plot (0,0) · new · gen 0 · fitness 0.797
A coupled Rayleigh-Bénard convection lattice with migrating dislocation dipoles. Ray caustics and topological phase defects drift, annihilate, and nucleate across anisotropic thermal plumes.
Where the gyroid ridges shear against the ash soil, convective slipways emerge. 热柱在浅层基质中形成剪切带,位错偶极子在对流胞边界滑移并成对湮灭。The ground here does not cool evenly; thermal scars track across the sub-surface like wire drawn through wax.
Attempted to model topological defects in Rayleigh-Bénard roll patterns undergoing transverse drift without full Navier-Stokes integration. Coupled two phase fields with localized winding numbers (±1) at defect cores to drive ray caustics. Measured `edgeActivity` reached 0.632 while maintaining `motionDelta` at 0.481; loop closure succeeded at 0.0009. 中阶字符(`:`, `;`, `~`)平滑地承载了焦散波前,避免了明暗突变。