Research Article  Open Access
Application of AR Model in the Analysis of Preearthquake Ionospheric Anomalies
Abstract
Earthquake ionosphere coupling phenomenon is one of the hot research topics using the Global Positioning System (GPS). Taking Lushan earthquake in April 2013 as an example, this paper firstly establishes ionosphere TEC models and determines the optimal model based on Autoregression model by analyzing the TEC values of the epicenter area detected by GPS. Then it makes predictions about the ionosphere data, obtains the background value, and conducts anomaly analysis by using the optimal model. Finally the correlation between ionosphere anomalies and earthquake is analyzed quantitatively by presenting data diagrams explicitly; then a new method to do shortterm and imminent earthquake prediction is proposed in the end.
1. Introduction
An earthquake, as a result of a sudden release of energy in the Earth’s crust that creates seismic waves, is one of the major natural disasters which may cause huge property damage and casualties. Sichuan is one of earthquakeprone areas of China, where Wenchuan 8.0 earthquake took place. Until 12:00 on September 18, 2008, the earthquake resulted in 69,227 deaths, 374,643 being injured, and 17,923 being missing, and the latest strong earthquake Lushan 7.0 earthquake resulted in 1.52 million victims as well as a damaged area of 12,500 square kilometers. According to the website of China Seismological Bureau, until 14:30 on April 24, 2013, the earthquake caused a total of 196 deaths, 21 people missing, and 11,470 people injured. Earthquake prediction and forecasting, especially shortPro forecasting, are still in the exploratory stage [1]. In order to advance earthquake prediction research, many scientists continue to explore new methods of seismic monitoring, and the relationship between the earthquake gestation period ionospheric disturbances and seismic coupling has become a hot topic [2]. Leonard and Barnes firstly discovered the coupling relationship between earthquakes and ionospheric when they observed the ionospheric anomaly in the foreshock of Alaska earthquake [3]. Liu et al. in Taiwan’s National Central University did a survey about ionospheric anomalies in earthquakes of magnitude > 6 during the period 1994 to 1999, which showed that 1–6 days prior to the earthquake ionosphere f0F2 decreased significantly in value at local time 12:00–17:00 compared with the value 15 days before the earthquake and they regard this phenomenon as an earthquake precursory to predict earthquake [4].
Traditional methods usually study the ionosphere by using ionospheric altimeter. Currently there are about 200 ionosphere altimeters distributed around the world, but only a few are running [4]. With the development of GNSS technology, especially the indepth study of GPS technology, the use of dualfrequency GPS observation techniques solver ionospheric delay to obtain ionospheric total electron density (Total Electron Content, TEC) technology matures. Thousands of groundbased GPS receiving stations that are distributed all over the world improve the TEC spatial and temporal resolution, which will be more conducive to the sustained simulation research of the distribution and exception analysis of the ionosphere.
Currently, the main methods of ionospheric anomalies coupling studies include quartile method and sliding window method. Xinzhou recently proposed a preseismic ionospheric anomaly detection using time series method. The above methods all detect by selecting a normal period of time or a period of TEC value as the background without explaining the reasons for selecting the time window. The scale and change of the ionosphere, affected by crustal movements and solar activity, are periodic and certain. Therefore, adopting time series method (ARMA model) can better take into account the uncertainty components and be able to calculate changes in the ionosphere TEC uncertainty [5].
2. Principle of AR Model
Autoregression model (AR model) is a method of processing statistical time series and making predictions about values of variables currently and afterwards based on the value of the same variable at different stages. The formula iswhere is the autoregressive order and is the constant term. To establish Autoregression model, we should reasonably determine its order firstly which can be normally set within a range of the order, then make a parameter estimation within the scope of the various model, and test the significance of the parameters. Finally determine the order by using fixedorder criteria. We use the linear hypothesis method for model order. The principle is as follows: observational data set (), first set of order , establish Autoregression model,
Then consider model, , obtain order model, and obtain the model parameter estimation and residual sum of squares, denoted , . Assuming linear method.
The formula isSuppose is true; distribution can be used for statistics:Select significant level , molecular degrees of freedom for 1, and denominator degrees of freedom ; look up table ; if , then is not established, . Since there are significant differences between order and order model, order should be used. Otherwise ; then accept . It means order and order model have no significant difference; then order should be used [6].
3. The Establishment of AR Model
Autoregression model in the study of ionospheric anomalies needed no more information, but it must comply with the following two conditions.(1)It must be autocorrelated; if autocorrelation coefficient () is less than 0.5, then it should not be used to predict the results which will be highly inaccurate.(2)Autoregression model only applies to the forecast and its earlyrelated phenomenon, which is influenced by its own historical factors [6].
For these reasons, the paper must first verify Lushan ionospheric electron content relevance, that is, different trends within the same month of the year whether converge. In probability theory and statistics, correlation (correlation, also known as the correlation coefficient or correlation coefficient) shows the strength and direction of the linear relationship between two random variables. Therefore, the correlation efficient may be used to determine whether they converge. Specific experiments are as follows: by using the TEC data in March 2011, March 2012, and March 2013, the TEC data prior to Lushan earthquake can be obtained with the interpolation method. The correlation coefficient can be calculated with the TEC data in March 2011 data and March 2012 and March 2013, respectively. The formula is as follows:
When for low linear correlation, when correlation coefficient is calculated using the interpolated data shown in Table 1 with March 2011 data.

As can be seen from Table 1, the same month in different years TEC has a very high correlation, Lushan local ionosphere can be determined with different years, and TEC in March has a great similarity. The correlation between TEC in March 2012 and that in March 2013 is up to 0.925. Figure 1 shows the time series of TEC Lushan three years of observations, Figure 2 Lushan March 2011 and March 2013 TEC time series of observations, and Figure 3 Lushan March 2012 and March 2013 TEC time series of observations.
The Autoregression model data is eventually based on the TEC observation data in March 2012 according to the correlation analysis. By doing the regression analysis of the TEC data in March 2012, we get the following results.
Autoregression model is as follows:
Autoregression model is as follows:
Autoregression model is as follows:
The predicted value of TEC in March 2013 is obtained by using the 16step model equations and then we compare it with the actual value. is calculated by the sum of error square formula:
Inside the formula is the predicted value, TEC is actual value, and is the sum of error square. The results are shown in Table 2. Figure 4 shows the sum of error square trends, and Figure 5 presents the trends.

Figure 4 shows that the sum of error square decreases with the increase of the order, but the significant difference exists only when by comparing the data in Figures 4 and 5, according to hypothesis testing formulas and molecular dof 1, denominator dof ∞, and degree of confidence , checking distribution table . So we determine the Autoregression model of order 8 as the optimal model:
4. Analysis of Ionospheric Anomalies of Lushan Earthquake
The predicted value is calculated based on formula (10) and 2013 TEC observations 3 months ago. And standard deviation is obtained as follows: so .
TEC values in April are predicted based on . The results are shown in Figure 6.
Take the upper and lower boundaries:
By comparing the predicted value in April and the actual value in April 2013, we obtain the results in Figure 7.
Based on the above analysis of the ionosphere anomaly formulas, we can further analyze the difference between TEC predicted values and actual values in Lushan regions.
5. Conclusions
Using autoregressive model to make predictions and do anomaly analysis of Lushan earthquakes ionosphere, we can draw the following conclusions.(1)Since April 6th, 2013, the ionospheric TEC over the epicenter displays obvious anomalies with little disturbance by space weather. Therefore it can be inferred that they are caused by the coming earthquake and there is duration of 9 days. This is consistent with the Wu Yun’s results which showed 10 days before the 3 big earthquakes in Asia; ionospheric TEC over the epicenter and its vicinities displays obvious abnormal disturbances. Here the first TEC abnormal changes appeared about 14 days prior to the seismic event.(2)On April 13th 2013, the abnormal disturbances (TEC) of ionosphere appear and abnormal value reached 18 TECu with longitude span of 25° and latitude span of 5° in the spatial distribution of anomalies. Abnormal peak is located near the epicenter near the equator. The ionospheric abnormities 7 days before the main shock are indeed related to the preparation process of Lushan earthquake.
Based on the above analysis, we can draw the conclusion that model can be applied effectively to establish model with the optimal background data to analyze preearthquake ionospheric anomalies.
Conflict of Interests
The authors declare that there is no conflict of interests regarding the publication of this paper.
Acknowledgments
This paper is financially supported by Natural Science Foundation of China (Grant no. 51174170) and National Science and Technology Major Project of China under Grant no. 2011ZX05013006.
References
 Z. Fuying, W. Yun, and L. Jian, “Before the Wenchuan 8.0 earthquake ionospheric TEC anomaly analysis,” Geodesy and Geodynamics, vol. 28, no. 6, pp. 16–21, 2008. View at: Google Scholar
 R. S. Leonard and R. A. Barnes, “Observation of ionospheric disturbances following the Alaska earthquake,” Journal of Geophysical Research, vol. 70, no. 5, pp. 1250–1253, 1965. View at: Publisher Site  Google Scholar
 P. F. Weaver, P. C. Yuen, G. W. Prolss, and A. S. Furumoto, “Acoustic coupling into the ionosphere from seismic waves of the earthquake at Kurile Islands on August 11, 1969,” Nature, vol. 226, no. 5252, pp. 1239–1241, 1970. View at: Publisher Site  Google Scholar
 J. Y. Liu, Y. J. Chuo, S. J. Shan et al., “Preearthquake ionospheric anomalies registered by continuous GPS TEC measurements,” Annales Geophysicae, vol. 22, no. 5, pp. 1585–1593, 2004. View at: Publisher Site  Google Scholar
 W. Xinzhou, Higher Surveying Adjustment, Surveying and Mapping Press, Beijing, China, 2006.
 W. Yun, Q. Xuejun, and Z. Yiyan, “Before the earthquake detection using groundbased GPS ionospheric TEC anomalies,” Geodesy and Geodynamics, no. 2, pp. 36–40, 2005. View at: Google Scholar
Copyright
Copyright © 2015 Xiaojun Dai et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.