scholarly journals EquatorialEregion electric fields at the dip equator: 2. Seasonal variabilities and effects over Brazil due to the secular variation of the magnetic equator

2016 ◽  
Vol 121 (10) ◽  
pp. 10,231-10,240 ◽  
Author(s):  
J. Moro ◽  
C. M. Denardini ◽  
L. C. A. Resende ◽  
S. S. Chen ◽  
N. J. Schuch
2016 ◽  
Vol 68 (1) ◽  
Author(s):  
Juliano Moro ◽  
Clezio Marcos Denardini ◽  
Laysa Cristina Araújo Resende ◽  
Sony Su Chen ◽  
Nelson Jorge Schuch

2013 ◽  
Vol 51 (10) ◽  
pp. 1857-1869 ◽  
Author(s):  
C.M. Denardini ◽  
H.C. Aveiro ◽  
J.H.A. Sobral ◽  
J.V. Bageston ◽  
L.M. Guizelli ◽  
...  
Keyword(s):  
E Region ◽  

1993 ◽  
Vol 98 (A10) ◽  
pp. 17517 ◽  
Author(s):  
J. Hanumath Sastri ◽  
J. V. S. Visweswara Rao ◽  
K. B. Ramesh

1981 ◽  
Vol 86 (A4) ◽  
pp. 2095 ◽  
Author(s):  
S. Prakash ◽  
P. Muralikrishna
Keyword(s):  

1992 ◽  
Vol 40 (5) ◽  
pp. 655-662 ◽  
Author(s):  
R.Balachandran Nair ◽  
N. Balan ◽  
G.J. Bailey ◽  
P.B. Rao

2009 ◽  
Vol 27 (2) ◽  
pp. 631-638 ◽  
Author(s):  
H. C. Aveiro ◽  
C. M. Denardini ◽  
M. A. Abdu

Abstract. We analyze the effects of the 2-day wave activity in the EEJ using one coherent scatter radar and eight magnetometer stations located close to the dip equator. The wavelet analysis of the magnetometer data reveals a 2-day signature in the semidiurnal geomagnetic tide. The E-region zonal background ionospheric electric field, derived from coherent radar measurements, shows 2-day oscillations in agreement with such oscillations in the magnetometers data. An anticorrelation between the amplitude of the tidal periodicites (diurnal and semidiurnal) and that of the 2-day signature is also shown in the electric fields. The results are compared with simultaneous observations of 2-day planetary wave in meridional winds and ionosonde data. Further, our results are discussed based on the analysis of the magnetic activity.


1993 ◽  
Vol 13 (1) ◽  
pp. 299-302
Author(s):  
N. Balan ◽  
R. Balachandran Nair ◽  
G. Gopkumar ◽  
P.B. Rao

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