Space Weather Alert: Sunspots, Coronal Holes, and Space Storms

SETI News https://www.seti.org/news/space-weather-alert-sunspots-coronal-holes-and-space-storms/

What Is Space Weather?

Space weather refers to changes in the environment driven by the Sun, specifically the flow of plasma – ionized gas – and radiation that interacts with a planet’s magnetic field and atmosphere. Unlike Earth’s meteorological weather, space weather is shaped by electromagnetic forces rather than temperature or moisture.

Dr. Robinson explains that the Sun constantly emits a steady stream of charged particles known as the solar wind. Earth’s magnetic field protects the planet from most of this radiation. Still, fluctuations in solar activity, such as coronal mass ejections (CMEs) or bursts of high-speed solar wind, can disturb that balance.

At the moment, the Sun is just past solar maximum, the peak of its roughly eleven-year magnetic activity cycle. During this phase, solar storms become more frequent and intense. The timing has coincided with Earth’s autumnal equinox this year, when the planet’s magnetic field aligns more directly with the Sun’s. The result is a “perfect storm” for enhanced space weather effects.

The Role of Coronal Holes

Most space weather events originate in bright, magnetically active regions of the Sun, but the recent storm is unusual – it begins in a coronal hole.

In ultraviolet images captured by NASA’s Solar Dynamics Observatory, coronal holes appear dark because they are slightly cooler than their surroundings. The magnetic field lines in these regions are open, allowing plasma to escape freely into interplanetary space. Dr. Robinson describes this as a “magnetic superhighway” that channels solar wind directly toward Earth.

When the solar wind carries a southward-pointing magnetic field, it interacts efficiently with Earth’s northward magnetic field. This process, called magnetic reconnection, allows solar particles to penetrate Earth’s magnetosphere, generating impressive geomagnetic storms and auroral displays. The recent event produced a particularly strong southward magnetic component, an ideal setup for intense geomagnetic activity.

From the Sun to the Sky

As the solar wind reaches Earth, it disturbs both the planet’s magnetic field and the ionosphere, a layer of charged particles in the upper atmosphere. These disturbances can be detected using magnetometers, instruments that record local changes in magnetic field strength.

In Norway, magnetometer readings during the recent storm showed rapid dips, called substorms, signaling active aurorae overhead. Additional data from the Norwegian Mapping Authority revealed a surge in the ionosphere’s total electron content, confirming that a powerful wave of solar particles had entered the atmosphere.

When these energetic electrons collide with oxygen and nitrogen in the atmosphere, they excite the atoms and emit photons (light). Green emissions come from oxygen at mid-altitudes, while purple and red hues occur when electrons strike nitrogen deeper in the ionosphere. The stronger the storm, the farther south these aurorae extend, which is why the recent display was visible across much of North America and Europe.

Lessons from the Carrington Event

The conversation also revisits the Carrington Event of 1859—the most powerful geomagnetic storm on record. That event produced aurorae visible near the equator and disrupted telegraph systems worldwide. Electrical currents induced by the storm’s magnetic fluctuations shocked operators and sent messages through disconnected lines.

If a similar event occurred today, it could severely damage our power grids, communication systems, and satellites. Estimates suggest recovery from such a disruption could take years and tens of billions of dollars.

This activity underscores the importance of missions like the Multi-slit Solar Explorer (MUSE). Planned for launch no earlier than 2027, MUSE will study the Sun’s corona using a 35-slit imaging spectrograph, an instrument that measures light at multiple wavelengths to infer plasma temperature, speed, and turbulence. This data will help scientists better understand and eventually predict significant solar eruptions.

Understanding and Predicting the Unpredictable

Scientists estimate that it takes solar material 14 hours to several days to reach Earth; accurate forecasting remains a challenge. The complex interactions between the Sun’s magnetic field and the interplanetary medium make prediction difficult.

Citizen scientists play a vital role in monitoring these events. Projects like Aurorasaurus collect real-time reports from observers worldwide, helping researchers track the extent and intensity of auroral activity.

As Dr. Robinson notes, space weather is not just a scientific curiosity; it is a dynamic system that connects the Sun, Earth, and human technology in profound ways.

Watch the whole conversation on SETI Live to learn how SETI Institute scientists are decoding the Sun’s magnetic secrets and safeguarding our planet from the next big space storm.