Parker spiral: how it works and what it teaches us
As the solar wind flows outward, the Sun’s rotation winds the magnetic field into a spiral geometry. This structure magnetically connects distant regions of the heliosphere back to their solar source.
What it really means
The Sun is not a static surface but an evolving magnetised plasma. Understanding Parker spiral therefore requires looking at magnetic fields, temperature, density and plasma motion together; isolating a single parameter easily leads to the wrong conclusion. Observed properties can change quickly and also depend on viewing geometry, so a single image is not enough to describe the full evolution.
Why it matters
These processes occur long before any disturbance reaches Earth. Their relevance to aurora observers is precisely that they explain the physical origin of conditions that, hours or days later, may alter the solar wind and Earth’s magnetosphere. For an aurora observer it is mainly a causal piece of the puzzle: it helps identify what kind of disturbance may be produced, but by itself it cannot tell how geoeffective that disturbance will be at Earth.
How to interpret it without oversimplifying
Images of the Sun show only part of the story. Different wavelengths reveal different layers and temperatures, while magnetograms and coronagraphs provide information that visible-light photographs cannot.