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Possible Ionospheric Electromagnetic Perturbations Induced by the Ms7.1 Yushu Earthquake

机译:玉树Ms7.1地震可能引起的电离层电磁扰动

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摘要

The power spectrum density (PSD) of magnetic field in the ELF/VLF band recorded by the experiment IMSC onboard the DEMETER satellite were used to study the Ms7. 1 Yushu earthquake taking place on April 13, 2010 in China. The results indicate that possible ionospheric electromagnetic perturbations occurring 4 days before the earthquake in the frequency range [370-897 Hz]. Along the orbit 30880_up, which passed over the epicenter area on 9 April, enhanced PSD value of magnetic field at 410 Hz was detected both over the epicentral area and its conjugate point in the southern hemisphere. While on revisited orbits during other days (before and after the earthquake) the magnetic field spectra remained at a relatively low level. In order to be sure that the electromagnetic disturbances were induced by this Yushu earthquake, relative variations of the magnetic field in the ELF/VLF range [370-897 Hz] were calculated and compared with the normal background during 3 years (2007, 2008 and 2009) in the time interval from Jan. 1st to Apr. 30 and in the area [23°N-43°N, 86°E-106°E]. The results show that the normal level of magnetic field in this area is relatively low (~10 ~(-7) nT ~2/Hz), but a large increase occurred from Apr. 1st to Apr. 14 which exceeds 5σ _b. After the earthquake, the magnetic field in the ELF/VLF range gradually decreased. In order to exclude the influence of geomagnetic field activity, we selected only the data recorded during magnetically quiet local night-times. In addition, artificial noises were also removed from the dataset used in the present paper. Therefore the observed perturbations were independent of geomagnetic field disturbances, and might be attributed to seismic activity.
机译:由DEMETER卫星上的实验IMSC记录的ELF / VLF频带中磁场的功率谱密度(PSD)用于研究Ms7。 2010年4月13日,中国发生了1宗玉树地震。结果表明,在地震发生前4天,在[370-897 Hz]频率范围内可能发生了电离层电磁扰动。沿着4月9日越过震中区域的30880_up轨道,在南半球的震中区域及其共轭点都检测到410 Hz磁场的增强PSD值。在其他几天(地震前后)在重新访问的轨道上时,磁场频谱保持在较低水平。为了确保此玉树地震引起电磁干扰,计算了三年(2007年,2008年和2007年)在ELF / VLF范围[370-897 Hz]中磁场的相对变化并将其与正常背景进行比较。 2009年)从1月1日至4月30日的时间间隔以及[23°N-43°N,86°E-106°E]区域。结果表明,该区域的正常磁场水平较低(〜10〜(-7)nT〜2 / Hz),但从4月1日到4月14日发生了很大的增加,超过了5σ_b。地震后,ELF / VLF范围内的磁场逐渐减小。为了排除地磁场活动的影响,我们只选择了在当地磁场安静的夜间记录的数据。此外,还从本文使用的数据集中删除了人工噪声。因此,所观察到的扰动与地磁场干扰无关,并且可能归因于地震活动。

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