Radiative imbalance with the sky → Light
Radiative imbalance with the skyRadiative sky coolingTemperature gradientThermal emissionLight
Epistemic state of the route
- known constituent relations
- 4 / 4 established or replicated · weakest constituent replicated
- constituent maturity floor
- K4 · experimentally observed
- search for this exact route
- Not assessed — complete composition not searched.
- recorded-pathway overlap
- shares its closing relations with Incandescent lamp · 2/4 relations shared
- route-level evidence
- 0 sources for the complete composition · 6 cited by the constituent steps
- boundaries and interfaces
- BOUNDARY compatible · no region transition
Explorematrix context · physics checks · steps · route evidence · constituent evidence · cite
Matrix context
D = disequilibrium row · C = coupling family column. A cell reads the state of the atlas for that pair.
D.12 × C.20 · Radiative imbalance with the sky × Photothermalfamily: PhotothermalD.12 × C.07 · Radiative imbalance with the sky × Thermophotovoltaicfamily: Thermophotovoltaic
Typed bounds on this route
Every limit the atlas holds for this route, as constraint records: reached through bounded_by claims on the route's own entities. Hard bounds (an upper bound or a formula) decide the thermodynamic-bound check above; benchmarks, constitutive relations and resource limits are listed and never decisive. No prose limit exists anywhere (pass 42).
- Radiative cooling power bound · resource-bound · listed, never decisivenet cooling power ≲ 100–150 W/m² under a clear sky
- Carnot limit · formula-bound · hard, filtered out by its applicabilityη ≤ 1 − T_c/T_h for any heat engine between reservoirs at T_h and T_c
- Visible-band fraction of thermal emission · formula-bound · hard, applies to this routeη_vis ≤ ∫₃₈₀ⁿᵐ⁷⁸⁰ⁿᵐ B_λ(λ, T) dλ / σT⁴ — the share of a thermal emitter's radiated power that Planck's distribution places in the visible band at the emitter temperature
Steps
- 01radiative → thermal
- an emitter with high emissivity in the 8–13 µm window and high solar reflectance
- a clear sky; humidity and cloud close the window
refs [1] [2] [3] - 02thermal → thermal
- the cooled surface sits a few kelvin below ambient air
refs [1] [4] [3] - 03thermal → radiative
- an emitter hotter than the surface it faces
refs [5] [6] - 04radiative → radiative · loss to radiative
- incandescence at > 2000 K
refs [6] [5]
Evidence for the complete composition · 0
No source on record for this exact composition. The sources below support the individual steps, not the route as a whole.
Evidence for the constituent relations · 6
- [1]A. P. Raman et al.. Passive radiative cooling below ambient air temperature under direct sunlight (2014)
- [2]Y. Zhai et al.. Scalable-manufactured randomized glass-polymer hybrid metamaterial for daytime radiative cooling (2017)
- [3]J.-l. Kou et al.. Daytime radiative cooling using near-black infrared emitters (2017)
- [4]A. P. Raman, W. Li, S. Fan. Generating light from darkness (2019)
- [5]A. Bejan. Advanced Engineering Thermodynamics (4th ed.) (2016)
- [6]P. T. Landsberg, G. Tonge. Thermodynamic energy conversion efficiencies (1980)
Cite this route
Physical Transformation Atlas (2026). route p-fa2d6049a4: Radiative imbalance with the sky → Radiative sky cooling → Temperature gradient → Thermal emission → Light. Dataset revision rbfbfcbb70e57 (hash of the canonical data). https://physical-transformation-atlas.wldud5192.workers.dev/path/fa2d6049a4
Ids and matrix addresses are stable across revisions; the revision hash identifies the exact canonical files the record was compiled from and is meta.data_hash in every /api export. Reuse terms: see the license field in any export.