Corotational solar streams and cosmic-ray diurnal anisotropy
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A detailed comparison of the behavior of cosmic-ray diurnal anisotropy with the solar activity cycle indicates that the amplitude of the diurnal anisotropy is significantly modulated by the corotational streams that produce the secondary peak in geomagnetic activity. However, the time of the maximum of diurnal anisotropy does not show any systematic changes with solar activity but indicates a shift towards earlier hours (~12:00 LT), corresponding to the reversal of polarity of solar magnetic fields.
2019 ◽
Vol 15
(S354)
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pp. 147-156
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2012 ◽
Vol 50
(6)
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pp. 712-715
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2018 ◽
Vol 58
(2)
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pp. 169-177
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2016 ◽
Vol 12
(S328)
◽
pp. 130-133
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