Mantle Convection — high-Ra thermal convection L1-286

GeophysicsExtended Boussinesq mantle flowδ=10 · hardL_DAG = 4📋 Stub — not mineable

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Unclaimed Principle — open for contribution

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Forward model E

S t o k es : - g r a d p + d i v (e t a \cdot e p s_{d} o t) = R a \cdot T \cdot g; e n er g y : d T / d t + u . g r a d T = L a pl a c ian T + H

Mantle Convection — high-Ra thermal convection forward model.

L-DAG

L.stokes_infinite_prandtl -> L.energy -> L.rheology -> int.temporal

L.stokes_infinite_prandtlL.energyL.rheologyint.temporal

Well-posedness W

Existence:: true
Uniqueness:: true
Stability:: conditional
κ:: 1600

Chaotic for Ra > 10^7; initial condition of mantle is unknown.

Solvability C

Solver class:: CitcomS, ASPECT, StagYY
Convergence rate q:: 1
Complexity:: O(N log N) per iteration

Specs (0)

No L2 specs registered yet for this principle.