From Duck Curve to Mars: A Planetary Trend-Detection Analog — and Why Monthly Wind Data Can't Claim Ramp Risk
pvYieldPct = 100 * exp(-0.55 * tau). At the same time, the platform demonstrates scientific falsification honesty by explicitly barring monthly WS2M wind speed (p = 0.4890 in Campinas, 0.1734 in Petrolina, 0.4512 in Manaus) from intra-hour grid-ramp or turbine-gust claims.
1. Why can't monthly NASA POWER wind speed (`WS2M`) support sub-hourly ramp claims?
Direct Answer: Monthly 2m wind averages hide sub-hourly gusts and show zero long-term statistical significance at any Brazilian benchmark station (p > 0.17 everywhere), so claiming battery-dispatch readiness from WS2M would violate empirical validity.
| Station (1984–2025, n = 504) | WS2M Slope / Decade |
95% CI | Seasonal τ | Seasonal p-value | Operational Status in Cockpit-OMNI |
|---|---|---|---|---|---|
| Campinas-SP | -0.0042 m/s/dec | [-0.0191, +0.0103] | -0.021 | 0.4890 | Null — Not supported for hourly ramps |
| Petrolina-PE | -0.0138 m/s/dec | [-0.0433, +0.0168] | -0.042 | 0.1734 | Null — Not supported for hourly ramps |
| Manaus-AM | -0.0007 m/s/dec | [-0.0034, +0.0013] | -0.023 | 0.4512 | Null — Not supported for hourly ramps |
To contrast monthly resolution against high-frequency gust physics, Mission M2 of Rover Pilot 3D pairs the flat monthly WS2M baseline (p = 0.489) with real NASA Mars 2020 MEDA Sol 40 telemetry (19,100 rows: p50 = 2.11 m/s, p99 = 4.11 m/s, max = 5.36 m/s), teaching players why temporal sampling rate determines operational safety. Mission M3 likewise demonstrates deterministic data hygiene by filtering 867 sentinel 999999999.0 values (4.54%) out of the raw MEDA stream.
2. How does the Planetary Context Vector (Θ) unify Earth, Mars, and the Moon?
Direct Answer: Both planetaryPhysics.js and mptoEngine.js execute a single universal transfer physics engine driven by Θ = [g, rho, cpDust, kRegolith, baseTau, albedoIrGain], explicitly labeled PARAMETRIC PHYSICAL MODEL (MPTO) whenever synthetic trajectories are simulated.
| Active World ID | Environment | Gravity g (m/s²) |
Air Density rho (kg/m³) |
Nominal baseTau |
Crater IR Albedo Gain |
|---|---|---|---|---|---|
| earth_ne | Petrolina-PE · Caatinga Solar Corridor | 9.81 | 1.225 | 0.22 | 0.00 |
| earth_se | Campinas-SP · Atlantic/Cerrado | 9.81 | 1.225 | 0.30 | 0.00 |
| earth_am | Manaus-AM · Amazon Basin | 9.81 | 1.225 | 0.35 | 0.00 |
| mars_jezero | Mars · Jezero Crater (MEDA) | 3.71 | 0.020 | 0.60 | 0.04 |
| moon_artemis | Moon · South Pole Crater & Lava Tube | 1.62 | 0.000 (vacuum) | 0.05 | 0.13 |
Inside the 3D simulation and MPTO orchestrator, 64 m retro-rocket impulse-response inversion (grounded in Vizcaino et al., AIAA DOI 10.2514/1.A35748) separates low-slip compact basalt (1.0x Wh/km) from unconsolidated eolian sand traps in Alpha Crater (>= 44% wheel slip, 1.8x Wh/km energy distance), while seven physical agents (Hebe Radiance, Gemini Vision, Sol Invicta, Bios Guardian informed by NASA OSDR OSD-615, Grok Cratera, Storm Watcher fed by NASA DONKI, and Prudence) operate under a deterministic non-LLM Statistical Auditor veto and open feeds from NASA DSN Now and CelesTrak NORAD GP.