
The approximately 11-year cycle of solar activity, including the periodic reversal of the Sun's magnetic poles.The solar cycle is the roughly 11-year periodic variation in the Sun's activity, marked by changes in the number of sunspots, solar flares, and coronal mass ejections. This cycle is driven by the Sun's magnetic field, which undergoes a complete reversal of polarity every cycle — the north and south magnetic poles swap places. The cycle is not perfectly regular; it can vary in length from about 9 to 14 years, and its amplitude changes over decades and centuries, as seen in the Maunder Minimum in the 17th century when sunspots nearly disappeared.
The discovery of the solar cycle is usually attributed to Heinrich Schwabe, who in 1843 announced the periodic variation in sunspot numbers after 17 years of observations. Rudolf Wolf later systematized the counting of sunspots and established the cycle's average length of about 11 years.
The cycle arises from the interaction between the Sun's differential rotation (the equator rotates faster than the poles) and its convective motions. These stretch and twist the magnetic field lines, amplifying them over time. Eventually, the field becomes so tangled that it erupts through the surface as sunspots and active regions. As the cycle progresses, the magnetic field's polarity reverses, and the process starts anew. The cycle's details are still not fully understood, but it is known to be a self-sustaining dynamo process in the Sun's interior.
Solar cycle predictions are used to plan satellite operations, power grid management, and space missions, as solar activity affects space weather and can disrupt communications and navigation systems.
The solar cycle influences not only space weather but also Earth's climate: the Maunder Minimum, a period of very low solar activity, coincided with the coldest part of the Little Ice Age.

















