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Potential reasons for ionospheric anomalies detected by nonlinear principal component analysis just before the China Wenchuan earthquake, and their relationship to source conditions

机译:非线性主成分分析在中国汶川地震之前检测到电离层异常的潜在原因及其与源条件的关系

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摘要

Nonlinear principal component analysis (NLPCA) was performed to examine the total electron content (TEC) anomalies for the China Wenchuan earthquake of May 12, 2008 (= 7.9). This was applied to global ionospheric maps (GIMs) at heights from 150 km to 450 km, with the transforms conducted for the time period 00:00 to 06:00 UT on May 12, 2008. The earthquake occurred at 06:28 UT. The GIMs were analyzed by PCA and NLPCA, whereby they were separated into 100 smaller maps of 36° in longitude and 18° in latitude. These smaller maps are constructed at 71 × 71 pixels, which forms the transform matrix for NLPCA. The transform allows a principal eigenvalue to be assigned for each of the smaller maps. The results of the transforms provide 100 principal eigenvalues that cover the region, which includes the epicenter of the Wenchuan earthquake. The possibility of TEC anomalies caused by X-ray fluxes and geomagnetic activity is eliminated by reviewing X-ray flux data and the Kp index. The eigenvalues of NLPCA are compared with those of PCA. TEC anomalies were clearly detected using NLPCA, with large principal eigenvalues that represent earthquake-related TEC anomalies near the epicenter for the time period 00:00-0600 UT. The results of this study are discussed in terms of the potential causes of these TEC anomalies, especially for the time period 02:00-04:00 UT, when rocks around the epicenter were potentially subjected to a rapid increase in stress, which might have induced very pronounced p-type semiconductor effects. These effects will probably have been present for the other time periods, but might not have been so pronounced.
机译:进行非线性主成分分析(NLPCA)来检查电子总含量(TEC)为异常5月12日,(= 7.9)的中国汶川地震。将其在高度应用于全球电离层映射(的GIMs)从150公里至450公里,该变换的时间段进行00:00至06:00 UT 5月12日,2008年在地震发生的6点28 UT。所述的GIMs通过PCA和NLPCA,由此它们被分成的36°经度100张较小的地图和在北纬18°进行分析。这些较小的地图是在71×71像素,其形式变换矩阵为NLPCA构成。变换允许被分配用于每个较小的地图的主本征值。该变换的结果提供了覆盖区域,其中包括汶川地震的震中100个主要特征值。引起的X射线通量和地磁活动TEC异常的可能性通过审查X射线通量数据和Kp的索引消除。 NLPCA的特征值与PCA相比。 00-0600 UT:使用NLPCA,与代表震中附近的地震有关的异常现象TEC的时间段00大主要特征值TEC异常清晰地探测到。这项研究的结果在这些TEC异常的可能原因进行了讨论,特别是对于该时间段02:00-04:00 UT,当震中周围岩石可能经受压力的迅速增加,这可能有诱导的非常显着的p型半导体的效果。这些效应可能已经存在的其他时间段,但可能还没有那么明显。

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    Jyh-Woei Lin;

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  • 年度 2012
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  • 原文格式 PDF
  • 正文语种 eng
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