The European Space Agency is preparing to push its solar storm sentinels ten times farther from Earth, a move that could give power grid operators, satellite controllers and airline dispatchers something they have never had during a major geomagnetic event: hours of warning instead of minutes.
The mission is called HENON and it carries a UK-built magnetometer designed to sense the magnetic structure of incoming coronal mass ejections from roughly 15 million kilometers upstream of Earth. Imperial College London researchers unveiled the completed flight instrument this week at the National Astronomy Meeting in Birmingham.
The stakes are structural. Today’s operational forecasts, drawn from spacecraft at the Sun-Earth L1 Lagrange point 1.5 million kilometers out, give forecasters between 15 and 60 minutes of lead time before a CME strikes. For the fastest storms, that window collapses to about 15 minutes — far short of what utilities say they need to isolate transformers and reroute load.

Why L1 is not far enough
The current 15-minute floor is a geometry problem, not a technology problem. L1 sits where it does because it is a gravitationally stable perch. No sharper sensor at that location can change how long a CME takes to cross the last 1.5 million kilometers.
HENON’s proposed vantage point sits ten times farther upstream, in a Distant Retrograde Orbit — a trajectory first described mathematically by French astronomer Michel Hénon in 1969, from which the mission takes its name. At solar wind speeds of 250 to 3,000 kilometers per second, that extra distance translates into an additional two to three hours of transit time before the storm reaches Earth.
That interval matters because of a physics constraint known as the Bz problem. The north-south orientation of the magnetic field embedded inside a CME is the single dominant factor determining whether an event will be a light show or a grid-wrecker. Bz cannot be inferred from remote imaging or from current models — it can only be measured by an instrument physically inside the cloud.
MAGIC and the miniaturization bet
The magnetometer, called MAGIC, is what makes flying that measurement on a CubeSat feasible. Traditional space-science magnetometers, like those aboard Solar Orbiter and JUICE, use fluxgate sensors that weigh several kilograms and draw significant power. MAGIC uses anisotropic magnetoresistive sensors weighing just 23 grams, mounted on a one-meter deployable boom.
The AMR approach requires roughly ten times less power and mass than fluxgate instruments while still meeting ESA’s space weather monitoring thresholds — sensitivity better than 3 nanoteslas across the 0 to 10 Hz band relevant for detecting Bz swings inside a CME.
This is the fourth generation of the MAGIC design. Earlier versions have flown on the CINEMA CubeSat in 2012 and on RadCube, launched in August 2021. The RadCube instrument was in orbit during the G5 storm of May 2024 — the most intense geomagnetic event in two decades — giving engineers on-orbit performance data under exactly the conditions HENON is being built to detect.
Jonathan Eastwood, the Imperial College London physicist who leads MAGIC, has said HENON will mark the first time the miniaturised instrument flies in deep space to measure the interplanetary magnetic field directly.
A CubeSat doing what CubeSats have not done
HENON is scheduled to launch in early 2027 as a secondary payload on the Ariane 6 rocket carrying ESA’s PLATO exoplanet telescope. After separation, HENON will use a miniaturized radiofrequency ion thruster running on xenon to spiral outward from an L2-bound trajectory and maneuver independently into its operational orbit. The transit is expected to take roughly 14 months.
No prior CubeSat has attempted anything comparable. NASA’s MarCO twins, the first CubeSats to reach interplanetary space, performed only a ballistic flyby of Mars with minor course corrections in 2018. HENON will also be the first CubeSat to operate with an X-band link to ESA’s ESTRACK ground stations at distances ranging from 12 million to 24 million kilometers.
Two other national instruments will fly alongside MAGIC on the platform, contributed by the Czech Republic and Finland, rounding out the spacecraft’s plasma and radiation measurement suite.
The economic case for hours instead of minutes
Power grid managers have said for years that 15 minutes is not enough to execute the most protective actions. Isolating vulnerable transformers, rerouting power flows and reorienting satellites all require preparation windows measured in hours.
The financial argument is well documented. Economic modeling suggests that severe geomagnetic disturbances could cause substantial GDP losses without improved forecasting and grid resilience measures. A major storm could lead to cascading transformer failures with economic damage potentially exceeding $1 trillion.
Historical events have already tested the lower end of that range. In March 1989, geomagnetically induced currents blacked out the entire province of Quebec — roughly 6 million people — for more than nine hours. In October 2003, the Halloween storms caused a roughly 30-hour outage of the FAA’s Wide Area Augmentation System, which provides GPS support to aircraft, and knocked out power to about 50,000 people in Malmö, Sweden. Severe space weather is formally listed on the UK National Risk Register.
Recent events have kept the issue current. A growing body of research suggests the tail risk from extreme storms may be larger than earlier estimates assumed, and the July 4 aurora event this year exceeded NOAA’s forecast by two G-scale levels — a reminder that current predictive tools still miss on severity.
What HENON is really testing
ESA is explicit that HENON is a technology demonstration, not an operational asset. A single spacecraft in a Distant Retrograde Orbit will inevitably drift through geometries where it cannot see incoming storms cleanly. The follow-on concept, called SHIELD, would deploy four to five CubeSats equally spaced along the DRO to provide continuous upstream coverage.
Eastwood has framed the mission’s success as a step change in space weather forecasting, one that would pave the way for SHIELD, a future operational mission under development at ESA.
The institutional logic mirrors how Earth observation and GPS matured — a demonstration mission proves the physics and the platform, then an operational constellation follows. What is different here is scale. HENON’s total mass and power budget are a small fraction of legacy space weather assets like the larger heliophysics spacecraft that have historically monitored the Sun-Earth line.
The forecasting gap that remains
Even if HENON works exactly as designed, the underlying scientific problem does not vanish. Forecasters will still not be able to predict Bz orientation before a CME leaves the Sun. What changes is the moment at which they gain reliable knowledge — from roughly 15 minutes before impact to roughly two to three hours before.
For utilities, that shift is the difference between reactive damage control and pre-positioned defense. For satellite operators managing constellations in low Earth orbit, it is the difference between rushed safe-mode commands and orderly reorientation. For airlines flying polar routes, it is the difference between diverting mid-flight and rescheduling before takeoff.
Space.com has examined how critical infrastructure remains exposed to worst-case space weather, and the operational forecasting community has argued for years that the L1 vantage point is a structural bottleneck.
The MAGIC flight instrument is now complete and headed to Argotec in Italy for integration into the HENON spacecraft. If the schedule holds, the CubeSat will begin its 14-month spiral into deep space early next year. Whether it delivers the promised two-to-three-hour warning window will not be known until it enters its operational orbit and the next major CME crosses its path.