Qualitative Vector Field & Streamline Space
Method: RK4
Climate & Ocean Models
Stommel Ocean Model: x = Temperature diff, y = Salinity diff. Models double-diffusive thermohaline circulation bifurcation.
Simulation & Overlays
Jacobian Matrix & Stability
Local Linearization J(x,y) at Nearest Equilibrium:
∂f/∂x: 0.00
∂f/∂y: 0.00
∂g/∂x: 0.00
∂g/∂y: 0.00
Equilibrium (x*, y*):
(1.000, 1.000)
Trace T = λ1 + λ2:
-1.500
Determinant Δ = λ1·λ2:
0.500
Eigenvalues λ1, λ2:
-1.00, -0.50
STABLE NODE