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Viewing Northern Lights in the UK

Northern Lights from 21st Oct 2003 in Crooktree, NE Scotland. Photo courtest of Jim Henderson Photography

Chart showing the current and recent geomagnetic activity in the UK and globally. The K-index values for the 3 UK observatories and the estimated global Kp is shown.

Model showing likely locations that will see auroraas the auroral oval moves south as activity increases. Based on geomagnetic activity level Kp. Image from

It is easier to see the northern lights (aurora borealis) in the UK than you might think. All you need is a dark place, a clear sky and very good timing!

The good timing is important as the northern lights are a result of a geomagnetic storm. These storms are short-lived periods of high geomagnetic activity where the Earth's magnetic field changes very quickly and strong electric currents flow high in the atmosphere.

Why does it happen?

The aurora is a consequence of activity on the surface of the Sun. Occasionally there are large explosions on the Sun, and huge amounts of charged particles are thrown out into space. These particles sometimes travel towards Earth where they are captured by the Earth's magnetic field and guided towards the geomagnetic polar regions.

On their way down these particles are slowed down by Earth's atmosphere, which acts as a shield. These charged particles collide with gas molecules in the atmosphere. The energy released in these collisions is given off as light.

What makes the colours?

When a charged particle collides with a molecule in the atmosphere the molecule becomes excited. The excited molecule is unstable and will give up its extra energy by emitting light.

The colour of the light depends on the molecules being excited. Like a sodium street light which gives off an orange light, the oxygen, nitrogen and other gases in the atmosphere have their own particular colours resulting in the range of blues, greens, yellows and reds observed in the aurora.

Where can you see it?

The auroral ovals represent the places on Earth where aurora occur most often and with greatest intensity. Under normal conditions the northern oval covers Scandinavia, Greenland, Alaska, Canada and Russia. The southern oval covers the Antarctic regions. With increasing geomagnetic activity the ovals widen and spread, so that during periods of high geomagnetic activity it becomes possible to see aurora further south in the UK.

When can I see it?


On average you might expect to see aurora in the far north of Scotland every few months, but less often as you travel further south.

Geomagnetic storms follow the 11-year solar cycle. The chance of big magnetic storms will be greatest around the years leading up to solar maximum and shortly afterwards. The current progress of the solar cycle is tracked by counting the number of sunspots seen on the Sun.

Generally, there are more magnetic storms around the equinoxes (March-April, September-October).

Tips for a budding aurora hunter


1. Look out for a geomagnetic storm

Check the internet to look for strong geomagnetic storm activity. For example, here

There are many ways to represent geomagnetic activity. One of these is the Kp index which ranks the variations in geomagnetic activity from 0 to 9, in 3-hour intervals. The larger the Kp index is, the stronger the storm and the further south the northern lights will be visible. The map on the right shows roughly where you might expect to see aurora based on Kp index levels.

Follow us on Twitter:

Twitter logo @BGSauroraAlerts for occasional aurora alerts

Twitter logo @BGSspaceWeather for daily forecasts of Space Weather

2. When there is a storm...

  • Find a dark place away from street lights.
  • You will need a cloud-free sky.
  • In general, look to the north although it could be overhead or elsewhere.
  • In general, for the best chance of sighting an aurora, try to look during the hours around local midnight (22:00-02:00). However geomagnetic activity can happen at any time!