An aurora borealis, also known as the northern lights, is seen in the sky in the early morning hours of April 24, near Washtucna, Wash.

An aurora borealis, also known as the northern lights, is seen in the sky in the early morning hours of April 24, near Washtucna, Wash. / AP

Updated July 12, 2023 at 4:12 PM ET

An updated forecast for this week's northern lights display shows they won't be as visible in the mainland U.S. as previously thought.

A previous forecast by the University of Alaska Fairbanks said the aurora would be visible in more than a dozen states.

The university now says the previous forecast derived from a long-term forecast based on the sun's rotation that went back 54 days. The features it observed on the sun typically last one to three months, which led to its initial report, Rod Boyce, a spokesperson for UAF's Geophysical Institute, said Wednesday.

"However, now that the forecast activity is less than three days in the future, we can see that the solar features that produced the prior activity have actually diminished over the last month," he said.

Geomagnetic storms are classified G1 (minor) through G5 (extreme) on the Kp-index, or planetary index. A G1 storm has a Kp-index of 5, while a G5 storm has a Kp index of 9.

"You really got to get higher levels of storming really to be visible in the U.S., but the G2 prediction has since been degraded down to G1 or less," Bill Murtagh, the program coordinator for the National Oceanic and Atmospheric Administration's Space Weather Prediction Center, said Wednesday.

What happens during a geomagnetic storm?

During the storm, a coronal hole (the spots that appear black on the sun) prompts high winds, which in turn, trigger coronal mass ejections, or CMEs. A CME projects plasma and pieces of the sun's magnetic field into the atmosphere.

"CMEs typically take several days to arrive at Earth, but have been observed, for some of the most intense storms, to arrive in as short as 18 hours," NOAA's Space Weather Prediction Center says.

What is an aurora?

The sun's activity is volatile, and in some cases, the disturbances are so strong they can pull the Earth's magnetic field away from our planet.

But, like a taut rubber band when it's released, the magnetic field snaps back, and the force of that recoil creates powerful ripples known as Alfvén waves about 80,000 miles from the ground. As those waves get closer to Earth, they move faster thanks to the planet's magnetic pull.

Sometimes electrons hitch a ride on these superfast Alfvén waves, reaching speeds as high as 45 million mph as they hurtle downward.

"Think about surfing," Jim Schroeder, an assistant professor of physics at Wheaton College who has led research on the process. "In order to surf, you need to paddle up to the right speed for an ocean wave to pick you up and accelerate you, and we found that electrons were surfing. If they were moving with the right speed relative to the wave, they would get picked up and accelerated."

When the electrons reach Earth's thin upper atmosphere, they collide with nitrogen and oxygen molecules, sending them into an excited state. The excited electrons eventually calm down and release light, which is what we see as the aurora.

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