IndisputableMonolith.Physics.AtmosphericPhysicsFromRS
The module derives atmospheric equilibrium in Recognition Science by setting the J-cost to zero. Researchers modeling planetary strata would cite it when assembling the atmosphere component of the 15-stratum decomposition. The module supplies definitions for layers and phenomena together with a certification that equilibrium holds precisely when J vanishes.
claimAtmospheric equilibrium holds when the J-cost satisfies $J=0$. The module defines AtmosphericLayer, WeatherPhenomenon, atmosphericLayerCount, weatherPhenomenonCount, atmospheric_equilibrium, AtmosphericPhysicsCert and atmosphericPhysicsCert.
background
The module imports IndisputableMonolith.Cost, which supplies the J-cost functional whose vanishing defines equilibrium. It introduces the sibling definitions AtmosphericLayer (a discrete layer in the atmosphere), WeatherPhenomenon (observable events), and the associated counting functions. The local theoretical setting is the extraction of atmospheric physics directly from the Recognition Science forcing chain, with equilibrium stated as J=0.
proof idea
This is a definition module, no proofs. It assembles type declarations for layers and phenomena, counting functions, an equilibrium predicate, and a certification record whose body is the statement that J vanishes.
why it matters in Recognition Science
The module supplies the atmospheric stack required by the downstream C2 theorem in PlanetStrataC2, which decomposes the planet into three independent 5-stratum direct sums (atmosphere, solid Earth, ocean). It therefore occupies the atmospheric-equilibrium slot in the Recognition Science derivation of planetary structure.
scope and limits
- Does not derive dynamical equations of motion.
- Does not treat non-equilibrium or time-dependent states.
- Does not compute numerical values for layer thicknesses.
- Does not address coupling to solid-Earth or ocean strata.