NASA’s
TRACERS (Tandem Reconnection and Cusp Electrodynamics Reconnaissance
Satellites) mission has gathered its first clues to how space weather affects
Earth’s magnetic field. In a new paper, researchers break down how these
interactions work after analyzing initial observations from the first year of
the mission.
The two TRACERS spacecraft launched last year to explore how the Sun’s solar wind
interacts with Earth’s magnetic shield in an explosive process known as
magnetic reconnection. While scientists are familiar with the process of
magnetic reconnection, questions remain on how energy is transferred during the
process and how the edge of Earth’s magnetic field — the magnetopause —
reacts.
“Analyzing the data TRACERS collected gave our team a
clearer view of solar wind particle behavior and how it connects to
reconnection events,” said Stephen Fuselier, TRACERS deputy principal
investigator and instrument lead at the Southwest Research Institute in San
Antonio. “This is an important first step in understanding how magnetic
reconnection works and how these processes can affect Earth.”
Magnetic reconnection occurs when the Sun’s magnetic field, embedded in a continuous outpouring of electrically charged particles called the solar wind, collides with Earth’s magnetic shield, known as the magnetosphere. At the magnetosphere’s boundary with space, called the magnetopause, these collisions cause energy to build up and can cause the magnetic field lines to snap and explosively fling away nearby particles at high speeds directly into our atmosphere.
In this animation, the Sun’s magnetic field collides
with Earth’s, resulting in dayside, or frontside, magnetic reconnection. The
solar wind — waves of charged particles from the Sun traveling at speeds over 1
million miles per hour and shown in orange — push the Sun’s magnetic field
(represented by a vertical orange line) toward a collision course with Earth’s
magnetic field. When the two meet, there’s a tremendous energy release and the
magnetic field lines snap and reconnect, creating new field lines.
NASA’s Goddard Space Flight Center Conceptual Image
Lab
Understanding
what primarily drives the reconnection process — specifically whether the
location of reconnection events influences the magnetopause reaction more than
the rate of reconnection — is a critical initial step. The TRACERS mission was
designed to explore these dynamics by having twin satellites fly one behind the
other, locked in a Sun-synchronous orbit, passing through areas where Earth’s
magnetic field converges like funnels over the north and south magnetic poles.
These areas, called polar cusps, funnel solar wind particles, concentrating the
solar wind particles in a small region of our upper atmosphere. The repeated
orbits through this concentrated region give TRACERS the opportunity to collect
measurements on reconnection events at the southern cusp, allowing scientists
to compare the data between the two satellites and observe how quickly
reconnection changes and evolves.
This animation shows the TRACERS spacecraft as they
enter the polar cusp — a unique region where particles from the Sun are
funneled straight down toward Earth — and where the two spacecraft are
investigating dayside magnetic reconnection. Orange particles and shading
represent an artistic rendering of what flying through the polar cusp would
look like if the region was visible to the naked eye.
NASA’s Goddard Space Flight Center Conceptual Image
Lab
Now,
a year after launch, TRACERS researchers have analyzed the initial data
collected and outlined the results in a new paper published in the Journal of Geophysical Research. The paper discusses
how data taken by the Analyzers for Cusp Ions instruments on the TRACERS
satellites show that magnetic reconnection is largely a spatial process,
meaning where reconnection is occurring is moving, rather than changing in
time. Future measurements will help confirm these results.
According to TRACERS Principal Investigator David
Miles of the University of Iowa, publishing these findings and exploring the
mysteries of magnetic reconnection in the magnetopause is deeply meaningful to
the team. “The TRACERS team has demonstrated exceptional collaboration and
resolve to gather and evaluate this data,” Miles said. “I am excited to see
what is revealed by future measurements.”
After a setback with one of the satellites after launch, the TRACERS team worked
determinedly to re-establish contact with the satellite and establish routine data collection. The TRACERS spacecraft now observe the southern cusp routinely several
times a day. In September, NASA approved a prime mission extension for the
spacecraft to continue studying reconnection events into spring 2027.
This image is one of NASA’s twin TRACERS spacecraft in
low-Earth orbit, captured in August 2025. Images like these give information
about the spacecraft’s orientation and velocity that help analysts understand
how the object is behaving.
Vantor
Understanding
how magnetic reconnection varies helps scientists better understand space
weather, since reconnection provides the fundamental linkage between solar wind
and Earth’s space environment. Studying space weather also helps scientists
better predict geomagnetic storms that can affect the safety of astronauts near
Earth, as well as the power grids and communication systems that we rely
on.
The TRACERS mission is led by David Miles at the University of Iowa with support from the Southwest Research Institute in San Antonio. NASA’s Heliophysics Explorers Program Office at the agency’s Goddard Space Flight Center in Greenbelt, Maryland, manages the mission for the agency’s Heliophysics Division at NASA Headquarters in Washington. The University of Iowa, Southwest Research Institute, University of California, Los Angeles, and University of California, Berkeley, all lead instruments on TRACERS that study changes in Earth’s magnetic field and electric field.
Source: NASA’s TRACERS First Results Offers Peek into Violent Magnetic Process


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