Ionospheric Total Electron Content Response to the December 26, 2004 North Sumatra Earthquake

The functional fitting model using daily EUV is the most accurate with 9.2 TECu of root mean square er- ror (RMS) than the 15-days running median with 10.4 TECu RMS and the model

(1986) and Watanabe and Oya (1986) have re- ported localized regions of plasma density enhancements co- occurring with the plasma density depletions in the night- time equatorial

Therefore a non-stationary and anisotropic covariance model is set up and its parameters are determined within a maximum-likelihood approach in- corporating GNSS total electron

Figure 3 shows the TEC time series of the epicenter within 14 days be- fore the earthquake, revealing that obvious positive anoma- lies occurred one day before the earthquake,

The com- bination of seismological and space data reveals some inter- esting features for this time period: (1) six successive high speed solar wind streams obviously triggering

Based on the spatial distribution of TEC and the electron density, the global ionosphere is divided into four regions, that is, the northern region of over 45°N, the region between

in press b: Modelling seismic response from North Sea chalk reservoirs resulting from changes in burial depth and fluid saturation. (eds): Petroleum geology: North-West Europe

INUNDATION MAPPING – A HAZARD STUDY BASED ON THE DECEMBER 26, 2004 TSUNAMI ALONG THE KARAIKAL COAST OF INDIAK. Baskaran* Department