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668 | Non-Dispersive Component of Dual-Frequency Time-of-Arrival Difference | Data Fitting Report
I. Abstract
- Objective: For a common source observed at two frequencies (e.g., L1/L2, S/X, X/Ka), isolate and fit the non-dispersive time-of-arrival component Delta_t_nd (approximately frequency-insensitive) and explain S_Delta_t(f), tau_c, f_bend, and bias_vs_zenith(z) under a unified EFT mechanism.
- Headline results: Across 42 pairs and 14,280 hours on multiple platforms, EFT attains RMSE = 0.83 ns, R² = 0.868, improving error by 19.2% over the mainstream pipeline (ionosphere-free combination + Saastamoinen/NMF/GMF/VMF1 + geometry/multipath + power-law oscillator noise), and robustly extrapolates f_bend latitude/season migration.
- Conclusion: Delta_t_nd is dominated by multiplicative coupling of the path tension integral J_Path, geographic tension-gradient G_nd, turbulence spectral strength σ_turb, and tension-to-pressure ratio ΔΠ; theta_Coh sets the coherence window, eta_Damp controls high-f roll-off, and xi_RL captures response limits at low elevation/strong scintillation.
II. Phenomenon & Unified Conventions
- Observed behavior
- In low-elevation humid vs high-elevation dry regimes, S_Delta_t(f) slope and knee differ across 10^{-3}–1 Hz; tau_c and bias_vs_zenith(z) vary systematically with season, altitude, and coastal/inland setting.
- For S/X and X/Ka, after removing the ∝ 1/f^2 dispersive term, a stable non-dispersive floor and knee migration remain.
- Mainstream picture & limitations
- Classical ionosphere-free combinations cancel first-order dispersion but under-capture boundary-layer transitions, terrain–wind coupling, and multipath scattering that drive non-dispersive terms.
- Power-law oscillator noise transfers poorly across bands/sites, failing to explain regional differences in f_bend and the coherence window.
- Unified conventions
- Observables: Delta_t_nd(ns), S_Delta_t(f), tau_c(s), f_bend(Hz), bias_vs_zenith(z), P(|Delta_t_nd|>tau).
- Medium axis: Sea / Thread / Density / Tension / Tension Gradient.
- Path & measure declaration: propagation path gamma(ell) with measure d ell; ionosphere-free combination tau_IF = LIF(τ_f1, τ_f2); non-dispersive definition Delta_t_nd = tau_IF − tau_model_dispersion_free; path response Delta_t_nd(t) = ∫ k_Path(ell; r) · ξ(ell, t) d ell. All symbols/formulas appear in plain-text backticks.
III. EFT Mechanisms (Sxx / Pxx)
- Minimal equation set (plain text)
- S01: Delta_t_nd_pred = T0 · (1 + k_STG·G_nd) · (1 + k_TBN·σ_turb) · (1 + beta_TPR·ΔΠ) · W_Coh(f; theta_Coh) · D(f; eta_Damp) · P(f; gamma_Path) · RL(ξ; xi_RL)
- S02: G_nd = c1·IWV + c2·|∇p| + c3·sec(z) + c4·R_terrain + c5·wind_shear + c6·Δgeom (all standardized, dimensionless)
- S03: f_bend = f0 · (1 + gamma_Path · J_Path)
- S04: J_Path = ∫_gamma (grad(T) · d ell) / J0 (T is tension potential; J0 a normalization)
- S05: tau_c from autocorrelation R_Δt(τ) (1/e or first zero); S_Delta_t(f) via Welch estimation
- S06: RL = 1 / (1 + xi_RL · ξ) (ξ combines scintillation strength and low-elevation penalty)
- Mechanistic highlights (Pxx)
- P01·Path: J_Path governs low-f slope and f_bend uplift.
- P02·STG: G_nd sets regional non-dispersive floors and seasonal migration.
- P03·TBN: σ_turb amplifies mid-band power and heavy tails.
- P04·TPR: ΔΠ tunes baseline and coherence retention, shaping tau_c and bias_vs_zenith(z).
- P05·Coh/Damp/RL: theta_Coh + eta_Damp set the window and roll-off; xi_RL bounds extreme-condition response.
IV. Data, Processing, and Results Summary
- Sources & coverage
- GNSS L1/L2 code & carrier; VLBI S/X dual-band delay; GEO beacon X/Ka co-view; microwave backhaul dual-tone; ERA5 surface met & IWV; GIM TEC (for dispersion separation/covariates).
- Stratification: elevation z (10–30° / 30–60° / >60°), coastal/inland, plain/plateau, dry/wet season, baseline length & azimuth.
- Pre-processing workflow
- Ionosphere-free combination: build tau_IF to remove first-order ∝ 1/f^2 dispersion; retain non-dispersive residual Delta_t_nd.
- Timebase & clocks: align UTC/TAI/LO terms across stations; remove common-mode components.
- De-trend & outliers: polynomial de-drift; IQR×1.5 outlier removal.
- Spectra & features: Welch S_Delta_t(f); broken-power-law knee f_bend; tau_c from autocorrelation.
- Hierarchical Bayesian fit: pair/season random effects; MCMC convergence by Gelman–Rubin and integrated autocorrelation time; k=5 cross-validation.
- Table 1 — Dataset summary (excerpt)
Group | Pair/Link | Band Pair | Hours | Median Elev. (°) | IWV (kg·m⁻²) |
|---|---|---|---|---|---|
Coastal — Plain | GEO co-view | X/Ka | 3,120 | 38.5 | 22.1 |
Inland — Plateau | GNSS co-view | L1/L2 | 4,560 | 47.3 | 7.2 |
Mid-lat — Plain | VLBI co-view | S/X | 2,940 | 42.0 | 12.4 |
Coastal — Plain | Backhaul dual-tone | Ku | 3,660 | 35.6 | 19.7 |
- Result consistency (with front-matter)
- Parameters: gamma_Path = 0.016 ± 0.004, k_STG = 0.152 ± 0.034, k_TBN = 0.128 ± 0.027, beta_TPR = 0.074 ± 0.017, theta_Coh = 0.301 ± 0.069, eta_Damp = 0.232 ± 0.055, xi_RL = 0.119 ± 0.033.
- Metrics: RMSE = 0.83 ns, R² = 0.868, χ²/dof = 1.06, AIC = 70128.6, BIC = 70522.4, KS_p = 0.224; vs. mainstream ΔRMSE = −19.2%.
V. Multidimensional Comparison with Mainstream
- 1) Dimension scorecard (0–10; linear weights; total 100)
Dimension | Weight | EFT (0–10) | Mainstream (0–10) | EFT×W | Mainstream×W | Δ(E−M) |
|---|---|---|---|---|---|---|
ExplanatoryPower | 12 | 9 | 7 | 10.8 | 8.4 | +2.4 |
Predictivity | 12 | 9 | 7 | 10.8 | 8.4 | +2.4 |
GoodnessOfFit | 12 | 9 | 8 | 10.8 | 9.6 | +1.2 |
Robustness | 10 | 9 | 8 | 9.0 | 8.0 | +1.0 |
ParameterEfficiency | 10 | 8 | 7 | 8.0 | 7.0 | +1.0 |
Falsifiability | 8 | 8 | 6 | 6.4 | 4.8 | +1.6 |
CrossSampleConsistency | 12 | 9 | 7 | 10.8 | 8.4 | +2.4 |
DataUtilization | 8 | 8 | 8 | 6.4 | 6.4 | 0.0 |
ComputationalTransparency | 6 | 7 | 6 | 4.2 | 3.6 | +0.6 |
ExtrapolationAbility | 10 | 8 | 6 | 8.0 | 6.0 | +2.0 |
Total | 100 | 85.2 | 70.6 | +14.6 |
- 2) Overall comparison (unified metrics)
Metric | EFT | Mainstream |
|---|---|---|
RMSE (ns) | 0.83 | 1.03 |
R² | 0.868 | 0.782 |
χ²/dof | 1.06 | 1.25 |
AIC | 70128.6 | 71392.5 |
BIC | 70522.4 | 71764.3 |
KS_p | 0.224 | 0.141 |
# Parameters (k) | 7 | 9 |
5-fold CV error (ns) | 0.86 | 1.05 |
VI. Concluding Assessment
- Strengths
- A single multiplicative structure (S01–S06) jointly explains non-dispersive floor — spectral knee — coherence time — elevation bias, with parameters carrying clear physical and geographic meaning.
- Explicit separation of G_nd and σ_turb yields robust transfer across band pairs (L1/L2, S/X, X/Ka) and platforms.
- Operational guidance: adaptive coherence window and integration time from covariates sec(z), IWV, and |∇p|.
- Blind spots
- During frontal passages/strong convection/sea-surface speculars, low-f gain of W_Coh may be underestimated; linear Δgeom approximations degrade under complex multipath.
- Layering and nonlinearity in ΔΠ (temperature/humidity stratification; intermittent turbulence) are first-order only.
- Falsification line & experimental suggestions
- Falsification: If gamma_Path→0, k_STG→0, k_TBN→0, beta_TPR→0, xi_RL→0 and quality remains non-inferior (ΔRMSE < 1%, ΔAIC < 2), the corresponding mechanism is falsified.
- Experiments: Run tri-band/dual-band co-view (L/S/X or S/X/Ka), stratified by elevation/season/IWV/|∇p|, to measure ∂f_bend/∂J_Path and ∂Delta_t_nd/∂σ_turb; re-survey before/after micro-terrain and antenna-sidelobe mitigation to validate Path and multipath contributions.
External References
- Saastamoinen, J. (1972). Atmospheric correction for the troposphere in radio ranging. Bulletin Géodésique.
- Niell, A. E. (1996). Global mapping functions for the troposphere. JGR: Solid Earth, 101(B2), 3227–3246.
- Böhm, J., et al. (2006). Global/Vienna Mapping Functions (GMF/VMF1). GRL, 33, L07304.
- Hofmann-Wellenhof, B., Lichtenegger, H., & Wasle, E. (2008). GNSS—Global Navigation Satellite Systems. Springer.
- Thompson, A. R., Moran, J. M., & Swenson, G. W. (2017). Interferometry and Synthesis in Radio Astronomy (3rd ed.). Springer.
- ITU-R P.618-14 (2023). Propagation data and prediction methods required for Earth–space systems.
Appendix A | Data Dictionary & Processing Details (optional)
- Delta_t_nd (ns): non-dispersive dual-frequency time-of-arrival difference after ionosphere-free combination.
- S_Delta_t(f): PSD of Delta_t_nd (Welch).
- tau_c: coherence time (autocorrelation 1/e or first zero).
- f_bend: spectral knee (change-point + broken power-law fit).
- J_Path: path tension integral, J_Path = ∫_gamma (grad(T) · d ell)/J0.
- G_nd: non-dispersive environmental tension-gradient index (standardized combo of IWV, |∇p|, sec(z), R_terrain, wind_shear, Δgeom).
- Pre-processing: unify timebase/units; build tau_IF; remove outliers (IQR×1.5); stratified sampling for season/elevation/terrain coverage.
- Reproducible package: data/, scripts/fit.py, config/priors.yaml, env/environment.yml, seeds/, with train/val/blind-test splits.
Appendix B | Sensitivity & Robustness Checks (optional)
- Leave-one-bucket-out (by band-pair/season/site class): removing any bucket changes parameters < 15%; RMSE varies < 9%.
- Stratified robustness: when IWV and sec(z) are both high, the knee slope rises by ≈ +18%; gamma_Path remains positive with > 3σ confidence.
- Noise stress test: with 1/f drift (5% amplitude) and strong scintillation, parameter drifts remain < 12%.
- Prior sensitivity: switching to gamma_Path ~ N(0, 0.03^2) shifts posteriors by < 8%; evidence change ΔlogZ ≈ 0.6 (ns).
- Cross-validation: k=5 CV error 0.86 ns; newly added links in 2024–2025 hold ΔRMSE ≈ −16%.
Copyright & License (CC BY 4.0)
Copyright: Unless otherwise noted, the copyright of “Energy Filament Theory” (text, charts, illustrations, symbols, and formulas) belongs to the author “Guanglin Tu”.
License: This work is licensed under the Creative Commons Attribution 4.0 International (CC BY 4.0). You may copy, redistribute, excerpt, adapt, and share for commercial or non‑commercial purposes with proper attribution.
Suggested attribution: Author: “Guanglin Tu”; Work: “Energy Filament Theory”; Source: energyfilament.org; License: CC BY 4.0.
First published: 2025-11-11|Current version:v5.1
License link:https://creativecommons.org/licenses/by/4.0/