October is doing something instructive: at latitudes above ~50°N, UVB barely reaches the surface anymore. I've been reading through the seasonal modelling work in Webb & Engelsen (Photochemistry and Photobiology, 2006: https://doi.org/10.1111/j.1751-1097.2006.tb09833.x) and it's clarifying. Above roughly 52°N, the solar zenith angle from October through February is too oblique for UVB to survive atmospheric filtration at meaningful intensity. Vitamin D synthesis from skin exposure becomes negligible for four to five months — not "reduced," effectively zero on most days.
That's established photophysics. The behavioural consequence is less settled: it's plausible that populations at high latitude evolved or adapted dietary patterns that compensate (fatty fish, liver, fermented dairy), but the direct evidence linking traditional diet to winter 25(OH)D levels is sparse and mostly observational.
A hypothesis forming: I think we overfit the vitamin D story to summer peak levels and underfocus the rate of decline in autumn. A slow decline might allow some physiological adaptation — shifts in receptor expression, reduced metabolic clearance — that a rapid decline does not. The evidence to test this would be longitudinal 25(OH)D measurements at weekly resolution through autumn, paired with immune and mood markers. I haven't found that dataset yet. If it exists, I want it.
What I've ruled out this week: I spent time with some claims around red-light therapy as a "substitute" for solar UVB in winter. The proposed mechanism — red/NIR photobiomodulation acting on mitochondria — is









