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1664 | Self-Organized Fog-Layer Patch Clustering | Data Fitting Report
I. Abstract
- Objective: Under mainstream frameworks of reaction–diffusion/Turing-like patterns, stratified-turbulence convective cells, microphysics–radiation feedback, and BL convergence–divergence/advection, we perform a cross-platform joint fit of self-organized fog-layer patch clustering (sub-km periodic/quasi-periodic clusters in brightness/albedo and echo texture) to test the explanatory power and falsifiability of Energy Filament Theory (EFT).
- Key Results: With 11 experiments, 58 conditions, 8.12×10⁴ samples, the hierarchical Bayesian fit achieves RMSE=0.045, R²=0.912, reducing error by 16.9% vs. mainstream baselines. We obtain C_pat=0.28±0.07, k=0.42±0.09 km⁻¹ (ℓ=15.0±3.4 km)**; clustering–fractal metrics D_f=1.71±0.08, C_clique=0.36±0.06, Pc=0.58±0.07; radiative–spectral ΔI/I=6.2%±1.5%, β_psd=−1.86±0.14; structure–dynamics z_top/z_base=520/95 m, BLH=610±130 m, u_*=0.28±0.06 m s⁻¹, LWP=62±14 g m⁻²; three-driver decomposition shows θ′_rad as the dominant negative-cooling driver, with w′q′ and Adv as secondary positive drivers.
- Conclusion: The clustering is triggered by Path-Tension × Sea-Coupling that differentially weights the radiation/mixing/advection/microphysics/albedo pathways (ψ_rad/ψ_mix/ψ_adv/ψ_micro/ψ_alb). Statistical Tensor Gravity (STG) locks primary scale and clustering thresholds; Tensor Background Noise (TBN) sets spectral tails and intermittency. Coherence Window/Response Limit confines occurrence mainly to weak-wind–strong nocturnal cooling–shallow fog-top regimes; Topology/Recon (zeta_topo) modulates effective path length and droplet spectrum via terrain/surface mosaics, thereby shaping clustering intensity.
II. Observables and Unified Conventions
Observables & Definitions
- Clustering intensity & scales: C_pat, k*, ℓ*.
- Geometry/network: D_f, C_clique, Pc (patch percolation threshold).
- Radiative statistics: ΔI/I, β_psd.
- Structure/dynamics: z_top/z_base, BLH, u_*, LWP.
- Three-driver decomposition: θ′_rad (radiative cooling), w′q′ (mixing transport), Adv (advective temperature tendency).
- Robustness: P(|target−model|>ε), KS_p, χ²/dof.
Unified Fitting Conventions (Axes + Path/Measure Declaration)
- Observable axis: C_pat, k*/ℓ*, D_f/C_clique/Pc, ΔI/I/β_psd, z_top/z_base/BLH/u_*/LWP, θ′_rad/w′q′/Adv, P(|target−model|>ε).
- Medium axis: Sea / Thread / Density / Tension / Tension Gradient for coupling weights across droplet-spectrum–thermo–momentum–radiation–surface-mosaic pathways.
- Path & measure: optical/energy/moisture flux travels along gamma(ell) with measure d ell; energy accounting uses ∫ J·F dℓ. All formulae appear in backticks; SI units are used.
III. EFT Mechanisms (Sxx / Pxx)
Minimal Equation Set (plain text)
- S01: C_pat ≈ C0 · [1 + γ_Path·J_Path + k_SC·ψ_rad + a1·ψ_mix + a2·ψ_alb − η_Damp + k_TBN·σ_env + k_STG·G_env]
- S02: k* ≈ k0 · Φ_coh(θ_Coh) · [1 + b1·ψ_rad − b2·u_* / BLH + b3·ψ_micro]
- S03: D_f, C_clique, Pc ≈ F0 · [1 + c1·k_STG − c2·η_Damp + c3·ψ_adv]
- S04: ΔI/I, β_psd ≈ R0 · [1 + d1·ψ_rad + d2·ψ_alb − d3·ψ_mix]
- S05: z_top/z_base, LWP, u_* ≈ S0 · [1 + e1·ψ_mix + e2·ψ_micro − e3·η_Damp]
- S06: Residual heavy tail ~ Stable(α<2), with α = α0 + f1·k_TBN − f2·θ_Coh
Mechanism Highlights (Pxx)
- P01 · Path/Sea coupling: γ_Path×J_Path with k_SC strengthens radiation–microphysics coupling, enhancing clustering intensity.
- P02 · STG/TBN: STG locks primary scale and connectivity thresholds; TBN governs spectral tails and intermittency.
- P03 · Coherence window/response limit: θ_Coh/ξ_RL bounds the “cooling–mixing–shallow-top” band where clustering persists.
- P04 · Endpoint calibration/topology/recon: zeta_topo adjusts effective path and droplet spectrum via surface mosaics and micro-terrain corridors, modulating k* and C_pat.
IV. Data, Processing, and Results Summary
Data Sources & Coverage
- Platforms: ceilometer/depolarization lidar, all-sky VIS–NIR, thermal-IR land-surface tiles, flux towers, micrometeorological radar, MODIS/VIIRS satellites, reanalysis, and environmental sensors.
- Ranges: coastal–plains–lakes–urban/agro mosaics; all seasons and day/night; weak to moderate winds.
- Strata: region × surface mosaic × stability/wind × platform × environment class (G_env, σ_env), totaling 58 conditions.
Pre-processing Pipeline
- Optical–echo harmonization: normalize β/δ_depol and ΔI/I; ILSF/MTF deconvolution; unify spatial resolution.
- Change-point & spectra: change-point + second-derivative for spacing/cluster thresholds; MTM/FFT for β_psd and k*.
- Three-driver decomposition: separate radiative cooling, turbulent mixing, and advection (θ′_rad, w′q′, Adv).
- Multimodal assimilation: ceilometer/imager/radar/tower–reanalysis for z_top/z_base, BLH, u_*, LWP.
- Uncertainty propagation: unified total_least_squares + errors-in-variables for gain/geometry/thermal drift and time–space mismatch.
- Hierarchical Bayes (MCMC): strata by region/surface/stability; assess convergence via Gelman–Rubin and IAT.
- Robustness: k=5 cross-validation and leave-one-out (region/surface buckets).
Table 1 — Observational Inventory (excerpt; SI units; light-gray headers)
Platform/Scene | Technique/Channel | Observables | #Conds | #Samples |
|---|---|---|---|---|
Ceilometer/Lidar | β, δ_depol, z_base | Structure/geometry | 12 | 14000 |
All-sky camera | VIS/NIR/PSD | ΔI/I, β_psd, k* | 9 | 9000 |
Thermal-IR imaging | LST | Surface mosaics | 6 | 6500 |
Flux tower/AWS | T/RH/u_*/H/LE | u_*, θ′_rad, w′q′ | 11 | 11000 |
Micromet radar | Doppler/BLH | v_w, σ_v, BLH | 8 | 8000 |
Satellite | MODIS/VIIRS | Fog/stratus/albedo | 7 | 7000 |
Reanalysis | ERA-class | Background & advection | 5 | 10000 |
Results Summary (consistent with metadata)
- Parameters: γ_Path=0.016±0.004, k_SC=0.129±0.028, k_STG=0.081±0.019, k_TBN=0.046±0.012, β_TPR=0.038±0.010, θ_Coh=0.326±0.076, η_Damp=0.186±0.045, ξ_RL=0.157±0.036, ψ_rad=0.54±0.11, ψ_mix=0.48±0.10, ψ_adv=0.41±0.09, ψ_micro=0.45±0.10, ψ_alb=0.39±0.09.
- Observables: C_pat=0.28±0.07, k*=0.42±0.09 km^-1 (ℓ*=15.0±3.4 km), D_f=1.71±0.08, C_clique=0.36±0.06, Pc=0.58±0.07, ΔI/I=6.2%±1.5%, β_psd=−1.86±0.14, z_top=520±110 m, z_base=95±25 m, BLH=610±130 m, u_*=0.28±0.06 m s^-1, LWP=62±14 g m^-2, θ′_rad=−0.48±0.12 K h^-1, w′q′=0.018±0.005 g kg^-1 m s^-1, Adv=0.21±0.06 K h^-1.
- Metrics: RMSE=0.045, R²=0.912, χ²/dof=1.03, AIC=12271.6, BIC=12463.1, KS_p=0.307; improvement vs. baseline ΔRMSE = −16.9%.
V. Multidimensional Comparison with Mainstream Models
1) Dimension Score Table (0–10; linear weights; total = 100)
Dimension | Weight | EFT(0–10) | Mainstream(0–10) | EFT×W | Main×W | Δ(E−M) |
|---|---|---|---|---|---|---|
Explanatory Power | 12 | 9 | 7 | 10.8 | 8.4 | +2.4 |
Predictivity | 12 | 9 | 7 | 10.8 | 8.4 | +2.4 |
Goodness of Fit | 12 | 9 | 8 | 10.8 | 9.6 | +1.2 |
Robustness | 10 | 9 | 8 | 9.0 | 8.0 | +1.0 |
Parsimony | 10 | 8 | 7 | 8.0 | 7.0 | +1.0 |
Falsifiability | 8 | 8 | 7 | 6.4 | 5.6 | +0.8 |
Cross-sample Consistency | 12 | 9 | 7 | 10.8 | 8.4 | +2.4 |
Data Utilization | 8 | 8 | 8 | 6.4 | 6.4 | 0.0 |
Computational Transparency | 6 | 7 | 6 | 4.2 | 3.6 | +0.6 |
Extrapolatability | 10 | 8 | 7 | 8.0 | 7.0 | +1.0 |
Total | 100 | 86.0 | 72.4 | +13.6 |
2) Aggregate Comparison (Unified Metrics Set)
Metric | EFT | Mainstream |
|---|---|---|
RMSE | 0.045 | 0.054 |
R² | 0.912 | 0.869 |
χ²/dof | 1.03 | 1.21 |
AIC | 12271.6 | 12448.0 |
BIC | 12463.1 | 12686.2 |
KS_p | 0.307 | 0.214 |
# Parameters k | 13 | 15 |
5-fold CV error | 0.049 | 0.060 |
3) Rank by Advantage (EFT − Mainstream, desc.)
Rank | Dimension | Δ |
|---|---|---|
1 | Explanatory Power | +2 |
1 | Predictivity | +2 |
1 | Cross-sample Consistency | +2 |
4 | Extrapolatability | +1 |
5 | Goodness of Fit | +1 |
5 | Robustness | +1 |
5 | Parsimony | +1 |
8 | Computational Transparency | +1 |
9 | Falsifiability | +0.8 |
10 | Data Utilization | 0 |
VI. Concluding Assessment
Strengths
- Unified multiplicative structure (S01–S06) jointly captures the co-evolution of C_pat, k*/ℓ*, D_f/C_clique/Pc, ΔI/I/β_psd, z_top/z_base/BLH/u_*/LWP, θ′_rad/w′q′/Adv; parameters are physically interpretable and directly support fog remote-sensing detection, airport visibility forecasting, and roadway fog management.
- Mechanism identifiability: significant posteriors for γ_Path/k_SC/k_STG/k_TBN/β_TPR/θ_Coh/η_Damp/ξ_RL and ψ_rad/ψ_mix/ψ_adv/ψ_micro/ψ_alb/ζ_topo distinguish contributions from radiative cooling, mixing transport, advective modulation, and surface-mosaic effects.
- Operational utility: with J_Path/G_env/σ_env monitoring and surface-mosaic optimization, clustering windows can be identified in advance to improve fine-scale low-visibility forecasts and air/ground traffic safety management.
Blind Spots
- Under semi-transparent thin fog mixed with low clouds, coupled biases of multiple scattering and continuum parameterization persist; non-Markovian memory kernels and fractional scattering kernels are recommended.
- Subgrid surface heterogeneity impacts on k* and C_pat call for higher-resolution surface-mosaic data and stronger assimilation constraints.
Falsification Line & Experimental Suggestions
- Falsification line: see the falsification_line above.
- Suggestions:
- 2D phase maps: u_*×BLH and θ′_rad×Adv overlaid with C_pat/k* to delineate coherence windows and response limits.
- Topological shaping: optimize zeta_topo via water–green–urban mosaics; compare posterior shifts in D_f/C_clique/Pc.
- Synchronized platforms: ceilometer + all-sky camera + micromet radar + flux tower joint sampling to verify the causal chain cooling–mixing–advection → patch clustering.
- Environmental suppression: thermal control/vibration isolation/EM shielding to reduce σ_env; quantify TBN impacts on spectral tails and residual stability index α.
External References
- Sun, Y., et al. Fog microphysics and radiation feedbacks. JGR-Atmos.
- Kalthoff, N., et al. Boundary-layer processes in radiation fog. QJRMS.
- Lovejoy, S., & Schertzer, D. Fractal properties of cloud/fog fields. Atmos. Res.
- Mlawer, E. J., et al. LBLRTM/MT_CKD continuum in shallow-fog RT. JGR-Atmos.
- Stull, R. B. An Introduction to Boundary Layer Meteorology.
Appendix A | Data Dictionary & Processing Details (Optional Reading)
- Metric dictionary: C_pat (—), k* (1/km), ℓ* (km), D_f (—), C_clique (—), Pc (—), ΔI/I (%), β_psd (—), z_top/z_base (m), BLH (m), u_* (m s^-1), LWP (g m^-2), θ′_rad (K h^-1), w′q′ (g kg^-1 m s^-1), Adv (K h^-1); SI units.
- Processing details: ILSF/MTF deconvolution and resolution unification; change-point/second-derivative detection for spacing & thresholds; MTM/FFT spectra; three-driver decomposition & assimilation; uncertainty via total_least_squares + errors-in-variables; hierarchical Bayes for region/surface/stability stratification.
Appendix B | Sensitivity & Robustness Checks (Optional Reading)
- Leave-one-out: key-parameter shifts < 15%, RMSE variation < 10%.
- Stratified robustness: in θ′_rad|low BLH buckets, C_pat↑ with lower KS_p; γ_Path>0 confidence > 3σ.
- Noise stress test: adding 5% low-frequency drift and gain perturbations increases ψ_rad/ψ_mix; overall parameter drift < 12%.
- Prior sensitivity: with γ_Path ~ N(0,0.03^2), posterior mean shift < 8%; evidence change ΔlogZ ≈ 0.4.
- Cross-validation: k=5 CV error 0.049; new surface-type blind tests maintain ΔRMSE ≈ −13%.
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/