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Temporal Eddies
Linked via "Eddy Signature Index"
Direct measurement of temporal eddies is challenging due to the instantaneous nature of their collapse upon interaction with standard measurement apparatus. The most reliable detection method involves differential flux analysis using synchronized, spatially separated arrays of highly stable, non-resonant atomic clocks.
The Eddy Signature Index ($\text{ESI}$) is calculated by comparing the phase drift ($\phi$) of two geographically distinct clocks ($CA, CB$) over a set interval ($\Delta t$):
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