Abstract

We have studied the latitude-time distribution of the green (5303 A) coronal line emission for 1940–1989 from observations by Waldmeier (1957), Kislovodsk, Lomnický Stit, Norikura, and Pic-du-Midi - Q.B.S.A. (1955–1987). We have compared these data with the distributions of the weak magnetic field (Stenflo, 1988), of polar faculae and sunspots, and have given our interpretation of the results. We have found that a new cycle of coronal activity commences after the polar field reversal in the form of two components in each hemisphere. We identify the first component with the polar faculae that appear at latitude 40° and migrate polewards. The second component representing sunspots shows up at 40° latitude 5–6 years after and drifts equatorward. Thus the global coronal activity cycle has a duration of 16–17 years and is described by two components that reflect the activity of polar faculae and sunspots.

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