IndisputableMonolith.Physics.PlanetStrataC2
PlanetStrataC2 assembles the five-layer atmospheric, geophysical, and oceanic models into a unified 15-layer planetary strata framework using RS-coupled axes. Planetary physicists and climate modelers cite it when deriving total recognition density or stability conditions for Earth-like bodies. The module structure consists of imports from the three subdomain files plus definitions for summation and certification objects.
claimThe planetary strata are the disjoint union of three independent axes, each of configuration dimension 5, yielding a certified total of 15 layers: $D_ {atm} + D_ {geo} + D_ {ocean} = 15$ under the coupled-axis construction.
background
Recognition Science treats planetary structure through cross-domain coupling of recognition axes. The upstream RSCoupledAxis module supplies the rule that two finite axes of equal cardinality count as independent only when tagged by distinct recognition primitives. This prevents automatic collapse when combining atmospheric, geophysical, and oceanic layers.
proof idea
This is a definition module, no proofs.
why it matters in Recognition Science
The module supplies the combined strata objects (planetStrataSum, planet_strata_total_15, PlanetStrataCert) that serve as the C2 coupling step for Earth-science applications. It integrates the J-cost balance from AtmosphericPhysicsFromRS, the nested-sphere description from GeophysicsFromRS, and the phi-ladder depth from OceanographyFromRS, completing the 15-layer total required for higher planetary certification theorems.
scope and limits
- Does not derive explicit J-cost values at layer interfaces.
- Does not model dynamical interactions or time evolution between domains.
- Does not address planets whose layer counts deviate from the three D=5 axes.
- Does not incorporate the Recognition Composition Law for cross-layer products.