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module module high

IndisputableMonolith.Climate.AtmosphericLayeringFromPhiLadder

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This module assigns atmospheric layer boundaries to specific rungs on the Recognition Science phi-ladder. Climate modelers and atmospheric physicists cite it to link the J-cost function and self-similar fixed point to observed tropopause, stratopause, mesopause, and thermosphere altitudes. The module consists of rung definitions, equality lemmas, a strict ordering proof, and altitude formulas derived from the phi-ladder.

claimTropopause rung = 0 (recognition-base altitude); stratopause rung, mesopause lower/upper rungs, and thermosphere rung follow on the phi-ladder with altitude_at_rung(r) = yardstick * phi^{r-8+gap(Z)} in RS-native units.

background

The module imports Constants (providing the RS time quantum τ₀ = 1 tick) and Cost (supplying the J-cost function J(x) = (x + x^{-1})/2 - 1). It operates in the setting of the forcing chain where T5 establishes J-uniqueness, T6 forces phi as the self-similar fixed point, and T7 introduces the eight-tick octave. Rung assignments build directly on the phi-ladder structure for spatial scaling.

proof idea

This is a definition module. It introduces constant rung values for each layer, states equality lemmas (tropopause_rung_eq etc.), proves rung_strict_ordering by direct comparison, and derives altitude_at_rung and altitude_geometric from the phi-ladder formula.

why it matters in Recognition Science

The module supplies the concrete rung-to-layer map that lets the phi-ladder (T6-T8) reach observable climate structure. It feeds downstream climate applications by grounding layer altitudes in the Recognition Composition Law and D=3 spatial dimensions. No parent theorems are listed in the used_by edges yet.

scope and limits

depends on (2)

Lean names referenced from this declaration's body.

declarations in this module (22)