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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Faculty of Mathematics and Physics, Charles University, Prague, Czech RepubliNew observations of electromagnetic harmonic ELF emissions in the ionosphere by the DEMETER satellite during large magnetic storms
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Faculty of Mathematics and Physics, Charles University, Prague, Czech RepubliNew observations of electromagnetic harmonic ELF emissions in the ionosphere by the DEMETER satellite during large magnetic storms

机译:捷克共和国布拉格查尔斯大学数学与物理学院,捷克共和国共和国DEMETER卫星在大磁暴期间对电离层中电磁谐波ELF发射的新观测

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摘要

DEMETER (Detection of Electro-Magnetic Emissions Transmitted from Earthquake Regions) is an ionospheric microsatellite launched on a polar orbit at an altitude of 710 km. Its scientific payload allows to measure electromagnetic waves and plasma parameters. During the strong magnetic storm from 8 to 10 November 2004, intense electromagnetic harmonic emissions between 500 and 2000 Hz have been detected at midlatitudes and similar emissions were also observed on 21–22 January 2005 and on 15 May 2005 during two magnetic storms of lower intensity. They can be observed on consecutive orbits, either in one hemisphere or in both hemispheres at the same L values. On the dynamic energy/time spectrograms that are available in the DEMETER survey modes these emissions appear most often as patches of intensified signals lasting a few tens to hundreds of seconds with a frequency structure showing nearly equally spaced frequency bands. Such a frequency structure could be explained if the waves originate from the generation of Electro-Magnetic Ion Cyclotron (EMIC) waves at proton cyclotron harmonics. When waveforms are available during burst modes, allowing a fine-resolution frequency analysis, these emissions appear in one orbit be composed of a set of lines slowly drifting in frequency with time. During periods with a high magnetically activity, the ionosphere and the magnetosphere are severely disturbed and these waves could be generated at relatively low L values and propagate from their equatorial source region along density gradients down to the altitude of the satellite. Energetic electron data obtained onboard DEMETER indicate that these waves interact with the energetic electron populations.
机译:DEMETER(地震区域传输的电磁辐射检测)是在极地轨道上以710公里的高度发射的电离层微卫星。其科学的有效载荷可以测量电磁波和等离子体参数。在2004年11月8日至10日的强磁风暴中,在中纬度检测到500至2000 Hz的强电磁谐波辐射,在2005年1月21-22日和2005年5月15日的两次低强度磁暴期间也观察到类似的辐射。可以在一个半球或两个半球的相同L值的连续轨道上观测到它们。在DEMETER勘测模式下可用的动态能量/时间频谱图上,这些发射最常以持续几十到几百秒的增强信号斑块出现,其频率结构显示几乎等间隔的频带。如果这些波起源于质子回旋加速器谐波产生的电磁离子回旋加速器(EMIC)波,则可以解释这种频率结构。当在突发模式下可以使用波形时,可以进行精细的频率分析,这些辐射出现在一个轨道上,是由一组频率随时间缓慢漂移的线组成的。在具有高磁活动的期间,电离层和磁层受到严重干扰,这些波可能以相对较低的L值生成,并从它们的赤道源区域沿密度梯度传播到卫星的高度。在DEMETER上获得的高能电子数据表明这些波与高能电子种群相互作用。

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