Pacific Core-Flow Reversal Signals a More Dynamic Geodynamo
A broad region of liquid iron beneath the equatorial Pacific flipped from westward to eastward flow around 2010, revealing the outer core can change circulation more abruptly than previously thought. Using nearly 30 years of data from ground observatories plus ESA Swarm, CryoSat, CHAMP and Ørsted satellites, researchers traced how this flow reversal reshapes our view of the geodynamo and Earth's magnetic field. The finding raises questions about core–mantle–inner-core interactions and whether such reversals are temporary fluctuations or part of a longer cycle, underscoring the need for ongoing monitoring.
