North-south asymmetry of the substorm intensity depending on the IMF BY-component

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Scientific paper

The dependence of maximum variations of H-component negative bays at magnetic conjugate stations on a sign of the IMF BY-component during the substorms of small and moderate intensity with |DH|max < 750 nT developed at Bz < 0 and |Bz/BY| < 1 has been studied. By data from Kotzebue (F = 64.5°; L = 249.7°) and Macquarie Isl. (F = -64.5°; L = 247.8°) observatories in the eastern hemisphere and Leirvogur (F = 65.3°; L = 68.2°) and Syowa (F = -66.1°; L = 71.0°) stations in the western hemisphere it is shown that at BY < 0 the absolute values of negative bays |DH|max are greater in the southern hemisphere and at BY > 0, on the contrary, in the northern hemisphere.

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