Gloucester roofs, specifically
Why Gloucester roofs grow moss almost year-round.
Gloucester sits on the floor of the Severn Vale, with the river curving past the docks and the floodplain stretching west to the Forest of Dean. The combination of low elevation, river-borne humidity and mild winters makes the city one of the dampest urban environments in the county. Where Cheltenham sits in a basin against the Cotswold escarpment and Newent picks up Forest of Dean cloud, Gloucester gets the worst of both worlds — mist rising off the Severn nearly every morning, low cloud trapped in the vale on still days, and a winter that almost never freezes hard enough to set back biological growth on roofs.
For tiles, that means a microclimate where moss, lichen and gloeocapsa algae have an effectively year-round growing season. We see this most dramatically on the post-war and modern stock that makes up the bulk of the city — Tuffley, Quedgeley, Hucclecote, Coney Hill, Matson, Saintbridge, Abbeymead, Abbeydale, Brockworth and the newer Quedgeley estates. Concrete interlocking tiles in Marley, Redland and Sandtoft profiles dominate, and the textured surface of those tiles is exactly what moss spores need to colonise. Twenty-year-old estates that haven't been touched routinely show a continuous green carpet across north-facing pitches by their second decade.
The older Victorian streets — Kingsholm, Tredworth, Linden, the streets around the cathedral, Spa — tell a different story. Welsh slate dominates here, often laid over pitched roofs at relatively shallow angles by modern standards. The slate itself is fine, and Welsh slate cleaned and biocided properly will outlast most owners. The issue tends to be moss build-up between the courses, lead flashings around chimneys staining the slates below, and the occasional cracked or slipped slate that we'll spot during the survey and flag before quoting.