Science Explainer

How the Northern Lights Work

From a solar eruption 150 million kilometres away to a curtain of green light over an Icelandic glacier — the complete journey of the Aurora Borealis.

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The Sun

The Sun constantly emits a stream of charged particles — electrons and protons — called the solar wind, traveling at 400–800 km/s. During periods of high solar activity, the Sun also produces solar flares and Coronal Mass Ejections (CMEs).

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Earth's Magnetic Field

Earth's magnetosphere acts as a protective bubble, deflecting most solar wind particles around the planet. However, at the polar cusps, magnetic field lines converge and funnel particles inward toward the atmosphere.

Earth's magnetic field and magnetosphere diagram
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The Atmosphere — How Colors Form

When charged particles spiral down the magnetic field lines, they collide with oxygen and nitrogen molecules in the atmosphere. These collisions excite the molecules and emit light — the aurora.

Green
Oxygen at 100–150 km altitude
Most common aurora color
Red
Oxygen above 200 km altitude
Rare, seen at extreme activity
Purple/Blue
Nitrogen molecules at lower altitudes
Often at the base of green arcs
Pink
Mixed O and N₂ at aurora boundaries
Seen on the lower edge of green aurora
Understanding Activity

The KP Index Explained

The Planetary K-index (Kp) measures global geomagnetic activity on a scale from 0 to 9. It is derived from magnetometers at 13 stations worldwide and updated every 3 hours.

KP 0 – 1
No aurora
Geomagnetically quiet. No visible aurora even at polar latitudes.
KP 2 – 3
Faint aurora possible
Faint arcs may be visible from northern Iceland in dark skies. Best seen by camera.
KP 4
Good aurora activity
Curtains and bands visible to the naked eye from Iceland. A good night for viewing.
KP 5 – 6
Geomagnetic storm
Bright, active aurora with rapid movement. Visible from most of Iceland and northern Europe.
KP 7 – 9
Severe storm
Dramatic full-sky displays. Aurora visible at mid-latitudes in Scotland, Germany, and even further south.
Key Terms

Aurora Glossary

Bz

The north-south component of the interplanetary magnetic field (IMF). Negative Bz allows solar wind energy to flow into Earth's magnetosphere, triggering aurora.

Solar Wind Speed

The velocity of charged particles streaming from the Sun. Normal is 350-500 km/s. During solar storms it can exceed 800 km/s.

OVATION Model

A model from NOAA that predicts the intensity and location of the auroral oval in real time using solar wind data.

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