IndisputableMonolith.Physics.AtmosphericPhysicsFromRS
This module defines atmospheric physics in Recognition Science by declaring equilibrium at J=0. It introduces types for discrete layers and phenomena plus a certification object, all built on the imported Cost framework. Planetary modelers cite it when assembling the three-stack strata decomposition of a planet. The module contains only definitions and no proofs.
claimAtmospheric equilibrium holds when $J=0$. AtmosphericLayer is the type of a discrete layer satisfying this condition; AtmosphericPhysicsCert certifies that the layer physics follows from the J-cost axioms.
background
Recognition Science starts from the J-cost functional equation in the Cost module, where J(x) satisfies the composition law J(xy) + J(x/y) = 2J(x)J(y) + 2J(x) + 2J(y) and equilibrium is the fixed point J=0. This module applies that setting to the atmosphere as one of three independent 5-strata stacks. It declares AtmosphericLayer, atmosphericLayerCount, WeatherPhenomenon, weatherPhenomenonCount, atmospheric_equilibrium, and AtmosphericPhysicsCert to encode the J=0 condition for atmospheric strata.
proof idea
This is a definition module, no proofs.
why it matters in Recognition Science
The module supplies the atmospheric 5-stratum stack required by the downstream PlanetStrataC2 declaration of the planetary 15-stratum direct sum (atmosphere + solid Earth + ocean). It therefore closes the atmospheric equilibrium step that feeds the larger Recognition Science derivation of planetary structure from the J-cost and the phi-ladder.
scope and limits
- Does not assign numerical thicknesses or pressures to layers.
- Does not derive radiative or chemical transport equations.
- Does not prove stability of the J=0 state beyond the declaration.