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sunspot





sunspot
Close-up of a sunspot obtained by the Japanese-led Hinode spacecraft
sunspot group
Sunspot group. Image courtesy Richard Crisp
An area of the Sun's photosphere, typically 2,500 to 50,000 km across, that appears dark because it is cooler than its surroundings. Sunspots are concentrations of magnetic flux and usually occur in pairs of opposite polarity that move in unison across the face of the Sun as it rotates; these pairs are linked by loops of magnetic field that arch through the Sun's corona.

The magnetic flux of a spot (normally measuring about 0.4 tesla but occasionally reaching 1.0 tesla or more), inhibits the rising of convective heat from below and so keeps the spot at a lower temperature – 1,500 to 2,500 K cooler than the rest of the photosphere.

Moderate to large spots usually have a darker central region (umbra) surrounded by a lighter halo (penumbra) with many short fine fibrils. In the umbra, the magnetic field lines tend to be nearly vertical, while in the penumbra, they are almost horizontal.

Sunspots are most commonly found within about 30° either side of the Sun's equator, although they can occur at higher latitudes. The lifetime of individual sunspots varies, from as little as a few days, or even hours, to (in the case of the largest spots) several months.


Sunspot cycle

As a whole, sunspot activity rises and falls regularly on an cycle that is approximately 11 years long, the frequency of sunspots varying from a maximum to a minimum level and back again. During a given cycle, the leading sunspots in groups in the northern solar hemisphere all tend to have the same polarity, while the same is true of sunspots in the southern hemisphere, except that here the common polarity is reversed. During the next sunspot cycle, the leading spots in each hemisphere flip to the opposite polarity. From this it's clear that the fundamental period governing solar activity is actually the 22-year magnetic cycle.


How sunspots are classified and counted

Sunspots are described using the McIntosh scheme, classified in terms of their field structure using the Mount Wilson magnetic classification, and counted using the relative sunspot number.

The Mcintosh scheme is a classification scheme for sunspots that superceded the older Zürich scheme in 1966. A three-letter code describes the class of sunspot group (single, pair, or complex), penumbral development of the largest spot, and compactness of the group.

The Mount Wilson scheme classifies sunspots in terms of their magnetic properties. Alpha denotes a unipolar sunspot group. Beta denotes a sunspot group having both positive and negative magnetic polarities, with a simple and distinct division between the polarities. Beta-Gamma denotes a sunspot group that is bipolar but in which no continuous line can be drawn separating spots of opposite polarities. Delta denotes a complex magnetic configuration of a solar sunspot group consisting of opposite polarity umbrae within the same penumbra. Gamma denotes a complex active region in which the positive and negative polarities are so irregularly distributed as to prevent classification as a bipolar group.

The relative sunspot number is a number devised by Rudolf Wolf of Zurich in 1849 to describe sunspot activity. Sometimes called the Wolf number, it is defined as:

R = k (10g + f)

where R is the sunspot number, k is a constant depending on the instrument used, g is the number of disturbed regions, and f is the total number of sunspots.


Related category

   • SOLAR TOPICS