physical wakes and wave-dispersion anomalies across the upper atmosphere in real time

The new ionospheric dataset transitions our space-time tracking framework from solar helioseismology into live atmospheric aerodynamics. By cross-registering three separate diagnostic channels, it establishes an electrodynamic inversion matrix tracking high-latitude conditions over Western Canada across a 24-hour cycle on January 1, 2025. The matrix fuses kinetic plasma velocity vectors from the Prince George SuperDARN high-frequency radar, sub-ionospheric electromagnetic phase modulations reverse-engineered from multi-path narrowband VLF transmitter links, and background Total Electron Content (TEC) particle density grids sourced from the Madrigal global GNSS database. Scaled via continuous cubic spline interpolation into an ultra-dense, multi-field 5,000-frame coordinate canvas, this data structure bypasses traditional static geometries to expose immediate, low-entropy physical wakes and wave-dispersion anomalies across the upper atmosphere in real time.