Aurora Alert: New Zealand's Magnetometer Network Catches Biggest Storm Since 1994
New Zealand has caught its most violent geomagnetic storm in three decades, thanks to a freshly completed network of magnetic field sensors that went live just in time to witness solar chaos.
The MANA (Magnetometer Array for New Zealand Aotearoa) network, which finished deployment in 2023, recorded a historic geomagnetic storm on May 10-12, 2024. Named the "Gannon" storm, it produced the fastest recorded change in Earth's magnetic field ever observed across New Zealand—a rate of 478 nanoTesla per minute at the Awarua station, shattering the previous record of 191 nanoTesla per minute set in November 2001. For context, Earth's magnetic field normally changes imperceptibly; this storm compressed dramatic shifts into single-minute intervals.
Why This Matters Now
Geomagnetic storms aren't just spectacles for aurora hunters. They degrade GPS accuracy, disrupt power grids, and threaten communications satellites—critical infrastructure that modern economies depend on. The May event hit harder than scientists anticipated, and the MANA network's real-time observations proved essential for understanding how these solar plasma waves interact with Earth's magnetic environment at regional scales.
The timing is significant. Space weather activity follows the Sun's roughly 11-year cycle, which is currently ramping up toward solar maximum (expected around 2025). That means more storms like this are likely coming. MANA's deployment in 2023 positioned New Zealand as a front-row observer for this intensifying period.
A Network Built for the Challenge
MANA consists of five new variometer stations strategically distributed across New Zealand, complementing the existing Eyrewell geomagnetic observatory. The network captures magnetic field data at a standard 1-second cadence, with the ability to stream high-resolution measurements at up to 130 hertz—roughly the same sampling rate as professional audio equipment—for detailed storm analysis.
The October 10-12 geomagnetic storm provided a revealing secondary data point. Though less intense (202 nanoTesla per minute at Awarua), it revealed something unexpected: magnetic responses varied dramatically across the country. While Awarua recorded a sharp spike, the Eyrewell station simultaneously logged only 40 nanoTesla per minute—a five-fold difference across a nation-sized footprint. This spatial variability suggests that local magnetospheric substorms, rather than global planetary effects alone, were driving the observed phenomena. The two storms' peak impacts also lagged the global magnetic maximum by roughly 10 hours, indicating regional atmospheric and plasma dynamics were at play.
Technical Arsenal
The network serves dual purposes: operational monitoring and scientific research. The MANA website (solartsunamis.otago.ac.nz/mana/data/) provides near-real-time storm alerts, enabling utilities and satellite operators to prepare for disruptions. Simultaneously, the raw high-frequency data—available upon request at up to 130 Hz—provides researchers with unprecedented temporal resolution for modeling how geomagnetic storms interact with New Zealand's unique position in the Southern Hemisphere.
What Comes Next
With solar maximum approaching and MANA now battle-tested by historic storms, the network's data will become increasingly valuable for space weather forecasting models. New Zealand's geographic position makes it an ideal observing point for understanding how geomagnetic disturbances propagate across different latitudes. Expect this data to feed into improved early-warning systems for grid operators and satellite operators globally—making this small island nation a critical node in humanity's space weather defense network.






