Conjugate aspects of auroral zone electron precipitation are examined using data from ten simultaneous balloon flights of X-ray detectors from Fairbanks, Alaska, and Macquarie Island, Australia, as well as riometer data from Kotzebue and College, Alaska. These results indicate a close correspondence, in similarity and simultaneity, in regions of near conjugacy over a wide range (Kp = 0+ to 60) of geophysical disturbance. Whereas gross features of activity remain intact, dissimilarities become quite evident at locations well removed from near conjugacy.
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Brown et al. (1965) studied this question.
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