay from the changes in the solar wind and IMF from an upstream satellite to the ionosphere is sometimes ambiguous. To avoid this ambiguity we have also used the changes in the central polar cap convection related to the changes in the IMF. This method helps to test the hypothesis of the fast and or slow changes. We will also compare the response of the ion auroral oval and the open/closed field line boundary to better understand the sequence of response from the changes in IMF.

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