New analysis reveals why Ganymede has a magnetic field when other moons do not
Ganymede has long looked like a contradiction in orbit. Jupiter’s largest moon is the only moon known to generate its own magnetic field, a trait more commonly associated with planets like Earth and Mercury. But that magnetic shield points to a liquid, churning metal core, and by many formation models, Ganymede should have started out too cold to build one. A new analysis argues that both ideas may be true, at least in part. Instead of forming a metallic core near the beginning of the solar system and slowly cooling ever since, Ganymede may have begun cold and then warmed over billions of years. In that picture, metal inside the moon melted late, sank inward, and may still be feeding the core today. The result is a different kind of dynamo, the deep planetary engine that creates magnetic fields. Possible thermal evolution of Ganymede’s interior based on assumed initial temperatures. (CREDIT: Science Advances) “For decades, studies have progressed in parallel with conflicting assumptions about how Ganymede formed and evolved,” Kevin Trinh lead author from Arizona …









