SimAMOC CPU

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Simulation

Max Velocity
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Kinetic Energy
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Step
0
Season
Jan
AMOC
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The Physics

Two-layer ocean model

Surface: dq/dt + J(ψ, q) = curl(τ) − rζ + A∇²ζ
Deep: dqd/dt + J(ψd, qd) = −rdζd + A∇²ζd
Ts: dT/dt = S·cosθ − (A+BT) + κ∇²T

Full equations →

Velocity Profile

Radiative Balance

AMOC Strength

Overturning

Scenarios

AMOC
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Season
Jan

Paint Tools

SimAMOC

Ocean Circulation Simulator
Watch Earth's ocean currents emerge from first-principles physics.

Paint coastlines. Tune climate forcings. Scenarios replay Earth's history.

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