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Understanding aurora

What is the Kp index?

The Kp index is a single number, from 0 to 9, that sums up how disturbed Earth's magnetic field is right now. The higher it climbs, the further from the poles the aurora can be seen - which is exactly why it's the first number every aurora-watcher checks.

The short answer

"Kp" stands for planetary K-index - short for the German "planetarische Kennziffer", introduced by Julius Bartels in 1949. Every three hours, magnetic observatories around the world measure how much the local magnetic field has been disturbed by the solar wind. Those readings are combined into one global figure: the Kp index.

A quiet night sits at Kp 0–2. A decent display reaches Kp 4–5. The rare, history-making storms that paint aurora over southern Europe are Kp 8–9. Because it's measured globally, the same Kp number applies everywhere on Earth at once - what changes is what that number means for your latitude.

Quick rule of thumb: the further you are from the magnetic poles, the higher the Kp you need. Tromsø sees aurora at Kp 1; London needs roughly Kp 6–7.

The 0–9 scale

Each step up the scale roughly doubles the disturbance. Here's what each band means and how far south the lights typically reach:

KpLevelTypically visible from
0–2QuietSvalbard, northern Tromsø, far-north Alaska
3UnsettledTromsø, Iceland, Fairbanks, northern Norway
4–5Active · minor stormScotland, southern Norway, northern Canada
6–7Moderate–strong stormNorthern England, Ireland, Germany, Seattle
8–9Severe–extreme stormSouthern Europe, central US - rare and spectacular

How Kp is calculated

Thirteen observatories at mid-latitudes record how far Earth's magnetic field deviates from its quiet-day baseline every three hours. Each station converts its measurement to a local K index (0–9), then the 13 readings are averaged and standardised into the global Kp value.

The logarithmic nature of the scale matters. A jump from Kp 5 to Kp 7 is not twice as strong - it represents roughly 10 times the field disturbance. This is why aurora expands dramatically southward during high-Kp events.

What Kp doesn't tell you

Kp is powerful but blunt. It's an average over three hours and the whole planet, so it misses a lot of what decides your actual night:

  • Cloud cover - a clear Kp 3 beats a cloudy Kp 6 every time.
  • Timing - Kp can spike for 20 minutes and the three-hour value barely moves.
  • The Bz direction - when the solar wind's magnetic field points south, energy pours into the magnetosphere. This often matters more than Kp in the moment.

That's why the aurora forecast on this site pairs Kp with live solar-wind data, local cloud cover, and moon phase - turning one blunt number into a real answer for your sky.

Aurora by Kp level

Each Kp level reaches a different latitude band. Select a Kp level to see all locations that become visible at that threshold:

Sean Barraclough

Sean Barraclough

Creator of Aurora Tonight

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Common questions

What does Kp stand for?
Kp stands for "planetarische Kennziffer" - a German term meaning planetary index. It was introduced by Julius Bartels in 1949 and remains the standard global measure of geomagnetic disturbance.
How is the Kp index measured?
Kp is calculated from magnetometer readings at 13 observatories spread across mid-latitudes worldwide. Each station measures how much the magnetic field deviates from its quiet-day baseline over three-hour intervals. These readings are averaged and converted to a single 0-9 scale, updated eight times per day.
How often is the Kp index updated?
Eight times per day - once every three hours. Each value covers the previous three-hour window, so there is always a short lag between real-world conditions and the published number. During an active storm the Kp can shift significantly from one three-hour period to the next.
What Kp do I need to see the northern lights from the UK?
It depends on your location. From the Scottish Highlands, Kp 3-4 can be enough on a clear night away from light pollution. Edinburgh and southern Scotland typically need Kp 4-5. Newcastle and northern England need around Kp 5-6. London and the south of England need Kp 7 or above - that requires a significant geomagnetic storm.
Is a Kp of 5 a geomagnetic storm?
Yes. Kp 5 marks the threshold for a G1 (minor) geomagnetic storm on the NOAA storm scale. G1 storms can cause minor disruptions to satellite operations and produce aurora visible above around 60°N - that means northern Scotland and Scandinavia in clear conditions.
What is the difference between Kp and the G-scale?
They measure the same thing on different scales. The G-scale runs G1 to G5 and is used for public forecasting. Kp runs 0 to 9. G1 = Kp 5, G2 = Kp 6, G3 = Kp 7, G4 = Kp 8, G5 = Kp 9. Below Kp 5 is G0 - no storm, quiet conditions.
Where does this site get its Kp data from?
All space weather data comes from NASA's DONKI - the Space Weather Database Of Notifications, Knowledge, Information - maintained by the Community Coordinated Modeling Center. Data refreshes every 30 minutes.
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