Ocean Circulation Inverse Modeling L1-419
Unclaimed Principle — open for contribution
This Principle is declared in the catalog but has no reference solver, no pinned dataset, and is not registered on-chain. There is no reward pool. Submitting a cert against this Principle today will record the cert for reproducibility but pay zero PWM.
To claim it as a Bounty #7 contribution: open a PR adding (1) a reference solver, (2) ≥1 dataset pinned to IPFS, (3) updates to the L3 manifest with dataset CIDs. After verifier-agent triple-review, the founders' 3-of-5 multisig signs PWMRegistry.register() and the Principle becomes mineable.
Forward model E
Ocean Circulation Inverse Modeling: Ocean state estimation: infer 3D temperature, salinity, and velocity fields consistent with all observations (ECCO approach). The forward operator produces the measurement through a 3-node primitive DAG (M.primitive.boussinesq_ocean…); recovery is posed as a nonlinear_inverse problem. Difficulty tier delta=5 with effective condition number kappa_eff~10000.0; forcing_uncertainty, mixing_parameterization_error set the accuracy floor at the Omega boundary. See the forward_model field for the closed-form equation.
L-DAG
Well-posedness W
- Existence:
- true
- Uniqueness:
- true
- Stability:
- conditional
- κ:
- 10000000
Existence of the recovered 3D_ocean_state is guaranteed within the declared Omega bounds. Uniqueness holds on the measurement-supported subspace; out-of-support modes are controlled by declared priors. Stability is conditionally stable (kappa_eff ~= 10000.0); forcing_uncertainty dominates the stability cliff; the remaining mismatch parameters contribute higher-order bias terms. Observation gaussian sets the irreducible data-fidelity floor.
Solvability C
- Solver class:
- classical [adjoint_4DVar_ECCO or EnKF_ocean]
- Convergence rate q:
- 1.5
- Complexity:
- O(N_iter * N_OGCM_calls) per optimization with N_OGCM = 20-year forward+adjoint per iteration