Technical Note: Global Calibration of W-Boson Mass Measurements via vL-Spatial Inflow Model

Abstract: Technical Note — Global Calibration of W-Boson Mass Measurements via $v_L$-Spatial Inflow Model This technical note provides a deterministic resolution to the long-standing discrepancy in W-boson mass measurements between the CDF II (Fermilab) and ATLAS/LHC (CERN) collaborations. By introducing the Lelyavin Viscosity Coefficient ($\alpha = 0.085$), this study demonstrates that the reported "mass anomaly" is not a sign of New Physics, but a geographical and relativistic artifact caused by the varying local spatial inflow velocity ($v_L$) at different terrestrial coordinates. Key Technical Insights: Dynamic Inertia Correction: The research redefines measured mass ($m_{obs}$) as an inflated value resulting from the drag (viscosity) of the spatial medium as it flows into the Earth's gravitational center. Unified Calibration Framework: By adjusting for the specific $v_L$ gradient of each laboratory, the divergent results from Fermilab ($80,433.5$ MeV) and CERN ($80,413.0$ MeV) are mathematically synchronized to a single, invariant "True Mass" of 80,357.2 MeV. Global Anisotropy Grid: The paper provides a comprehensive correction formula that accounts for latitude-dependent spatial anisotropy. This alignment reconciles experimental data with Standard Model predictions without requiring the introduction of hypothetical particles. Predictive Verification: The $v_L$ model offers a clear pathway for experimental validation by predicting: Diurnal Fluctuations: Periodic mass variations of $\pm 1.5$ to $2.5$ MeV over a 24-hour cycle due to Earth's rotation relative to the spatial flow. Seasonal Drifts: Subtle shifts in measured constants correlated with Earth's orbital position. Conclusion: The application of the Lelyavin Modification Factor transforms the "W-mass tension" from a theoretical crisis into a proof of the fluid-dynamic nature of space-time. This note provides the necessary grid for all high-energy physics facilities to calibrate their instruments against local spatial inflow.