Regime
Set by the buoyancy frequency — stratification against shear or forcing
Every figure drawn under this hypothesis — 61 of them — with the essay each one belongs to and the generator that drew it.
61 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 cascade that arrives as stripes — a barotropic β-plane — no stratification, no forcing scale in the criterion · inverse-cascade · hero
- A cascade that arrives as stripes — a barotropic β-plane — no stratification, no forcing scale in the criterion · inverse-cascade
- A cascade that arrives as stripes — a barotropic β-plane — no stratification, no forcing scale in the criterion · inverse-cascade
- A cascade that arrives as stripes — a barotropic β-plane — no stratification, no forcing scale in the criterion · inverse-cascade
- A cascade that arrives as stripes — a barotropic β-plane — no stratification, no forcing scale in the criterion · inverse-cascade
- A stratified sea blocks a current sooner and traps less — Rossby number small and the hill low against the depth; any stratification B = NH/fa · rotating-frame · hero
- A stratified sea blocks a current sooner and traps less — Rossby number small and the hill low against the depth; any stratification B = NH/fa · rotating-frame
- A stratified sea blocks a current sooner and traps less — Rossby number small and the hill low against the depth; any stratification B = NH/fa · rotating-frame
- A stratified sea blocks a current sooner and traps less — Rossby number small and the hill low against the depth; any stratification B = NH/fa · rotating-frame
- A stratified sea blocks a current sooner and traps less — Rossby number small and the hill low against the depth; any stratification B = NH/fa · rotating-frame
- A stratified sea blocks a current sooner and traps less — Rossby number small and the hill low against the depth; any stratification B = NH/fa · rotating-frame
- A stratified sea blocks a current sooner and traps less — Rossby number small and the hill low against the depth; any stratification B = NH/fa · rotating-frame
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear · stratified · hero
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear · stratified
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear · stratified
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear · stratified
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear · stratified
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear · stratified
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear · stratified
- A wake that sheds its fluid sinks further, and past a point does not stop — stably stratified air, inviscid pair, Boussinesq; N in units of the pair's speed over its spacing · control-volume · hero
- A wake that sheds its fluid sinks further, and past a point does not stop — stably stratified air, inviscid pair, Boussinesq; N in units of the pair's speed over its spacing · control-volume
- A wake that sheds its fluid sinks further, and past a point does not stop — stably stratified air, inviscid pair, Boussinesq; N in units of the pair's speed over its spacing · control-volume
- A wake that sheds its fluid sinks further, and past a point does not stop — stably stratified air, inviscid pair, Boussinesq; N in units of the pair's speed over its spacing · control-volume
- A wake that sheds its fluid sinks further, and past a point does not stop — stably stratified air, inviscid pair, Boussinesq; N in units of the pair's speed over its spacing · control-volume
- A wake that sheds its fluid sinks further, and past a point does not stop — stably stratified air, inviscid pair, Boussinesq; N in units of the pair's speed over its spacing · control-volume
- A wake that sheds its fluid sinks further, and past a point does not stop — stably stratified air, inviscid pair, Boussinesq; N in units of the pair's speed over its spacing · control-volume
- Every unstable wave is inside one circle — a tanh shear layer, unstratified · turbulent-exact
- Every unstable wave is inside one circle — inviscid, unstratified · turbulent-exact
- Five numbers, one name — set by the Richardson number — an energy argument, and not a stability analysis · stratified
- Five numbers, one name — set by the buoyancy frequency — the period is a property of the fluid, not the flow · stratified
- Five numbers, one name — set by the buoyancy frequency — linear, inviscid and non-rotating · stratified
- Five numbers, one name — set by the buoyancy frequency — inviscid, non-rotating, and linear · stratified
- Sufficient, and not necessary — Richardson numbers from 0 to 0.5 — inviscid and non-diffusive · turbulent-exact · hero
- Sufficient, and not necessary — Richardson numbers from 0 to 0.5 — inviscid and non-diffusive · turbulent-exact
- Sufficient, and not necessary — Ri from 0 to 0.2499 · turbulent-exact
- Sufficient, and not necessary — inviscid, non-diffusive, at six Richardson numbers · turbulent-exact
- The number that stops the mixing — set by the buoyancy frequency — linear, inviscid and non-rotating · stratified · hero
- The number that stops the mixing — set by the buoyancy frequency — linear, inviscid and non-rotating · stratified
- The number that stops the mixing — set by the buoyancy frequency — a stratified, inviscid, non-rotating fluid · stratified
- The number that stops the mixing — set by the buoyancy frequency — inviscid, non-rotating, and linear · stratified
- The number that stops the mixing — set by the Richardson number — an energy argument, and not a stability analysis · stratified
- The number that stops the mixing — set by the buoyancy frequency — the period is a property of the fluid, not the flow · stratified
- The number that stops the mixing — set by the buoyancy frequency — linear, inviscid and non-rotating · stratified
- The number that stops the mixing — set by the buoyancy frequency — a stratified, inviscid, non-rotating fluid · stratified
- The number that stops the mixing — set by the Richardson number — an energy argument, and not a stability analysis · stratified
- What holds the shear decides whether the waves last — stratified shear, erf profiles; J the bulk Richardson number · stratified
- At thirty degrees the Earth keeps time with the sea breeze — N = 0.01 per second, H = 1 km · material-loop
- A thin interface keeps its waves past a quarter — inviscid, non-diffusive; Boussinesq; bulk Richardson number J; interface R times thinner than the shear; J = 0.5 · stratified
- What holds the shear decides whether the waves last — stratified shear, J = Δb·δu/U₀²; U₀ 1.5 cm/s, δu₀ 1 cm, R₀ 4, J₀ 0.2 · stratified · hero
- What holds the shear decides whether the waves last — stratified shear, J = Δb·δu/U₀²; U₀ 1.5 cm/s, δu₀ 1 cm, R₀ 4, J₀ 0.2 · stratified
- What holds the shear decides whether the waves last — stratified shear, J = Δb·δu/U₀²; U₀ 1.5 cm/s, δu₀ 1 cm, R₀ 4, J₀ 0.2; shear held · stratified
- What holds the shear decides whether the waves last — stratified shear, J = Δb·δu/U₀²; U₀ 1.5 cm/s, δu₀ 1 cm, R₀ 4, J₀ 0.2; both layers free · stratified
- What holds the shear decides whether the waves last — stratified shear, J = Δb·δu/U₀²; U₀ 1.5 cm/s, δu₀ 1 cm, R₀ 4, J₀ 0.2 · stratified
- What holds the shear decides whether the waves last — stratified shear, J = Δb·δu/U₀²; U₀ 1.5 cm/s, δu₀ 1 cm, R₀ 4, J₀ 0.2 · stratified
- What holds the shear decides whether the waves last — stratified shear, R 2.5, J 0.5 · stratified
- Stable air takes back the momentum a wing pushes down — stably stratified air of buoyancy frequency N; elliptic loading, b₀ = πb/4; a wide-body airliner · control-volume · hero
- Stable air takes back the momentum a wing pushes down — stably stratified air of buoyancy frequency N; elliptic loading, b₀ = πb/4; a wide-body airliner · control-volume
- Stable air takes back the momentum a wing pushes down — stably stratified air of buoyancy frequency N; elliptic loading, b₀ = πb/4; N = 0.01 s⁻¹ · control-volume
- Stable air takes back the momentum a wing pushes down — stably stratified air of buoyancy frequency N; elliptic loading, b₀ = πb/4 · control-volume
- Stable air takes back the momentum a wing pushes down — stably stratified air of buoyancy frequency N; elliptic loading, b₀ = πb/4; N = 0.01 s⁻¹ · control-volume
- Stable air takes back the momentum a wing pushes down — stably stratified air of buoyancy frequency N; elliptic loading, b₀ = πb/4 · control-volume