地震前地磁场强度的多重分形去趋势波动分析(Mf-Dfa)及异常

T. Chetia, S. Baruah, Chandan Dey, S. Baruah, Sangeeta Sharma
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摘要

本文报道了Mw 5.5 Kokrajhar事件前地磁总场强(B total)的异常。多重分形分析揭示了地磁总场强时间序列的潜在动力学。通过研究事件发生当天(T event day)及其代理(T surrogate)的多重分形谱,了解B Total时间序列中隐藏的行为和动态。多重分形谱在第T天(事件前一天的多重分形谱)和第T天之间有显著变化。我们还观察到,事件发生时(事件第T天)B Total的多重分形强于事件第T天的多重分形,来源于低值分布。T Day 1和T Event Day时间序列的多重分形不是来自源型长程相关,也不是来自广义概率密度函数。调查还显示出一些非线性特征,这可能证明异常是地震引起的。文章中详细地强调了这些观察结果。研究了地磁场强度时间序列的潜在动力学,用于地震前兆和预报研究。
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The Multifractal Detrended Fluctuation Analysis (Mf-Dfa) and Anomalies in Geomagnetic Total Field Intensity Prior To Mw~5.5 Earthquake
In the research article, we report the anomalies observed in geomagnetic total field intensity (B Total ) prior to Mw 5.5 Kokrajhar event. The multifractal analysis was scrutinized to reveal the underlying dynamics in the Geomagnetic Total field intensity time series. The multifractal spectrum on the day when the event occurred (T Event day ) and its surrogate (T Surrogate ) was investigated to understand the behavior and dynamics hidden in B Total time series. A significant variation in the multifractal spectrum was observed between T Day one (multifractal spectrum a day prior to the event) and T Event day . It was also observed that the mulfractality of B Total when the event occurred (T Event day ) got stronger than the multifractality of T Day one and was sourced from low values distribution. The multifractality in T Day one and T Event day time series was not from source type long range correlation or sourced from broad probability density function. The investigation also manifests some nonlinear features which probably evinces the anomalies to be seismic induced. The observations are elaborately emphasized in the article. The study scrutinizes the underlying dynamics in geomagnetic field intensity time series for earthquake precursory and forecast studies.
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