Lightning's Impact on Space Weather

Lightning's Impact on Space Weather

'Killer electrons': Lightning storms play cosmic pinball with space weather

Lightning strikes kick off a game of electron pinball in space
Visualization showing how magnetic field lines, thin cyan lines, circling Earth can trap charged particles, thin yellow lines. Credit: UCLA EPSS/NASA SVS

When lightning strikes, the electrons come pouring down. In a new study, researchers at the University of Colorado Boulder, led by an undergraduate student, have discovered a novel connection between weather on Earth and space weather. The team utilized satellite data to reveal that lightning storms on our planet can dislodge particularly high-energy, or "extra-hot," electrons from the inner radiation belt—a region of space enveloped by charged particles that surround Earth like an inner tube.

Researcher Affiliation Role
Max Feinland University of Colorado Boulder Lead Author
Lauren Blum University of Colorado Boulder Co-author
Robert Marshall CU Boulder Co-author
Longzhi Gan Boston University Co-author
Mark Looper The Aerospace Corporation Co-author

The team's results could help satellites and even astronauts avoid dangerous radiation in space. This is one kind of downpour you don't want to get caught in, said lead author and undergraduate Max Feinland.

"These particles are the scary ones or what some people call ','" said Feinland. "They can penetrate metal on satellites, hit circuit boards and can be carcinogenic if they hit a person in space."

The study appeared on October 8 in the journal Nature Communications.

The findings cast an eye toward the radiation belts, which are generated by Earth's magnetic field. Lauren Blum, a co-author of the paper and assistant professor in the Laboratory for Atmospheric and Space Physics (LASP) at CU Boulder, explained that two of these regions encircle our planet: While they move a lot over time, the inner belt tends to begin more than 600 miles above the surface. The outer belt starts roughly around 12,000 miles from Earth. These pool floaties in space trap charged particles streaming toward our planet from the sun, forming a sort of barrier between Earth's atmosphere and the rest of the solar system.

Radiation Belt Height from Earth Surface Features
Inner Radiation Belt 600 miles Contains high-energy particles, relatively stable
Outer Radiation Belt 12,000 miles More dynamic, subject to changes due to solar activity

But they're not exactly airtight; scientists have long known that high-energy electrons can fall toward Earth from the outer radiation belt. Blum and her colleagues, however, are the first to spot a similar rain coming from the inner belt.

Earth and space, in other words, may not be as separate as they look.

"Space weather is really driven both from above and below," Blum said.

Bolt from the Blue

It's a testament to the power of lightning. When a lightning bolt flashes in the sky on Earth, that burst of energy may also send spiraling deep into space. If those waves smack into electrons in the , they can jostle them free—a bit like shaking your umbrella to knock the water off. In some cases, such "lightning-induced electron precipitation" can even influence the chemistry of Earth's atmosphere.

To date, researchers had only collected direct measurements of lower energy, or "colder," electrons falling from the inner radiation belt.

"Typically, the inner belt is thought to be kind of boring," Blum said. "It's stable. It's always there."

Visualization of the radiation belts surrounding Earth
Credit: NASA

Her team's new discovery came about almost by accident. Feinland was analyzing data from NASA's now-decommissioned Solar, Anomalous, and Magnetospheric Particle Explorer (SAMPEX) satellite when he saw something odd: clumps of what seemed to be high-energy electrons moving through the inner belt.

"I showed Lauren some of my events, and she said, 'That's not where these are supposed to be,'" Feinland said. "Some literature suggests that there aren't any high-energy electrons in the inner belt at all."

The team decided to dig deeper.

In all, Feinland counted 45 surges of high-energy electrons in the inner belt from 1996 to 2006. He compared those events to records of lightning strikes in North America. Sure enough, some of the spikes in electrons seemed to happen less than a second after lightning strikes on the ground.

Event Type Count of Events Timeframe
High-energy electron surges 45 1996 to 2006

Electron Pinball

Here's what the team thinks is happening: Following a lightning strike, radio waves from Earth kick off a kind of manic pinball game in space. They knock into electrons in the inner belt, which then begin to bounce between Earth's northern and southern hemispheres—going back and forth in just 0.2 seconds.

And each time the electrons bounce, some of them fall out of the belt and into our atmosphere.

"You have a big blob of electrons that bounces, and then returns and bounces again," Blum said. "You'll see this initial signal, and it will decay away."

Blum isn't sure how often such events happen. They may occur mostly during periods of high solar activity when the sun spits out a lot of high-energy electrons, stocking the inner belt with these particles.

The researchers want to understand these events better so that they can predict when they may be likely to occur, potentially helping to keep people and electronics in orbit safe.

Feinland, for his part, is grateful for the chance to study these magnificent storms.

"I didn't even realize how much I liked research until I got to do this project," he said.

Further Research Directions

With insights gained from this study, future research may focus on the following areas to better understand the implications of lightning-induced electron precipitation:

  • Longitudinal studies to assess frequencies of such electron surges over different solar cycles.
  • Geographic studies to compare data from different regions based on lightning activity.
  • Technological assessments of satellite shielding against high-energy electrons.

This innovative research provides a striking reminder of the interconnectedness of weather systems on Earth and their cosmic counterparts. Such revelations could greatly improve our capabilities to predict, protect, and advance our understanding of both terrestrial and space weather phenomena.

For more information, refer to the following:

Universetoday reference

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