Wing I · the terraceRoom IV of IV
Inv. no. I.4 · the magnetometer
The northern lights
On the night of 10 May 2024 half the Netherlands stood in the garden holding up a phone, and the phones showed pink and green skies. It happens every few years over the Netherlands, more often when the Sun is near the top of its eleven-year cycle. The northern lights hang in a ring around the magnetic pole, a hundred kilometres up and more, and on most nights that ring stays far north, over Norway and Iceland. When the Sun throws a storm at us, the ring swells southwards. This room watches it live and works out whether it is over Eindhoven's horizon tonight.
Tonight from Eindhoven
Reading NOAA's forecast…
Fig. I. The Arctic from above, Europe at the bottom: NOAA's forecast of the oval for the coming hour, the chance of aurora overhead, brighter where it is likelier. Shaded: night.
- Kp, the storm scale
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- Edge of the oval, at Eindhoven's longitude
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- A bright curtain there, its top above our horizon
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- The solar wind
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- The sky over Eindhoven
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- The next three days
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The oval is NOAA's OVATION model, run on the solar wind measured a million and a half kilometres sunwards of us, half an hour to an hour before it arrives. Each point is the chance of aurora straight overhead. You do not have to stand under it: a curtain of light is tall, and from a long way south you can see its top over the horizon. So the question for Eindhoven is how close the edge comes, and how high that puts the top of the curtain in our northern sky.
Kp is how hard the Earth's magnetic field is being shaken, from 0 (calm) to 9, worked out every three hours from magnetometers at a dozen observatories; the figure here is NOAA's minute-by-minute estimate, and the verdict also looks at NOAA's forecast for the next twelve hours. On a quiet night it sits around 1 or 2. NOAA calls Kp 5 a minor storm; at Kp 7 the aurora is typically seen down to 50° geomagnetic latitude, at Kp 6 to 55°. Eindhoven is at about 52½°, so a Kp of 6 to 7 is roughly what we need, and a clear, dark sky to the north.
If the verdict says go: wait until it is properly dark, find a spot with no lamps between you and the northern horizon, give your eyes a few minutes, and take a photo in night mode. The phone often shows it first.
Over the curve of the Earth
Fig. II. From Eindhoven due north, heights and distances to the same scale. The dashed line is our horizon; anything below it is hidden by the Earth.
- From Eindhoven to the curtain
- Green, 120 km up, stands at
- Red, 300 km up, stands at
The colours are layers. Electrons from the solar wind, steered down along the magnetic field, hit the thin air a hundred kilometres up and more. Oxygen glows green between about 100 and 250 kilometres; higher up, where the air is so thin that an excited oxygen atom can wait up to two minutes for its turn to shine without bumping into anything, it glows red. Nitrogen at the bottom edge adds violet and a pink fringe. From far south, the Earth hides the green and only the red top clears the horizon. And in the big storms that bring it this far, more of the incoming electrons are slow ones, which give up their energy high up, where the red is made. Between the two, the aurora over the Netherlands is usually red.
And why phones see it better than people: a camera collects light for a second or more, and its sensor sees colour at any brightness. Our eyes at night see with rods, which are sensitive but colour-blind, so a faint aurora looks like a grey-white glow, a cloud that does not move with the wind. Press your eyes to see the difference. On a strong night, like May 2024, the colour shows to the eye too.
Where it already matters
A compass that swings, 1741. In Uppsala, Olof Hiorter and Anders Celsius noticed that their compass needle swung when the northern lights were overhead, and that observers far away saw it swing at the same time. The first clear proof that the aurora and the Earth's magnetism belong together; this room's instrument, the magnetometer, still measures it.
The Carrington event, 1859. On 1 September Richard Carrington saw a flash of white light on the Sun. Within a day the strongest geomagnetic storm on record hit: aurora as far south as the Caribbean, telegraph lines that sparked, and operators who disconnected their batteries and kept sending on the current the storm put in the wires.
A light in a box, around 1900. In Kristiania (now Oslo), Kristian Birkeland hung a magnetised sphere, a terrella, in a vacuum chamber and fired electrons at it. Glowing rings appeared around its poles: an aurora in a box, and the idea that particles from the Sun cause the real one.
Québec in the dark, 1989. On 13 March a storm induced currents in Hydro-Québec's long power lines and the grid collapsed in about a minute and a half. Six million people were without power for nine hours.
Starlink, 2022. In February SpaceX launched 49 satellites into a low orbit just as a minor geomagnetic storm warmed and puffed up the upper air. The extra drag brought down 38 of them within days.
Over the Netherlands, 2024. On 10 and 11 May the first G5 storm since 2003 reached Kp 9, and the aurora was seen and photographed all over the Netherlands. It came back strongly on 10 October the same year.
Threads through this room
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