OCEAN CURRENTS & TIDES SIMULATION

The Coriolis force does not decide which way your sink drains, but at ocean scale it decides everything: gyres turn clockwise in the Northern Hemisphere and anticlockwise in the Southern, the same mechanism flipped. When the Moon lines up with the Sun, the two tidal pulls add together into spring tides. El Nino and La Nina, meanwhile, shift the whole equatorial warm pool and switch the Peruvian upwelling on and off.

▸ Building the ocean basin & continental shores…
▸ Loading trade winds + the Coriolis force
▸ Starting the gyre & boundary currents
▸ Linking the Moon’s gravity → tides
▸ Calibrating the thermohaline conveyor…
▸ Ready — Online. ✅
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⌂ Earth

Simulation room Ocean Currents & Tides

Ocean & Tides
Online
Coriolis · tides
Moon – Sun – tide
🌙 Tides
aligned → spring tide
Hemisphere—
Rotation—
Wind—
Tide level—
Tide phase—
Note
In the Northern Hemisphere the gyre spins clockwise; in the Southern it spins the other way (the Coriolis force).
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Pick a mode & hemisphere on the right · drag “Moon phase” to toggle spring/neap tides · click a structure for details
The browser has not enabled canvas — the simulation cannot be built.
Tide level over time water level
About Ocean Currents

The Coriolis force does not decide which way your sink drains, but at ocean scale it decides everything: gyres turn clockwise in the Northern Hemisphere and anticlockwise in the Southern, the same mechanism flipped. When the Moon lines up with the Sun, the two tidal pulls add together into spring tides. El Nino and La Nina, meanwhile, shift the whole equatorial warm pool and switch the Peruvian upwelling on and off.

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