Global navigation satellite system detection of preseismic ionospheric total electron content anomalies for strong magnitude (Mw>6) Himalayan earthquakes

Abstract. Electron content in the ionosphere is very sensitive to temporary disturbances of the Earth’s magnetosphere (geomagnetic storm), solar flares, and seismic activities. The Global Navigation Satellite System (GNSS)-based total electron content (TEC) measurement has emerged as an important technique for computations of earthquake precursor signals. We examined the pre-earthquake signatures for eight strong magnitude (Mw>6: 6.1 to 7.8) earthquakes with the aid of GNSS-based TEC measurement in the tectonically active Himalayan region using International GNSS Service (IGS) stations as well as local GNSS-based continuously operating reference stations (CORS). The results indicate very significant ionospheric anomalies in the vertical total electron content (vTEC) a few days before the main shock for all of the events. Geomagnetic activities were also studied during the TEC observation window to ascertain their role in ionospheric perturbations. It was also inferred that TEC variation due to low magnitude events could also be monitored if the epicenter lies closer to the GNSS or IGS station. Therefore, the study has confirmed TEC anomalies before major Himalayan earthquakes, thereby making it imperative to set up a much denser network of IGS/CORS for real-time data analysis and forewarning.

[1]  Sergey Pulinets,et al.  Ionospheric Precursors of Earthquakes; Recent Advances in Theory and Practical Applications , 2004 .

[2]  M. Wilson,et al.  The Himalayan leucogranites: Constraints on the nature of their crustal source region and geodynamic setting , 2012 .

[3]  An Yin,et al.  Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation , 2006 .

[4]  B. V. Pai,et al.  Ionospheric Effects on GPS Signal in Low-Latitude Region: A Case Study Review of South East Asia and Africa , 2015 .

[5]  J. Raulin,et al.  Changes in Animal Activity Prior to a Major (M=7) Earthquake in the Peruvian Andes , 2015 .

[6]  D. S. Ramesh,et al.  The devastating Muzaffarabad earthquake of 8 October 2005: New insights into Himalayan seismicity and tectonics , 2006 .

[7]  Shuanggen Jin,et al.  GNSS ionospheric seismology: Recent observation evidences and characteristics , 2015 .

[8]  E. Essex,et al.  Using observations from the GPS and TOPEX satellites to investigate night-time TEC enhancements at mid-latitudes in the southern hemisphere during a low sunspot number period , 2000 .

[9]  Shuanggen Jin,et al.  Pattern and evolution of seismo‐ionospheric disturbances following the 2011 Tohoku earthquakes from GPS observations , 2014 .

[10]  Ljiljana R. Cander,et al.  Total electron content - A key parameterin propagation: measurement and usein ionospheric imaging , 2004 .

[11]  Jaume Sanz,et al.  Combining ionosonde with ground GPS data for electron density estimation , 2003 .

[12]  Shuanggen Jin,et al.  Statistical characteristics of seismo-ionospheric GPS TEC disturbances prior to global Mw ≥ 5.0 earthquakes (1998–2014) , 2015 .

[13]  Jared Hera Ndeda,et al.  Analysis of Longitudinal Advancement of the Peak Total Electron Content in the African Equatorial Anomaly Region Using Data From GPS Receivers and GIS Stations in Kenya , 2014 .

[14]  Julia Ling,et al.  Air ionization at rock surfaces and pre-earthquake signals , 2009 .

[15]  S. Pulinets,et al.  Spatial–Temporal Characteristics of Large Scale Disturbances of Electron Density Observed in the Ionospheric F-Region before Strong Earthquakes , 2003 .

[16]  Yi-Ben Tsai,et al.  Pre-earthquake ionospheric anomalies registered by continuous GPS TEC measurements , 2004 .

[17]  Anthony J. Mannucci,et al.  A global mapping technique for GPS‐derived ionospheric total electron content measurements , 1998 .

[18]  M. Berrocoso,et al.  Detection of ionospheric signatures from GPS-derived total electron content maps , 2014 .

[19]  Shuanggen Jin,et al.  Lower atmospheric anomalies following the 2008 Wenchuan Earthquake observed by GPS measurements , 2011 .

[20]  H. Chen,et al.  Constraints on average Taiwan Reference Moho Discontinuity Model—receiver function analysis using BATS data , 2010 .

[21]  Geoffrey Blewitt,et al.  An Automatic Editing Algorithm for GPS data , 1990 .

[22]  B. Mukhopadhyay Clusters of Moderate Size Earthquakes along Main Central Thrust (MCT) in Himalaya , 2011 .

[23]  I. P. Dobrovolsky,et al.  Estimation of the size of earthquake preparation zones , 1979 .

[24]  Sergey Pulinets,et al.  Seismic activity as a source of the ionospheric variability , 1998 .

[25]  Shuanggen Jin,et al.  Co-seismic ionospheric and deformation signals on the 2008 magnitude 8.0 Wenchuan Earthquake from GPS observations , 2010 .

[26]  F. Freund,et al.  Pre-earthquake signals: Underlying physical processes , 2011 .

[27]  T. Matsuda,et al.  Variation of nitric oxide concentration before the Kobe earthquake, Japan , 2001 .

[28]  M. Parrot Use of satellites to detect seismo-electromagnetic effects , 1995 .

[29]  Sergey Pulinets,et al.  Main phenomenological features of ionospheric precursors of strong earthquakes , 2003 .

[30]  Shuanggen Jin,et al.  TEC response to the 2008 Wenchuan Earthquake in comparison with other strong earthquakes , 2010 .

[31]  Byung-Kyu Choi,et al.  Electron Density Profiles Derived From Ground-Based GPS Observations , 2006, Journal of Navigation.

[32]  Y. J. Chuo,et al.  Variations of ionospheric total electron content during the Chi‐Chi Earthquake , 2001 .

[33]  Guanyi Ma,et al.  Derivation of TEC and estimation of instrumental biases from GEONET in Japan , 2002 .

[34]  Shuanggen Jin,et al.  GPS detection of ionospheric Rayleigh wave and its source following the 2012 Haida Gwaii earthquake , 2017 .

[35]  J. Bernard Minster,et al.  GPS, Earthquakes, the Ionosphere, and the Space Shuttle , 1998 .