CRR Atmospheric Molecular Simulation

Coherence • Rupture • Regeneration Framework
CRR Atmospheric Integration: C(x,t) = ∫ L(x,τ) dτ • δ(t-t₀) • R[χ](x,t) = ∫ φ(x->,τ) e^(C(x)/Ω) dτ

Many of our simulations utilise invisible (or visible) atmospheres to integrate the agents. For example, photosynthesising leaves which oxygenate the air, clouds which cohere because of water vapour in the atmosphere. This CRR demonstration aims to visually demonstrate how these coherence functions are utilised, using a highly visual, albeit dramatically rendered, simulation. This also enables real-time quantitative metrics and even LLM derived qualitative statements, depending on the field-state.

CRR Atmospheric Monitor
Field State: Stable
Molecular Count: 0
Diffusion Rate: 0.00
Temperature: 20.0°C
Pressure: 1.013 bar