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As
this month's string of powerful X-class solar flares sparked brilliant auroras
that lit up skies across an unusually wide swath of the globe—from northern
Europe to Florida—researchers at NJIT's Center for Solar-Terrestrial Research
(CSTR) captured a less visible, but crucial, record of the storm's impact on
Earth's upper atmosphere.
Recent measurements recorded by NJIT's
new network of radio telescopes show how a rare sequence of intense flares from
Nov. 9–14, including an X5.1 event marking 2025's strongest flare so far,
jolted the ionosphere—the plasma-filled atmospheric layer essential for radio
signals, GPS accuracy and satellite orbits.
The flares triggered R3 (strong) radio
blackouts across Africa and Europe, with several coronal mass
ejections (CMEs) fueling
a major geomagnetic storm and aurora at unusually low latitudes.
The cluster of explosive events
originated from a single active region on the sun, AR4274.
"It's somewhat unusual to see four
X-class flares in just a few days from the same region," said Bin Chen,
NJIT-CSTR professor of physics and director of the Expanded Owens Valley Solar
Array (EOVSA). "An X1.7 flare on Nov. 9, an X1.2 on Nov. 10, an X5.1 on
Nov. 11 and an X4.0 on Nov. 14—that's a very productive stretch. What really
stood out were the ripple effects right here on Earth."
Though the flares occurred during nighttime in California—out of view of NJIT's Big Bear Solar Observatory—the center's radio telescopes at the Owens Valley site in the Eastern Sierra recorded the flares' aftermath and their disturbances in real time.
OVRO-LWA
radio data contrasts a quiet day (Sept. 29, 2025) with the hours after the
X1.7-class flare recorded at 2:35 ET on Nov. 9. The type III radio bursts,
shown in the radio dynamic spectrum (horizontal axis is UT time, vertical axis
is frequency), appear nearly vertical bursts during stable ionospheric
conditions. After flare-driven X-ray and UV radiation ionized the lower
ionosphere and geomagnetic storms driven by the associated coronal mass
ejections, these radio bursts became curved and chaotic, particularly at low
frequencies (bottom of the plot). Credit: NJIT/OVSA Team
Tracking the flares' atmospheric effects
EOVSA and the newly operational
Long Wavelength Array at Owens Valley Radio Observatory (OVRO-LWA) tracked
dramatic atmospheric changes across a broad range of radio frequencies—from
microwaves observed by EOVSA (similar to those used in satellite communications
and Wi-Fi) down to the meter- and decameter waves captured by OVRO-LWA (similar
to FM radio frequencies).
"Normally, OVRO-LWA radio data
often show neat, nearly vertical bursts known as type III radio bursts,"
said Chen. "After these flares, these bursts are curved and chaotic at low
frequencies—a clear sign the ionosphere had been disturbed."
For ionospheric scientists, the
event was nearly as striking as the aurora.
"This storm was an excellent
reminder that Earth is part of a much larger cosmic system," said Lindsay
Goodwin, NJIT-CSTR assistant professor of physics and ionosphere expert.
"Not all extreme solar activity leads to a geomagnetic storm—sometimes the
material misses Earth. But in this case, it hit."
The result was a G4 geomagnetic
storm on NOAA's five-point
scale.
"The Dst index, which measures
how much Earth's magnetic field is compressed by the solar wind, plunged from
about –40 nT to nearly –250 nT in just a few hours," Goodwin said.
"That's a huge shock to our planet's magnetic defenses."
Impact on technology and research advances
Charged particles raining into the
atmosphere produced auroras, and this event was extreme enough to push aurora
far beyond their usual range, with sightings reported as far south as Florida.
"My aurora chat group was
exploding with images from places that almost never see northern lights,"
Goodwin said.
The episode also demonstrated the
growing capability of NJIT's radio observatories. OVRO-LWA recently entered
full solar-science operations, opening a new window into the sun's "middle
corona"—a region from about 1.5–10 solar radii where magnetic fields
restructure and CMEs accelerate.
OVRO-LWA and EOVSA now operate
together as an integrated community radio facility dedicated to solar and space
weather research, referred to as the Owens Valley Solar Arrays (OVSA).
"This dataset is new by
itself," said Chen. "OVRO-LWA complements EOVSA perfectly. Together,
they let us follow space-weather effects from their origin in the solar corona
all the way to their impact on Earth's upper atmosphere."
Goodwin's team, with help from NJIT
undergrad Jeremy McLynch, recently added another dimension to the analysis.
Over the summer, their team
deployed a high-precision GPS receiver beside the OVRO-LWA—nicknamed FLUMPH
(Field-deployed L-band Unit for Monitoring Phase Hiccups), after the popular
Dungeons & Dragons creature it resembles.
The device captures real-world
disruptions to satellite-navigation signals during solar storms.
"Plasma irregularities caused
by solar and geomagnetic activity disrupt radio and GPS communication,"
Goodwin said. "Pairing GPS measurements with the LWA data lets us see both
sides of the story—how the sun shakes the ionosphere, and how that affects the
technologies we rely on daily."
Looking ahead to future solar storms
For now, both Chen and Goodwin say
the space weather research community is still unpacking the storm's full
impact. With the sun near the peak of its 11-year activity cycle, Goodwin says
similar storms are possible near-term.
"Scientists are only beginning
to understand the full effects of this storm," Goodwin said.
"Historically, extreme solar and geomagnetic events can disrupt power
grids, interfere with radio communications, and threaten the safety and operation
of satellites and spacecraft. We've seen several major storms recently, because
the sun is still near the peak of its 11-year cycle.
"Such events will become less common as the sun quiets down, but they will return in roughly 11 years—and when they do, understanding them will be even more important as we rely more on space technology and venture farther into space."
Provided by New Jersey Institute of Technology
Source: Scientists track recent solar flare disruptions in Earth's ionosphere


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