The Sun undergoes a type of seasonal variability, with its activity
waxing and waning over the course of nearly two years, according to a
new study by a team of researchers led by the National Center for
Atmospheric Research (NCAR). This behavior affects the peaks and valleys
in the approximately 11-year solar cycle, sometimes amplifying and
sometimes weakening the solar storms that can buffet Earth’s atmosphere.
The
quasi-annual variations appear to be driven by changes in the bands of
strong magnetic fields in each solar hemisphere. These bands also help
shape the approximately 11-year solar cycle that is part of a longer
cycle that lasts about 22 years.
“What we’re looking at here is a
massive driver of solar storms,” said Scott McIntosh, lead author of the
new study and director of NCAR’s High Altitude Observatory. “By better
understanding how these activity bands form in the Sun and cause
seasonal instabilities, there’s the potential to greatly improve
forecasts of space weather events.”
The overlapping bands are
fueled by the rotation of the Sun’s deep interior, according to
observations by the research team. As the bands move within the Sun’s
northern and southern hemispheres, activity rises to a peak over a
period of about 11 months and then begins to wane.
The
quasi-annual variations can be likened to regions on Earth that have two
seasons, such as a rainy season and a dry season, McIntosh said.
The
study, published this week in Nature Communications, can help lead to
better predictions of massive geomagnetic storms in Earth’s outer
atmosphere that sometimes disrupt satellite operations, communications,
power grids, and other technologies.
The research was funded by NASA and the National Science Foundation, which is NCAR’s sponsor.
The
new study is one of a series of papers by the research team that
examines the influence of the magnetic bands on several interrelated
cycles of solar magnetism. In a paper last year in Astrophysical
Journal, the authors characterized the approximately 11-year sunspot
cycle in terms of two overlapping parallel bands of opposite magnetic
polarity that slowly migrate over almost 22 years from high solar
latitudes toward the equator, where they meet and terminate.
McIntosh
and his co-authors detected the twisted, ring-shaped bands by drawing
on a host of NASA satellites and ground-based observatories that gather
information on the structure of the Sun and the nature of solar flares
and coronal mass ejections (CMEs).
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