Can I See the Northern Lights Tonight?

This page checks two real, independent things live: whether current geomagnetic activity is strong enough to bring the aurora to your latitude, and whether your local sky is clear enough to actually see it. Enter your location below for a real-time answer, or read on for the full picture.

🔭 Localized Visibility Terminal

Current Kp Index

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Data Layer: NOAA SWPC

Geomagnetic Storm Level

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Data Layer: NOAA SWPC

Solar Wind Speed

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Data Layer: DSCOVR / ACE

Cloud Cover — Your Location

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Data Layer: Open-Meteo

Live NOAA Aurora Oval Forecast

NOAA OVATION model aurora oval forecast, northern hemisphere

Source: NOAA SWPC OVATION model — updates automatically on NOAA's servers.

Best viewing window tonight: typically 10 PM – 2 AM local time, centered on local magnetic midnight when your location rotates deepest into Earth's magnetotail.

What determines whether you can see the Northern Lights?

Aurora visibility comes down to two largely independent factors. First, geomagnetic activity: the aurora is produced when charged particles from the solar wind funnel down Earth's magnetic field lines into the upper atmosphere, and how far that activity extends toward the equator is measured by the Kp index. Second, local sky conditions: even a strong geomagnetic storm is invisible if your sky is overcast, since the aurora occurs roughly 60-250 miles up, well above any cloud layer. A genuinely clear forecast requires both a high enough Kp for your latitude and a clear or mostly-clear local sky.

What Kp index do you need for your location?

The aurora oval sits at a fairly consistent magnetic latitude during quiet conditions and expands toward the equator as Kp rises. Locations already close to the Arctic or Antarctic Circle — northern Scandinavia, Iceland, Alaska, northern Canada — sit under the oval on many clear nights even at Kp 2-3. Mid-latitude locations, like the northern United States or central Europe, typically need Kp 5-6 for a visible display. Southern US states or southern Europe generally require a rarer Kp 7 or higher event.

How solar wind affects the aurora

Beyond the Kp index itself, two solar wind properties matter directly: speed and the orientation of the interplanetary magnetic field (IMF Bz). Faster solar wind delivers more energy into the magnetosphere. When Bz points southward, it can link up with Earth's own northward-pointing field through a process called magnetic reconnection, opening a more efficient channel for solar wind energy to reach the upper atmosphere — which is why a southward Bz alongside elevated speed is one of the strongest real-time signs of an active or intensifying aurora.

Why cloud cover matters

The aurora happens far above the weather — typically 60 to 250 miles up, compared to clouds which top out around 8-12 miles. That means cloud cover doesn't weaken the aurora, it simply blocks the view entirely. A night with an extremely active geomagnetic storm but full overcast will show nothing, while a quieter night with a crystal-clear sky can still offer a great view if conditions are borderline. Checking both together, as this page does, gives a much more honest answer than checking either alone.

Best aurora viewing tips

Get away from city light pollution — even moderate light domes can wash out a faint display. Give your eyes 15-20 minutes to adjust to darkness. Check the Kp index and cloud cover shortly before heading out, since both can shift over a few hours. Look toward the pole-facing horizon (north in the Northern Hemisphere) first, since that's typically where a developing aurora appears earliest. A camera with a few-second exposure can sometimes pick up color and structure the naked eye misses on fainter nights.

How often this forecast updates

The Kp index, solar wind speed, and IMF Bz shown above refresh automatically roughly once a minute from NOAA's real-time feeds — this isn't a static daily forecast, it reflects current conditions as closely as the underlying satellite data allows.

Where this data comes from

Kp index, solar wind speed, density, and IMF Bz all come from NOAA's Space Weather Prediction Center (SWPC), sourced from real-time satellite measurements at the L1 Lagrange point roughly 1 million miles sunward of Earth. Cloud cover comes from Open-Meteo's weather data. Nothing on this page is a static or invented estimate — every number reflects a real, currently-reported measurement.

Frequently Asked Questions

It depends on two independent things: whether geomagnetic activity (the Kp index) is high enough to push the aurora oval down to your latitude, and whether your local sky is clear enough to actually see it. Enter your location above for a live check of both.

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