Regime
Set by the Ekman number — viscosity against the planet's rotation
Every figure drawn under this hypothesis — 27 of them — with the essay each one belongs to and the generator that drew it.
27 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.
- How long a fluid takes to forget it was not rotating — the same five cases — Ekman spin-up · how-long-viscosity-remembers
- How long a fluid takes to forget it was not rotating — eddy viscosities for the two geophysical cases — Ekman spin-up · how-long-viscosity-remembers
- How long a fluid takes to forget it was not rotating — eddy viscosities used for the ocean and the atmosphere — Ekman spin-up · how-long-viscosity-remembers
- The bath that was only ever a wait — eddy viscosities for the two geophysical cases — Ekman spin-up · how-long-viscosity-remembers
- The bath does not know the hemisphere — f = 4.99e-5 s⁻¹ at 20°, water at 20 °C · rotating-frame
- The bath that was only ever a wait — f = 9.83e-5 s⁻¹ at 42.4°, water at 20 °C · rotating-frame
- How long a fluid takes to forget it was not rotating — 0.1 m deep at one radian a second in water — Ekman number 10⁻⁴ · how-long-viscosity-remembers · hero
- How long a fluid takes to forget it was not rotating — 0.1 m deep at one radian a second in water — Ekman number 10⁻⁴ · how-long-viscosity-remembers
- The drift a rotating planet takes back — deep water, a 8 s swell at latitude 45° — f-plane, eddy viscosity 10⁻⁴ to 1 m²/s · mean-field
- The balance that is its own error — f = 1.03e-4 s⁻¹ at 45°, water at 20 °C · rotating-frame
- The bath does not know the hemisphere — f = 1.03e-4 s⁻¹ at 45°, water at 20 °C · rotating-frame
- The floor that gives the drift back — ν = 0.01 m²/s, 8 s waves, Ekman depth 12.9 m; steady; no-slip floor, stress-free surface, constant eddy viscosity; latitude 55°; no wind · mean-field
- How long a fluid takes to forget it was not rotating — 0.1 m deep at one radian a second in water — Ekman spin-up · how-long-viscosity-remembers
- How long a fluid takes to forget it was not rotating — 0.1 m deep at one radian a second in water unless stated — Ekman spin-up · how-long-viscosity-remembers
- The drift a rotating planet takes back — deep water, a 8 s swell of amplitude 1 m at latitude 45° — rotating frame, inertial period 16.9 h · mean-field · hero
- The drift a rotating planet takes back — deep water, a 8 s swell of amplitude 1 m at latitude 45° — rotating frame, inertial period 16.9 h · mean-field
- The drift a rotating planet takes back — deep water, a 8 s swell of amplitude 1 m at latitude 45° — rotating frame, inertial period 16.9 h · mean-field
- The drift a rotating planet takes back — deep water, a 8 s swell at latitude 45° — f-plane, eddy viscosity 0.01 m²/s · mean-field
- The drift a rotating planet takes back — deep water, a 8 s swell at latitude 45° — f-plane, eddy viscosity 0.001 to 0.1 m²/s · mean-field
- The drift a rotating planet takes back — deep water, a 8 s swell of amplitude 1 m at latitude 5° to 90° — rotating frame, inertial period 12 to 137 h · mean-field
- The drift a rotating planet takes back — deep water, a 8 s swell at latitude 45° — f-plane, eddy viscosity 0.01 m²/s · mean-field
- How long a fluid takes to forget it was not rotating — Ekman number small — latitude 45°, ν = 0.01 m²/s, steady and linear · layer-that-stops
- The layer that stops at a depth — Ekman number small — latitude 45°, ν = 0.01 m²/s, steady and linear · layer-that-stops · hero
- The layer that stops at a depth — Ekman number small — latitude 45°, ν = 0.01 m²/s, steady and linear · layer-that-stops
- The layer that stops at a depth — Ekman number small — latitude 45°, ν = 0.01 m²/s, steady and linear · layer-that-stops
- The layer that stops at a depth — Ekman number small — latitude 45°, steady, constant eddy viscosity · layer-that-stops
- The floor that gives the drift back — steady; no-slip floor, stress-free surface, constant eddy viscosity; latitude 55°; no wind · mean-field