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How Aurora Forecasting Works

Aurora forecasting combines real-time solar data with geomagnetic measurements to predict when and where the Northern Lights might be visible. Our system analyzes several key factors to provide accurate predictions.

Key Metrics We Track

Kp Index

The Kp index measures global geomagnetic activity on a scale from 0 to 9. Higher values indicate stronger aurora activity and visibility at lower latitudes.

Particle Density

The concentration of solar wind particles. Higher density combined with high speed can trigger intense auroral activity.

Solar Wind Speed

Measures how fast charged particles from the sun are traveling. Speeds above 500 km/s often indicate favorable conditions for aurora displays.

Magnetic Field (Bz)

The north-south direction of the interplanetary magnetic field. Negative values are more favorable for aurora activity.

Visibility by KP Index


1-2 | Tromsø, Abisko, Alta, Murmansk

2-3 | Lofoten, Bodø, Kiruna, Reykjavík

3-4 | Trondheim, Sundsvall, Nokia

4-5 | Oslo, Helsinki, Stockholm

5-6 | Copenhagen, Berlin, Hamburg

Factors Affecting Visibility

What You Need

  • Clear Skies: No clouds or precipitation
  • Dark Location: Away from city lights
  • Good Timing: Winter months are best
  • Patience: Aurora can appear suddenly
  • Warm Clothes: It gets very cold!

Best Viewing Tips

  • Look North: It appear in the north
  • Peak Hours: 10PM-2AM local time
  • Night Vision: Let your eyes adjust (20+ min)
  • Camera: Cameras can see the aurora better
  • Check Forecast: Use our KP index forecast

Understanding the Aurora Oval

The aurora oval shown above represents the typical area where Northern Lights are visible. This oval expands and contracts based on solar activity.

During periods of high solar activity (high KP index), the oval expands southward, making the aurora visible at lower latitudes.

The map shows the approximate aurora visibility zones at different latitudes.

Data delivered by Auroras.live 

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