☁️ Convective Cloud Base and Top: Dew-Point Spread, Thermal Ascent and Cumulus Depth Lab
Heat the ground, lift a thermal through a real temperature profile and watch it cool dry-adiabatically, condense at the lifting condensation level and rise as cumulus until it runs out of buoyancy; compare the numerical cloud base with the 125 m per degree rule and Bolton's formula.
Meteorology & Weather Patterns3DModerate60 FPS📱 Mobile-adapted🟠 Blender
⚙ Under the hood
Heat the ground, lift a thermal through a real temperature profile and watch it cool dry-adiabatically, condense at the lifting condensation level and rise as cumulus until it runs out of buoyancy; compare the numerical cloud base with the 125 m per degree rule and Bolton's formula.
Cloud BaseLifting Condensation LevelDew PointConvectionCumulusThree.jsBlender
3D · Three.js / WebGL renderer · 60 FPS target · runs fully client-side, no install