Earth's irregular day length explained by inner core gravitational torque
Research published in Nature found that subtle shifts in the rotational speed of Earth's inner core generate a gravitational torque on the mantle, causing the millisecond-scale variations in the length of Earth's day that have puzzled geophysicists for decades.
- Inner core rotational speed changes of fractions of a degree per year are sufficient to produce measurable day-length variation
- The mechanism links Earth's deep interior dynamics to surface-observable phenomena for the first time in this context
- Findings have direct implications for atomic clock calibration and long-baseline GPS accuracy