Inter-hemispheric trans-equatorial field-aligned currents deduced from MAGDAS at equatorial zone
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[1] I. Adimula,et al. Preliminary Results from the Magnetic Field Measurements Using MAGDAS at Ilorin, Nigeria , 2009 .
[2] T. Moretto,et al. On the cause of IMF By related mid‐ and low latitude magnetic disturbances , 2007 .
[3] S. Macmillan,et al. A magnetic field model with daily variations of the magnetospheric field and its induced counterpart in 2001 , 2004 .
[4] T. Iyemori,et al. Seasonal and local time dependences of the interhemispheric field‐aligned currents deduced from the Ørsted satellite and the ground geomagnetic observations , 2002 .
[5] M. Takeda. Features of global geomagnetic Sq field from 1980 to 1990 , 2002 .
[6] C. Onwumechili,et al. On the course of the geomagnetic daily variation in low latitudes , 1977 .
[7] H. Maéda. Field-aligned current induced by asymmetric dynamo action in the ionosphere , 1974 .
[8] W. Campbell. The field levels near midnight at low and equatorial geomagnetic stations , 1973 .
[9] D. Sabben. Solstitial Sq-currents through the magnetosphere , 1970 .
[10] D. Sabben. The computation of magnetospheric currents, caused by dynamo action in the ionosphere , 1969 .
[11] John W. Gettemy. Magnetic daily variation at Koror , 1962 .
[12] A. Onwumechilli. Fluctuations in the geomagnetic horizontal field near the magnetic equator , 1960 .
[13] M. Takeda. Geomagnetic field variation and the equivalent current system generated by an ionospheric dynamo at the solstice , 1990 .