Concept

Cosmogenic isotope — where it appears

A radioactive isotope made when cosmic rays strike atoms, chiefly carbon-14 and beryllium-10 made in the upper atmosphere. Stored in tree rings and polar ice, they record the cosmic-ray flux, which both the Sun's field and the Earth's field modulate.

Named by 2 essays across one field — each of them below, with the objects they name alongside it.

4 cycles of wings, and the polarity reverses at every boundary. Sunspot latitude against date, one mark per spot group, over 4 cycles of 11 years. The pattern is the reason the plot is called a butterfly diagram, and both of its features are laws with names. Spörer's law is the downward slope: spots emerge near ±28° at the start of a cycle and near ±7° at the end, so each wing narrows towards the equator and never crosses it. Hale's law is what the two mark shapes say: the leading spot of a pair has one magnetic polarity in the north and the other in the south, and both reverse when a new cycle starts — so a diagram that repeats every 11 years in appearance repeats only every 22 in magnetism. The wings overlap: the first high-latitude spots of a cycle appear about 1.6 years before the last low-latitude spots of the one before, which is why counting spots gives a cycle length slightly different from measuring one between polarity reversals. The dot density in time is the sunspot number itself, drawn from the standard skewed fitting function — the rise to maximum takes about four years and the decline about seven, in every cycle ever recorded.

A magnetic clock read off a butterfly

Plot sunspot latitude against date and the marks form wings that open at thirty degrees and march to the equator. The polarities reverse between wings, so the magnetic period is twenty-two years and the famous eleven is an artefact of counting spots rather than fields.

stars · Solar cycle $One production rate, many Suns. Global isotope production, as a fraction of today's average, over the modulation potential and the Earth's dipole moment. Each contour is one production rate — 0.85, 1, 1.2, 1.4, 1.7 times today's — and every point on it is a combination of Sun and Earth an isotope record cannot distinguish. Production at today's dipole of 7.8 × 10²² A m² and a modulation potential of 650 MV is reproduced exactly by a dipole of 10 with a potential of 449 MV. Over the last ten thousand years the dipole is thought to have ranged between about 6 and 11 in these units, the band across the middle of the plane. So a record of production becomes a record of the Sun only after a record of the dipole has been divided out, and the solar history inherits every error in the geomagnetic one.$

A Sun read through a shield that also changed

Carbon-14 in tree rings and beryllium-10 in ice extend the record of solar activity ten thousand years past the first telescope, because the Sun's field keeps cosmic rays out of the atmosphere that makes them. But the Earth's own field keeps them out too, and over those ten thousand years it changed by as much as the Sun does over a cycle. An isotope record measures the two shields together, so the Sun comes out of it only after the Earth has been divided out — and every slow trend in the reconstructed Sun is, until shown otherwise, a trend in that division.

stars · Solar cycle

Named alongside it

The objects these essays reach for when they reach for this one.

Maunder minimum Solar cycle Active region Butterfly diagram Carbon cycle Cosmic rays Differential rotation Dipole moment Geomagnetic cutoff Grand minimum Hale polarity law Modulation potential

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