Abstract
From the analysis of the external components of the equinoctial geomagnetic daily variation in Peru it follows that they are generated by a complex current system. In this work it is found that in addition to the global current system and the main electrojet, with I0=0.124Amp/m, it is necessary to include two secondary lateral currents parallel to the main electrojet. Their intensities are I1=0.38I0 and I2=0.03I0, north and south of the dip equator, respectively.
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