
Mysterious Core Reversal: Eastward Flow Detected Beneath the Pacific
Researchers using ESA Swarm and CryoSat data have traced a dramatic shift in a broad region of molten iron beneath the equatorial Pacific from westward to eastward flow around 2010, challenging the view of a stable outer-core circulation and potentially linking to inner-core changes; the eastward flow has weakened since 2020, and scientists will monitor to determine if this is a temporary fluctuation, part of a cycle, or a new long-term state, with implications for Earth's magnetic field generation (the geodynamo).











