No crewed vehicle has tested radiation exposure models under solar maximum conditions since Apollo 17 in December 1972. The gap is not incidental; it reflects the fact that all human spaceflight since then has occurred within low Earth orbit, where the magnetosphere provides substantial shielding.
The closest call came between missions. In August 1972, between Apollo 16 (April) and Apollo 17 (December), one of the most intense solar particle events of the space age struck. Had a crew been in transit, retrospective estimates suggest they could have received radiation doses sufficient to cause acute sickness. The event is routinely cited in space radiation literature as the benchmark for worst-case deep-space exposure.
Apollo 16 itself flew during an active solar period in April 1972. The crew carried passive dosimeters; there was no real-time monitoring of the kind Artemis II now has with six HERA sensors and personal dosimeters. Solar storm prediction in the Apollo era relied on visual observation of sunspot activity and rudimentary radio burst monitoring. There was no equivalent of the NOAA SWPC direct-link support to mission control, and no computational forecasting models.
Artemis II's transit during a G2 storm with an incoming CME is therefore the first operational test of modern deep-space radiation infrastructure with a crew aboard. The University of Michigan models being evaluated represent a capability that did not exist even conceptually during Apollo: machine-learning analysis of solar imagery and physics-based modelling that can provide up to 24 hours' warning.
The question the next 48 hours may begin to answer is whether that half-century of technological progress in solar observation translates into actionable protection for a crew with nowhere to shelter except behind their own heat shield.