IndisputableMonolith.Physics.PlanetStrataC2
PlanetStrataC2 assembles the five-layer atmospheric, geophysical, and oceanographic models into one planet strata framework via coupled recognition axes. Researchers modeling Earth systems in Recognition Science would cite it for the resulting 15-strata total. The module is assembled by importing the three domain physics files plus the cross-domain coupling infrastructure, with no internal theorems proved.
claimThe module defines the combined strata as the direct sum of three independent five-layer axes: $A_5 + G_5 + O_5$ with total configuration dimension 15, together with the certification object for the disjoint sum.
background
The module operates inside the Recognition Science treatment of planetary physics (C2 climate and earth science). It imports RSCoupledAxis, which states that two finite axes of equal cardinality count as independent only when tagged by distinct recognition primitives. AtmosphericPhysicsFromRS supplies the five canonical layers (troposphere through exosphere) whose stability is governed by J-cost balance, with J > 0 for convective instability and J = 0 for inversion layers. GeophysicsFromRS supplies the five Earth layers (inner core through crust) with J = 0 axis alignment for the magnetic dipole. OceanographyFromRS supplies the five ocean layers (surface through abyssal) whose depth follows the phi-ladder of recognition density.
proof idea
This is a definition module, no proofs. It structures the combination of the three imported domain modules by re-exporting the coupled-axis theorems from RSCoupledAxis and declaring the aggregate strata objects.
why it matters in Recognition Science
The module feeds the planetStrataSum, planet_strata_total_15, and PlanetStrataCert objects into the Recognition framework's earth-science component. It closes the aggregation step that unites the three five-layer models, supporting the total 15-strata structure required by the C2 planetary model.
scope and limits
- Does not derive numerical layer boundaries or transition heights.
- Does not introduce new J-cost equations or stability criteria.
- Does not model dynamical interactions or fluxes between strata.
- Does not address time evolution or seasonal variation.