The equatorial electrojet and the profile parameters B0 and B1 around midday

[1]  Ludger Scherliess,et al.  Radar and satellite global equatorial F-region vertical drift model , 1999 .

[2]  M. Menvielle,et al.  Equatorial electrojet at African longitudes: first results from magnetic measurements , 1998 .

[3]  S. Radicella,et al.  Diurnal variation of ionospheric profile parameters B0 and B1 for an equatorial station at low solar activity , 1998 .

[4]  J. O. Adeniyi Experimental equatorial ionospheric profiles and IRI model profiles , 1997 .

[5]  K. Viswanathan,et al.  Electric fields and currents in the equatorial electrojet deduced from VHF radar observations—III. Comparison of observed ΔH values with those estimated from measured electric fields , 1987 .

[6]  P. Mayaud,et al.  Equatorial electrojet and regular daily variation SR—IV. Special features in particular days , 1976 .

[7]  A. Richmond,et al.  The relationship between the structure of the equatorial anomaly and the strength of the equatorial electrojet , 1973 .

[8]  G. J. Bailey,et al.  Modeling studies of equatorial plasma fountain and equatorial anomaly , 1996 .

[9]  T. Gulyaeva Progress in ionospheric informatics based on electron-density profile analysis of ionograms , 1987 .

[10]  S. Sampath,et al.  Results from in situ Measurements of Ionospheric Currents in the Equatorial Region-I , 1979 .

[11]  P. Mayaud,et al.  Equatorial electrojet and regular daily variation SR—I. A determination of the equatorial electrojet parameters , 1976 .

[12]  P. Mayaud,et al.  Equatorial electrojet and regular daily variation SR—II. the centre of the equatorial electrojet , 1976 .