The level of the mid-latitude geomagnetic northward component on quiet days in northern summer is observed to decrease or to increase by about 5 γ, depending on whether the interplanetary magnetic field (IMF) is directed predominantly toward or away from the sun. This effect produces about a 4° equatorward or poleward shift of the Sq current focus location. A simple method to determine the IMF polarities based on the effect is suggested.
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Satoki Matsushita (1975) studied this question.
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