CRR Thunderstorm System

Physically Accurate Bidirectional Lightning Attachment
Mathematical Explanation: CRR Framework & Bidirectional Attachment Physics

1. Electric Field Accumulation and Coherence

Atmospheric electric fields accumulate through charge separation processes in thunderclouds. The CRR coherence operator represents this accumulation mathematically.

Classical Atmospheric Physics:
$$\mathbf{E}(x,t) = -\nabla \phi(x,t)$$ $$\frac{\partial \rho}{\partial t} = -\nabla \cdot \mathbf{J}$$ where \(\rho\) is charge density and \(\mathbf{J}\) is current density.
CRR Coherence Mapping:
$$C(x,t) = \int_0^t L(x,\tau) \, d\tau$$ where \(L(x,t)\) represents the local charge accumulation rate:
$$L(x,t) = \mu(x,t) \cdot \sigma(x,t) \cdot \rho_{\text{moisture}}(x,t)$$
Computational Implementation:
L_functional() = moisture × chargeRate × density × ageFactor
C += L_functional() × dt // Euler integration
→ The coherence \(C(t)\) accumulates as clouds develop charge separation through updrafts and ice particle collisions. The functional \(L(x,t)\) encodes moisture content, particle density, and atmospheric conductivity.

2. Critical Breakdown Field and Rupture Threshold

Lightning occurs when the electric field exceeds the dielectric breakdown threshold of air. This is mapped to the CRR rupture condition.

Classical Breakdown Physics:
$$E_{\text{breakdown}} \approx 3 \times 10^6 \, \text{V/m} \, (p/p_0)$$ where \(p\) is atmospheric pressure. Breakdown occurs when:
$$|\mathbf{E}(x,t)| \geq E_{\text{breakdown}}$$
CRR Rupture Mapping:
$$C_{\text{crit}} = \Omega \ln\left(\frac{\Lambda}{\lambda_0}\right)$$ Rupture occurs deterministically when:
$$C(x,t) \geq C_{\text{crit}}$$
Computational Implementation:
C_crit = Omega × log(Lambda / lambda0)
if (cloud.C >= cloud.C_crit) {
  performRupture(); // Deterministic trigger
}
→ The parameters map as: \(\Omega\) ∝ temperature scale affecting ionization rates, \(\Lambda/\lambda_0\) ∝ the ratio of field enhancement factors to ambient conditions. When accumulated coherence exceeds the critical threshold, discharge initiates.

3. Leader Propagation and Field-Guided Pathfinding

Lightning leaders propagate through regions of high field strength, following the path of least resistance. This is implemented through field-based pathfinding.

Classical Leader Physics:
$$\mathbf{v}_{\text{leader}} \propto \mathbf{E}_{\text{local}} + \nabla|\mathbf{E}|$$ Leader steps follow field gradients with stochastic perturbations.
CRR Implementation:
Step selection weighted by:
$$S(x') = \alpha|\mathbf{E}(x')| + \beta C_{\text{field}}(x') + \gamma(y' - y) + \epsilon$$ where \(\epsilon\) represents stochastic branching.
Computational Implementation:
score = fieldAttraction × 0.35 + coherenceAttraction × 0.45
        + groundAttraction × 0.035 + random() × 0.25
nextPos = argmax(score) // Select highest-scoring position
→ Leaders propagate step-by-step through the electric field grid, with each step weighted by local field strength and coherence. Branching occurs probabilistically based on the branching rate parameter.

4. Positive Leaders from Ground

When downward leaders approach the ground, upward positive leaders can emerge from tall objects or field-enhanced points, propagating upward to meet the descending leader.

Positive Leader Initiation:
When downward leader reaches height threshold:
$h_{\text{leader}} \leq h_{\text{threshold}} \approx 100\text{px}$ Positive leader initiates with strong parent-seeking bias:
$S_{\text{up}}(x') = \alpha_p|\vec{r}_{\text{parent}}|^{-1} + \beta|\mathbf{E}(x')| + \gamma C_{\text{field}}(x') + \epsilon$ Maximum propagation: \(\Delta h_{\text{max}} \approx 120\text{px}\)
Computational Implementation:
if (leaderY >= groundLevel - 100 && !hasPositiveLeader) {
  // Probabilistic spawn (60-85% based on proximity & field)
  probability = 0.6 + heightFactor×0.25 + fieldFactor;
  if (random() < probability) createPositiveLeader();
}
// Strong bias toward parent: parentAttraction × 0.6
// Terminates if parent dies or distance > 120px
→ Positive leaders emerge probabilistically (60-85% chance) when downward leaders are within ~100px of ground. Probability increases with proximity and local field strength. They propagate upward with strong attraction to the parent leader's position, creating the classic bidirectional attachment. They terminate if the parent becomes inactive or if they propagate more than 120px without connecting, preventing unrealistic long-distance propagation.

5. Post-Discharge Recovery and Regeneration

After discharge, the atmospheric system recovers through charge redistribution. The CRR regeneration operator weights this recovery by accumulated history.

Classical Recovery:
$$\frac{\partial \mathbf{E}}{\partial t} = -\frac{\mathbf{E}}{\tau_{\text{relax}}} + \mathbf{S}_{\text{source}}$$ where \(\tau_{\text{relax}}\) is the relaxation timescale.
CRR Regeneration Mapping:
$$\mathcal{R}[\chi](x,t) = \int_{-\infty}^t \phi(x,\tau) \exp\left(\frac{C(x,\tau)}{\Omega}\right) d\tau$$ Weight function exponentially amplifies based on prior coherence.
Computational Implementation:
rebirth_integral = 0;
for (hist of C_history) {
  rebirth_integral += exp(hist.C / Omega) × dt;
}
rebirthWeight = rebirth_integral / normalization;
→ After rupture, clouds retain 20% of accumulated coherence as "memory." Future charging is weighted by \(\exp(C/\Omega)\), representing enhanced ionization paths created by prior discharges. This produces the observed tendency for repeated strikes in the same location.

Summary: CRR as a Coarse-Grained Description

The CRR framework provides a coarse-grained mathematical description of thunderstorm electrodynamics. The coherence integral \(C(t) = \int_0^t L \, d\tau\) accumulates charge separation work. The rupture condition \(C \geq C_{\text{crit}}\) represents deterministic breakdown. The regeneration operator \(\mathcal{R} \propto \exp(C/\Omega)\) encodes memory effects in post-discharge recovery. Positive leaders from ground add physical realism to the bidirectional attachment process, spawning probabilistically (60-85% base chance) based on proximity and field strength, with strong parent-seeking behavior and realistic propagation limits.

CRR Core: C(x,t) = ∫₀ᵗ L(x,τ) dτ • Rupture at C ≥ Ω·log(Λ/λ₀) • R[χ] ∝ exp(C/Ω)
Coherence Phase: C(x,t) = ∫₀ᵗ L(x,τ) dτ
Atmospheric coherence building through charge accumulation
// Authentic CRR: C(t) = ∫₀ᵗ L(x,τ) dτ cloud.C += cloud.L_functional() * dt; // Rupture when C >= C_crit if (cloud.C >= cloud.C_crit) rupture();

Coherence Accumulation C(t) vs Critical Threshold C_crit

Max C(t): 0.00
C_crit: 0.00
Ω (scale): 1.00
Λ/λ₀: 10.0
Next Rupture: ---
Phase: Building

CRR Parameters

Ω (Temperature) 1.0
Λ (UV Cutoff) 10.0
λ₀ (IR Scale) 1.0
L Rate 0.15

Lightning System

Branch Rate 0.3
Step Size 8
Positive Leader Prob 60%
Bolt
Sheet
Mixed

Atmospheric System

Wind Speed 0.4
Cloud Formation 0.3

Audio System

Volume 0.7
Reverb 0.6

CRR Status

Phase: Coherence
Clouds: 0
Avg C(t): 0.00
State: Stable

Lightning

Ruptures: 0
Active Leaders: 0
Positive Leaders: 0
Last C at Rupture: ---

Performance

FPS: 0
Audio: Off
Rain Drops: 0
Mode: Bolt
Thunder