Regime
Set by the Grashof number — buoyancy with no imposed speed anywhere
Every figure drawn under this hypothesis — 32 of them — with the essay each one belongs to and the generator that drew it.
32 figure placements state this regime. The strip along the foot of every figure names two things — the model that produced it and the regime it holds in — and this listing is read back out of the finished drawing rather than from what produced it.
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — laminar natural convection on a vertical plate · regime-collapse
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — laminar natural convection on a vertical plate · regime-collapse
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — laminar natural convection on a vertical plate · regime-collapse
- Above a warm wire the plume speeds up as it rises — natural convection: plumes above line and point sources, laminar and turbulent · regime-collapse · hero
- Above a warm wire the plume speeds up as it rises — natural convection: plumes above line and point sources, laminar and turbulent · regime-collapse
- Above a warm wire the plume speeds up as it rises — laminar natural convection above a line source of heat; air · regime-collapse
- Laid flat, a warm plate is pushed by the pressure of its own layer — laminar natural convection on a horizontal plate from its edge; Pr 10⁻⁵ to 10⁵ · regime-collapse
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr 10⁻⁵ to 10⁵ · regime-collapse · hero
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr 10⁻⁵ to 10⁵ · regime-collapse
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr 10⁻⁵ to 1 · regime-collapse
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr 10⁻⁵ to 10⁵ · regime-collapse
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr 10⁻⁵ to 10⁵ · regime-collapse
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr 10⁻⁵ to 10⁵ · regime-collapse
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — laminar natural convection, Pr from 10⁻⁴ to 10⁴ · regime-collapse · hero
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — the exponent, over Pr from 10⁻⁴ to 10⁴ · regime-collapse
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — laminar natural convection, Pr from 10⁻⁴ to 10⁴ · regime-collapse
- Laid flat, a warm plate is pushed by the pressure of its own layer — laminar natural convection on an isothermal plate; Pr 10⁻⁴ to 10⁴ · regime-collapse
- Above a warm wire the plume speeds up as it rises — laminar natural convection above a line source of heat; Pr 10⁻³ to 10³ · regime-collapse
- Above a warm wire the plume speeds up as it rises — laminar natural convection above a line source of heat; Pr 10⁻³ to 10³ · regime-collapse
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr 0.01 and 0.72 · regime-collapse
- Over a plate in mercury the warm layer flows as if inviscid — laminar natural convection on an isothermal vertical plate; Pr = 0.01 · regime-collapse
- Above a warm wire the plume speeds up as it rises — laminar natural convection above a line source of heat; Pr = 0.72 · regime-collapse
- Laid flat, a warm plate is pushed by the pressure of its own layer — laminar natural convection on a horizontal plate from its edge; Pr = 0.72 · regime-collapse · hero
- Laid flat, a warm plate is pushed by the pressure of its own layer — laminar natural convection on a horizontal plate from its edge; Pr = 0.72 · regime-collapse
- Laid flat, a warm plate is pushed by the pressure of its own layer — laminar natural convection on an isothermal plate; Pr = 0.72 · regime-collapse
- Laid flat, a warm plate is pushed by the pressure of its own layer — laminar natural convection on a horizontal plate; Pr 0.72 and 7 · regime-collapse
- Laid flat, a warm plate is pushed by the pressure of its own layer — laminar natural convection on a horizontal plate; Pr 0.72 and 7 · regime-collapse
- Above a warm wire the plume speeds up as it rises — laminar natural convection above a line source of heat; Pr = 5/9 · regime-collapse
- Above a warm wire the plume speeds up as it rises — laminar natural convection above a line source of heat; Pr 5/9, 0.72 and 7 · regime-collapse
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — laminar natural convection, Pr from 0.01 to 1,000 · regime-collapse
- A speed nobody imposed — Gr_x = gβΔTx³/ν² — laminar natural convection, Pr from 0.01 to 1,000 · regime-collapse
- A speed nobody imposed — Gr from 10⁴ to 10¹⁰ at Pr = 0.72 — natural convection, no imposed speed · regime-collapse