From examination of X-ray and ionospheric absorption data during magnetic bays in the auroral zone, it has been found that electron precipitation on the atmosphere accompanies auroral-zone electrojets. The position of an electrojet and its associated electron precipitation region, rather than the amount of current in the system, largely controls the magnitude of X-ray and ionospheric absorption effects.
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Barcus et al. (1962) studied this question.
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