






Vol.2 , No. 3, Publication Date: May 21, 2015, Page: 68-79
[1] | Werneck De Carvalho V. J. O., Department of Geophysics, National Observatory – ON Rio de Janeiro, Brazil. |
[2] | Hamza V. M., Department of Geophysics, National Observatory – ON Rio de Janeiro, Brazil. |
[3] | Benyosef L. C. C., Department of Geophysics, National Observatory – ON Rio de Janeiro, Brazil. |
Records of geomagnetic field variations obtained during September 2011, at six sites in the eastern parts of the Amazon region, have been employed for a better understanding of diurnal changes and the relative influences of solar quiet variations and Equatorial Electro Jet (EEJ) at low latitudes in Brazil. Analysis of these data sets provide new insights into the nature of superposition of solar quiet (Sq) and EEJ variations. Model studies reveal that the center of symmetry of EEJ variations is located at the mean latitude of approximately two degrees north. Comparison with results of earlier studies point to a northward shift of four degrees in the position of EEJ, during the period of 1999 to 2011. Inverse power law fit to selected data sets indicates that horizontal and vertical variations at the source regions of EEJ are greater by at least a factor of two when compared with values recorded by ground level magnetometers. Analysis of data sets have also allowed a better understanding of high frequency variations of geomagnetic field at ground level. Occurrences of micro pulsations, with amplitude greater than two nanotesla (nT), are found to characterize perturbed periods of geomagnetic fields relative to those of the calm periods. In addition, results of spectral analysis reveal that variations in the power spectral density (PSD) of micro pulsations have distinctly different characteristics during calm relative to those of the perturbed periods of geomagnetic fields. It has been possible to identify two distinct trends in the frequency dependence of PSD. Thus, for frequencies less than 0.0025 Hz the decrease in PSD follow a liner trend, while for those higher than 0.003 Hz changes in PSD are nearly independent of the frequency.
Keywords
Geomagnetic Variations, Amazon Region, Equatorial Electro Jet, Diurnal Changes, Micro Pulsations, Power Spectral Density
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