Humidifier (Cold Mist)
Two large cold humidifiers combined ≈ 30–60 L/day.
Cold mist (2–35 °C). Boiled-then-cooled water at 18 °C; no thermal lift, no buoyancy-driven updraft.
Hygroscopic GCCN. Activates at s ≈ 0.05% per Borys/Ayala.
Your claim: boiled-water mist is way more effective. 10× = plausible; 100× = ultrasonic nano regime.
Atmosphere
Sahara ground RH 10–30%.
Pre-existing moisture at altitude. Higher = closer to needing only CCN trigger.
v3 cap at 5 (was 10 → caused CFL overflow). Stable at all values.
Without updraft the GCCN never reach cloud-base altitude.
Network Seeding (Compare)
✓ CFL stability restored · D ≤ 0.18 · two-sided clamp on source + final bounding pass · peak HR ∈ [0%, 100%] provably.
ODE-CCT Real-time Metrics
Mass Flux Ratio (kg/s ÷ 1 km²)
9.7 × 10⁻¹⁴
Raw water flux vs air column. Underscaled by ~10¹³× for 1 km² single-source.
Peak Local RH
15.0%
max single-cell humidity — provably bounded to [0%, 100%] by v3 patch
CCN Density (local, cm⁻³)
120/cm³
count of hygroscopic nuclei · >10³/cm³ needed for cloud modification
Droplet Settling Lifetime
30.0d
Stokes settling timescale. r_d ∝ 1/√efficiency
Network Density (100 km⁻²)
0units
Operational ground seeding needs ≥ 100/km² · aircraft = ~0.001/km²
Rain Probability / hr
0.00%
P(rain) given: P(lift) × P(CCN to LCL) × P(supersat aloft) × efficiency
Collapse Verdict (Cold-Mist Corrected)
Child
HighSch
Uni
Expert
Verdict