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首页> 外文期刊>Astronomy reports >Observation of a coronal mass ejection in January 1997 using radio sounding of the near-solar plasma with the GALILEO spacecraft
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Observation of a coronal mass ejection in January 1997 using radio sounding of the near-solar plasma with the GALILEO spacecraft

机译:使用GALILEO航天器在1997年1月使用近太阳等离子体的无线电探测对日冕物质的喷射

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Measurements of frequency fluctuations in radio signals generated by the GALILEO spacecraft from January 6 to 11, 1997 are presented and analyzed. The passage of a coronal mass ejection observed by the SOHO/LASCO coronagraph on January 6, 1997 through the radio-communication path between the spacecraft and a ground station was recorded. Radio sounding was carried out at a carrier frequency of 2295 MHz at a heliocentric distance of about 32 solar radii, with the signal being received at three ground stations. As the mass ejection intersected the propagation path, the mean frequency of the signal increased and several-hour-long frequency fluctuations were enhanced. A spectral analysis of the frequency fluctuations shows that the regime and level of plasma turbulence are substantially different in different sections of the quiet solar wind and the disturbed plasmoid. A correlation between the intensity and temporal spectrum of the frequency fluctuations is found. The plasma density in the leading part of the coronal mass ejection exceeds the mean background value by more than an order of magnitude. Our correlation analysis of the frequency fluctuations recorded simultaneously at two widely separated measuring points shows that two flow components with different velocities-the quiet solar wind and a perturbed stream-crossed the communication path. The radio-sounding data are compared with observations of the coronal mass ejection by the SOHO/LASCO coronagraph and plasma measurements near the Earth's orbit using the WIND satellite. A pronounced correlation is found between the variations in the mean frequency of the sounding signal and the plasma density in near-Earth space.
机译:介绍并分析了GALILEO航天器从1997年1月6日至11日产生的无线电信号的频率波动测量值。记录了由SOHO / LASCO日冕仪于1997年1月6日通过航天器与地面站之间的无线电通信路径观测到的日冕物质抛射的过程。在2295 MHz的载频上以约32太阳半径的日心距进行无线电探测,并在三个地面站接收信号。当大量喷射与传播路径相交时,信号的平均频率增加,并且长达数小时的频率波动增加。频率波动的频谱分析表明,在安静的太阳风和受干扰的等离子体中,不同区域的等离子体湍流的状态和水平有很大不同。发现频率波动的强度和时间频谱之间的相关性。冠状物质喷射的前部部分的血浆密度超过平均背景值一个数量级以上。我们对在两个相距很远的测量点同时记录的频率波动的相关性分析表明,速度不同的两个流动分量-安静的太阳风和扰动的水流穿过通信路径。无线电数据与SOHO / LASCO日冕仪观测到的冠状物质喷射以及使用WIND卫星对地球轨道附近的等离子体测量结果进行了比较。在探测信号的平均频率变化与近地空间中的等离子体密度之间发现了明显的相关性。

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