Snow-crystal DLA growth, glacier dynamics and permafrost thaw span the freezing, cryosphere and climate categories.
Ice is water's slow-motion twin: snowflake/snow-crystal grow by diffusion-limited aggregation, which is why no two are exactly alike; glacier and permafrost move on decade-to-century timescales driven by the same energy-balance physics as earth-energy-balance; and ice-water-density explains the one anomaly that keeps lakes from freezing solid — ice is less dense than liquid water, so it floats and insulates what's below.
Grouped here by theme only; categories and URLs are unchanged.
No. Everything runs entirely in your browser — no downloads, plugins or accounts. Works in Chrome, Firefox, Edge and Safari; most simulations also work on mobile.
No — an element (like fire or water) is a cross-cutting theme. A sim keeps its normal category (e.g. fluid-dynamics, geology) and can also appear on one or more element pages.
Yes — all content is free for educational use under CC BY 4.0. Link to any simulation directly or embed it in your LMS with an iframe.
Because freezing is a phase transition with its own physics — crystal lattice formation, diffusion-limited growth, density anomalies — that behaves quite differently from liquid flow. A handful of sims (like ice-water-density) genuinely bridge both, and carry both tags.
snowflake/snow-crystal realistic?▾Yes — they use diffusion-limited aggregation (DLA), the same growth process real ice crystals follow: water vapour molecules randomly walk through air until they stick to the crystal, and the six-fold symmetry comes from the hexagonal lattice water ice forms.