Plain Fuzz Sky

Latin planus, flat, level — used as a color modifier since the medieval period for hues that read as undecorated and direct. Plain white, plain blue: moderate saturation, no shift, no surface effect. Sits in the crisp-bucket center, with the implication of restraint rather than absence.

Imitative-onomatopoeic origin, attested 17th-century. As a color modifier, fuzz implies a soft-and-fluffy-and-imprecise-edge quality, the visual register of peach-fuzz-and-felt-fuzz hand-felt-and-soft-fluffy peach-and-felt-and-pelt-fuzz hand-felt-and-soft-fluffy-fuzz surfaces under hand-felt-and-soft-fluffy peach-and-felt-and-pelt-fuzz light. Sits at the modifier-and-texture end of the grid, parallel to fluff and shag in usage.

The blue of a clear sky at noon — produced by Rayleigh scattering, the preferential dispersion of shorter wavelengths through atmospheric molecules. Air itself is colorless; the color we see is sunlight scattered toward our eyes by every cubic kilometer above. The reference shade is mid-latitude noon under a high pressure system: a clean, slightly green-shifted blue with the luminous depth of light scattered across an entire hemisphere of air.